2016 Pacific typhoon season#Severe Tropical Storm Chanthu

During the year several national meteorological services and scientific agencies forecast how many tropical cyclones, tropical storms, and typhoons will form during a season and/or how many tropical cyclones will affect a particular country. These agencies included the Tropical Storm Risk (TSR) Consortium of University College London, PAGASA and Taiwan's Central Weather Bureau. Some of the forecasts took into consideration what happened in previous seasons and the El Niño conditions that were observed during the previous year. The first forecast of the year was released by PAGASA during January 2016, within its seasonal climate outlook for the period January – June. The outlook noted that one to two tropical cyclones were expected between January and March, while one to three were expected to develop or enter the Philippine Area of Responsibility between April and June.

During March the Hong Kong Observatory predicted that the typhoon season in Hong Kong would be near-normal, with four to seven tropical cyclones passing within {{convert|500|km|mi|round=5|abbr=on}} of the territory compared to an average of six,{{cite web|title=Speech by Mr Shun Chi-ming, Director of the Hong Kong Observatory March 15, 2016 |date=March 15, 2016 |access-date=April 3, 2016 |url=http://www.hko.gov.hk/dhkovoice/speech20160315e.pdf |url-status=live |archive-date=April 15, 2016 |archive-url=https://web.archive.org/web/20160415033623/http://www.hko.gov.hk/dhkovoice/speech20160315e.pdf |publisher=Hong Kong Observatory |author=Chi-ming, Shun }} which was revised to five to eight tropical cyclones in August. On May 7, Tropical Storm Risk issued its first forecast for the season and predicted that it will be a quiet season, with 22 tropical storms, 13 typhoons, and 6 intense typhoons developing during the year, while an ACE Index of 217 was also forecast. Ahead of the Thailand rainy season starting during May, the Thai Meteorological Department predicted that two tropical cyclones would move near Thailand during 2016.{{cite web|date=April 25, 2016 |title=The Seasonal forecast of Thailand during the Rainy Season of 2016 |archive-url=https://web.archive.org/web/20160507011945/http://www.tmd.go.th/en/seasonal_forecast.php |archive-date=May 7, 2016 |access-date=May 8, 2016 |url=http://www.tmd.go.th/en/seasonal_forecast.php |publisher=Thai Meteorological Department |url-status=dead }} They predicted that there was a high chance that the first tropical cyclone would move past northern and north-eastern Thailand during August or September. The second tropical cyclone was predicted to move past Southern Thailand during October and November. On June 28, Taiwan's Central Weather Bureau predicted that between 19 and 23 tropical storms would develop over the basin, while two — four systems were expected to affect Taiwan itself.

On July 6, TSR released their second forecast for the season. They predicted mostly the same numbers as the previous forecast, but raised the number of intense typhoons to 7. PAGASA issued their second and final forecast for the year on July 15, within its seasonal climate outlook for the period July – December. The outlook noted that between five and eleven tropical cyclones were expected between July and September, while four to nine were expected to develop or enter the Philippine Area of Responsibility between October and December. TSR issued their final forecast for the season on August 8, sustaining the tropical cyclone numbers, however its ACE was slightly lowered than the previous forecast.

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{{main|Timeline of the 2016 Pacific typhoon season}}

Despite the season's late start, the 2016 season was a normal and active season with a total of 53 tropical depressions, of which 26 became tropical storms. After five months of inactivity, the first tropical depression developed on May 26, making it the fifth-latest season for a system to form. According to existing records only four other seasons started later—the 1973, 1983, 1984, and 1998 seasons. Tropical activity throughout the basin became marginally favorable for development, and two tropical depressions developed during June. On July 3, Nepartak became the first named tropical storm, making it the second-latest first named storm on record. Nepartak's naming ended a 199-day period (from December 17, 2015, to July 2, 2016) during which no named storm was active within the basin; this period tied the 199-day period from December 22, 1997, to July 8, 1998.{{cite web|title=Ranking of Typhoon Inactive Period (W. North Pacific) : Top 500|url=http://agora.ex.nii.ac.jp/digital-typhoon/reference/period-inactive.html.en|publisher=Digital Typhoon|access-date=July 6, 2016}} Nepartak reached Category 5 super typhoon intensity before making landfall in Taiwan and East China, causing a total of US$1.52 billion of damage. In late July, Tropical Storm Mirinae reached its peak intensity while making landfall over Red River Delta in Northern Vietnam. The storm caused a total of US$334 million of damage{{refn|All damage totals are valued as of 2016 and in United States dollars, unless otherwise noted.|group="nb"}} in Hainan and Vietnam. Later, Nida reached near typhoon strength; it affected the Philippines, South China and Vietnam, but its damage was lower than that of Mirinae. The season became more active in August, with 7 named storms. Except Dianmu, which affected South China, Indochina, all of the tropical cyclones in August affected Japan and the Russian Far East. By the end of August, three storms (Chanthu, Lionrock and Kompasu) had hit the Japanese island of Hokkaidō, the most since 1951.{{cite web|author=Dave Ornauer|publisher=Stars and Stripes|date=August 28, 2016|title=Lionrock could give Tokyo area another drenching|access-date=August 28, 2016|url=http://japan.stripes.com/news/lionrock-could-give-tokyo-area-another-drenching|archive-url=https://web.archive.org/web/20160828020402/http://japan.stripes.com/news/lionrock-could-give-tokyo-area-another-drenching|archive-date=August 28, 2016|url-status=dead}} Lionrock was a large, powerful, long-lived and erratic tropical cyclone which caused significant flooding and casualties in North Korea and Japan in late August.

Image:MerantiMalakasRai 2016-09-13.jpg

In September, Typhoon Meranti became the strongest typhoon in terms of pressure since Typhoon Megi in 2010, as well as the strongest typhoon in terms of sustained winds since Typhoon Haiyan in 2013, and the second-strongest tropical cyclone worldwide in 2016, only behind Cyclone Winston, in terms of pressure. Typhoon Megi reached its peak intensity as a Category 3 typhoon while making landfall over Taiwan. Both Meranti and Megi made landfall in Fujian, China, and they caused a total of US$3.6 billion of damage. Rai became a weak tropical storm before it made landfall in Vietnam, Laos and Thailand in mid-September, causing flooding and moderate damage. Typhoon Malakas impacted Japan with a total of nearly $740 million of damage as a Category 4 typhoon. In late September and early October, Typhoon Chaba reached Category 5 super typhoon intensity and became the strongest tropical cyclone to make landfall in South Korea since Sanba in 2012. Chaba also caused 7 deaths in the country.{{cite news |url=http://english.yonhapnews.co.kr/national/2016/10/06/38/0302000000AEN20161006002652315F.html |title=Typhoon Chaba leaves 7 dead, 3 missing in southern S. Korea |author= |date=6 October 2016 |newspaper=Yonhap News |access-date=7 October 2016}} A tropical depression formed east of the International Date Line on October 3, and entered the basin before developing into Typhoon Songda. Songda struck the Pacific Northwest region of the United States and Canada as a powerful extratropical cyclone.{{cite web|author1=Bob Henson|title=Potential once-in-a-decade windstorm takes shape for Pacific Northwest|url=https://www.wunderground.com/blog/JeffMasters/bermuda-endures-direct-hit-from-nicole-fierce-winds-in-store-for-paci|publisher=Weather Ungerground|access-date=October 14, 2016|date=October 14, 2016}} Severe Tropical Storm Aere affected parts of Southeast Asia in mid-October, including the worst flooding in Vietnam since 2010, causing a total of US$209 million of damage.{{cite web|url=http://vnexpress.net/tin-tuc/thoi-su/mua-o-quang-binh-la-ky-luc-chua-tung-co-3484061.html|publisher=vnexpress.net|title=Mưa ở Quảng Bình là 'kỷ lục chưa từng có' – VnExpress|access-date=November 13, 2016}} Later, Typhoon Sarika became a powerful typhoon, and affected the Philippines, China and Vietnam, causing severe damage as well as severe flooding in southern China. After Sarika, Typhoon Haima reached Category 5 super typhoon strength before impacting the Philippines and China, causing a total of US$1.93 billion in damages. Haima was the most severe tropical cyclone to affect Hong Kong in October since 1995. In early November, a tropical depression made landfall in Southern Vietnam and caused heavy flooding throughout central and southern Vietnam, causing moderate damage. In late December, Nock-ten became the strongest Christmas tropical cyclone on record anywhere in the world since at least 1960 in terms of 1-minute sustained winds, before impacting the Philippines.{{cite web |url=https://twitter.com/philklotzbach/status/812854171653148672 |title=#Nockten's current intensity of 155 mph is strongest for TC anywhere around the globe on Christmas (UTC time) on record (since 1960) |last=Klotzbach |first=Phil |date=December 25, 2016 |access-date=December 27, 2016}}{{cite web |url=https://weather.com/storms/typhoon/news/typhoon-nock-ten-nina-philippines-christmas |title=Super Typhoon Nock-Ten (Nina), the Most Intense Christmas Tropical Cyclone in 56 Years, Hammers the Philippines |last1=Lam |first1=Linda |last2=Erdman |first2=Jon |date=December 26, 2016 |publisher=The Weather Channel |access-date=December 27, 2016}}

The Accumulated Cyclone Energy (ACE) index for the 2016 Pacific typhoon season as calculated by Colorado State University using data from the Joint Typhoon Warning Center was 261.9 units.{{cite web| title=Basin Archives: Northwest Pacific Ocean Historical Tropical Cyclone Statistics|url=http://tropical.atmos.colostate.edu/Realtime/index.php?arch&loc=northwestpacific|publisher=Colorado State University|location=Fort Collins, Colorado|access-date=21 June 2023}} Broadly speaking, ACE is a measure of the power of a tropical or subtropical storm multiplied by the length of time it existed. It is only calculated for full advisories on specific tropical and subtropical systems reaching or exceeding wind speeds of {{convert|39|mph|km/h}}.

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = May 25

| Dissipated = May 27

| Image = 01W 2016-05-27 0540Z.jpg

| Track = 01W 2016 track.png

| Type1 = nwpdepression

| 10-min winds = 30

| 1-min winds = 30

| Pressure = 1000

| Prewinds = <

}}

During May 25, Tropical Depression 01W developed over the northern South China Sea, about {{convert|600|km|mi|round=5|abbr=on}} to the south of Hong Kong, China.{{cite web|title=Monthly Global Tropical System Tracks - May 2016|publisher=Australian Severe Weather|date=June 29, 2016|access-date=June 29, 2016|url=http://australiasevereweather.com/cyclones/2016/trak1605.htm|author=Young, Steve}}{{cite web|title=Tropical Depression May 26-27, 2016 |url=http://www.weather.gov.hk/informtc/td0526/report.htm |publisher=Hong Kong Observatory|access-date=June 26, 2016 |archive-url=https://web.archive.org/web/20160618030026/http://www.weather.gov.hk/informtc/td0526/report.htm |archive-date=June 18, 2016|date=June 2016|url-status=live}} The system subsequently moved north-westwards and slightly developed further, before it made landfall near Yangjiang in Guangdong, China during the next day. The system subsequently quickly weakened and degenerated into an area of low pressure during May 27.

The system brought squally and heavy rain to the Pearl River Delta, including parts of Hong Kong, Macau and Guangdong province, where a bridge was destroyed by flooding and two people were injured. At the Macau Ferry Terminal, two passengers were injured as a vessel collided with the terminal, while there was no significant damage reported within Hong Kong. Damage in China were at CN¥60 million (US$9.14 million).

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{{Infobox tropical cyclone small

| Basin = WPac

| Formed = June 25

| Dissipated = June 28

| Image = Ambo 2016-06-26 0550Z.jpg

| Track = Ambo 2016 track.png

| 10-min winds = 30

| Pressure = 1004

}}

Early on June 26, the JMA and PAGASA reported that Tropical Depression Ambo had developed over the Philippine Sea, about {{convert|555|km|mi|round=5|abbr=on}} to the east of Manila on the island of Luzon in the Philippines.{{cite web|url=http://www.jma.go.jp/en/g3/ |date=June 26, 2016 |title=JMA WWJP25 Warning and Summary June 26, 2016 06z |agency=Japan Meteorological Agency |archive-date=May 23, 2024 |access-date=June 28, 2016 |archive-url=https://archive.today/20240523235821/https://www.webcitation.org/6ic1eJhOY?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201606260000.htm |url-status=dead }}{{cite report|title=Severe Weather Bulletin No. 01 re Tropical Depression "AMBO"|url=http://www.ndrrmc.gov.ph/attachments/article/2779/SWB_No_01_re_Tropical_Depression_AMBO_issued_on_26JUNE2016_1000H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=June 26, 2016|access-date=February 9, 2019}} The system was located within an environment that was thought to be favourable for further development, with low vertical wind shear and a fair outflow.{{cite web|date=June 26, 2016 |title=Tropical Cyclone Formation Alert June 26, 2016 00z |agency=United States Joint Typhoon Warning Center |archive-url=https://archive.today/20240523235901/https://www.webcitation.org/6il4aTK74?url=http://gwydir.demon.co.uk/advisories/WTPN21-PGTW_201606260000.htm |archive-date=May 23, 2024 |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |url-status=dead }} However, the depression's broad low level circulation centre was moving north-westwards quickly, which meant that the circulation's southern edge could not close off and was exposed. The system subsequently made landfall on Luzon in Philippines later that day, where according to PAGASA it quickly weakened into a low-pressure area.{{cite report|title=Severe Weather Bulletin No. 05 (Final) re Tropical Depression "AMBO"|url=http://www.ndrrmc.gov.ph/attachments/article/2779/SWB_No_05_FINAL_re_Tropical_Depression_AMBO_issued_on_27JUNE2016_0200H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=June 27, 2016|access-date=February 9, 2019}} However, the JMA continued to monitor the system as a tropical depression throughout June 27, as it emerged into an unfavourable environment for further development in the South China Sea.{{cite web|author=Young, Steve|title=Monthly Global Tropical System Tracks - June 2016|publisher=Australian Severe Weather|date=August 8, 2016|access-date=August 21, 2016|url=http://australiasevereweather.com/cyclones/2016/trak1606.htm}}{{cite web |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |agency=United States Joint Typhoon Warning Center |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans June 27, 2016 00z |archive-url=https://web.archive.org/web/20070216233156/http://weather.noaa.gov/pub/data/raw/ab/abpw10.pgtw..txt |archive-date=2007-02-16 |access-date=August 21, 2016 |url-status=dead }} The depression subsequently made landfall on China's Guangdong Province, before it was last noted during June 28, as it dissipated over land.

Several sea-trips in the Philippine island province of Catanduanes were cancelled with a total of seven passengers, three rolling cargoes and a sea vessel stranded at the port of Virac.{{cite report|url=https://ndrrmc.gov.ph/attachments/article/2780/FINAL_SITUATION_REPORT_re_Preparedness_Measures_and_Effects_of_Tropical_Depression_AMBO_as_of_26-27JUN2016.pdf|archive-url=https://web.archive.org/web/20210308204651/https://ndrrmc.gov.ph/attachments/article/2780/FINAL_SITUATION_REPORT_re_Preparedness_Measures_and_Effects_of_Tropical_Depression_AMBO_as_of_26-27JUN2016.pdf|url-status=dead|archive-date=March 8, 2021|title=Final Situation Report re Preparedness Measures and Effects of Tropical Depression (TD) "AMBO"|access-date=August 23, 2016|date=June 26–27, 2016}}

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{{Infobox tropical cyclone small

| Basin = WPac

| Formed = July 2

| Dissipated = July 10

| Image = Nepartak 2016-07-06 0450Z.jpg

| Track = Nepartak 2016 path.png

| 10-min winds = 110

| 1-min winds = 155

| Pressure = 900

}}

{{main|Typhoon Nepartak (2016)}}

On July 2, a tropical depression formed {{convert|780|km|mi|abbr=on}} to the southeast of Yap State.{{cite web|title=RSMC Tropical Cyclone Best Track 1601 NEPARTAK (1601)|url=http://www.wis-jma.go.jp/cms/warning/2016/08/22/typhoon-best-track-2016-08-22t050000z/|date=August 22, 2016|agency=Japan Meteorological Agency}}{{cite web|archive-date=May 23, 2024 |publisher=United States Joint Typhoon Warning Center |url=http://www.wis-jma.go.jp/d/o/PGTW/Alphanumeric/Analysis/Miscellaneous/20160701/170000/A_ABPW10PGTW011700_C_RJTD_20160701171817_1.txt |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans July 15, 2016 14z |url-status=dead |archive-url=https://archive.today/20240523112506/https://www.webcitation.org/6jw8uxuFH?url=http://www.wis-jma.go.jp/d/o/PGTW/Alphanumeric/Analysis/Miscellaneous/20160701/170000/A_ABPW10PGTW011700_C_RJTD_20160701171817_1.txt |access-date=August 21, 2016}} The following day, the depression became a tropical storm, receiving the name Nepartak. By July 4, organization increased and Nepartak intensified into a severe tropical storm. At that time, PAGASA assigned the local name Butchoy as it entered their area of responsibility.{{cite report|title=Severe Weather Bulletin No. 1 re Typhoon "NEPARTAK"|url=http://ndrrmc.gov.ph/attachments/article/2794/SWB_No_1_for_Typhoon_NEPARTAK_issued_on_05JUL2016_1100H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=July 5, 2016|access-date=February 9, 2019}} Early on July 5, Nepartak started to undergo rapid intensification, reaching typhoon strength. Nepartak soon reached Category 5 super typhoon intensity.{{#tag:ref|Tropical cyclones reaching Category 3 ({{convert|111|mph|km/h|disp=or|sp=us}}) and higher on the five-level Saffir–Simpson wind speed scale are considered major hurricanes.|group="nb"}}{{cite web |title=Super Typhoon 02W (Nepartak) Warning Nr 013 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607060300.htm |date=July 6, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524000144/https://www.webcitation.org/6itpIfpfH?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607060300.htm |access-date=May 22, 2017 }} During the course of July 6, Nepartak reached its peak intensity with 10-minute sustained winds of {{convert|205|km/h|mph|abbr=on|round=5}} and a minimum barometric pressure of 900 mbar.{{cite web|title=Super Typhoon 02W (Nepartak) Warning Nr 014 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607060900.htm |date=July 6, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524000223/https://www.webcitation.org/6itpIIxjG?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607060900.htm |access-date=May 22, 2017}} Nepartak started weakening during the next day, before making landfall in Taitung City on July 8. Nepartak weakened to a tropical storm{{cite web |title=Tropical Storm 02W (Nepartak) Warning Nr 024 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607082100.htm |date=July 8, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524000101/https://www.webcitation.org/6itpEVr2l?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607082100.htm |access-date=May 22, 2017 }} as it made its second landfall in Shishi, Fujian.{{cite web|script-title=zh:中央气象台9日13时45分发布台风登陆消息|url=http://www.nmc.cn/publish/typhoon/warning.html|publisher=National Meteorological Center|access-date=July 9, 2016|archive-url=https://web.archive.org/web/20160709061532/http://www.nmc.cn/publish/typhoon/warning.html|archive-date=July 9, 2016|language=zh|date=July 9, 2016}} Nepartak rapidly deteriorated over land and fully dissipated on July 10.{{cite web |title=Tropical Storm 02W (Nepartak) Warning Nr 026 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607090900.htm |date=July 9, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524000023/https://www.webcitation.org/6itpDhC91?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607090900.htm |access-date=May 22, 2017 }}

Two people drowned on July 7 after being washed out to sea by strong winds in Taiwan.{{cite web|url=http://focustaiwan.tw/news/asoc/201607080010.aspx|title=69 injured in Taitung as Typhoon Nepartak batters Taiwan|date=July 8, 2016|publisher=Focus Taiwan|access-date=July 8, 2016}} A total of seven major highways were damaged in Taiwan, too.{{cite news|author1=Yang Shu-min |author2=Chu Tze-wei |author3=Lilian Wu |publisher=Focus Taiwan|date=July 9, 2016|access-date=July 9, 2016|title=Typhoon causes estimated NT$800 million in agricultural losses|url=http://focustaiwan.tw/search/201607090016.aspx|location=Taipei, Taiwan}} At least 10 people were killed and 11 others were reported missing across Fujian and Jiangxi.{{cite news|author=Fei Fei|publisher=CRI English|date=July 11, 2016|access-date=July 11, 2016|title=Typhoon Nepartak leaves 9 dead, 18 missing in southeast China|url=http://english.cri.cn/12394/2016/07/11/3521s933787.htm|archive-url=https://web.archive.org/web/20160712125125/http://english.cri.cn/12394/2016/07/11/3521s933787.htm|url-status=dead|archive-date=July 12, 2016}} At least 3,144 homes were destroyed and {{convert|15800|hectare|acre|abbr=on}} of crops were damaged; total economic losses reached ¥2.2 billion (US$320 million).{{cite news|agency=Xinhua|date=July 11, 2016|access-date=July 12, 2016|title=Typhoon Nepartak leaves 10 dead, 11 missing in E China county|url=http://news.xinhuanet.com/english/2016-07/11/c_135505467.htm|archive-url=https://web.archive.org/web/20160712004218/http://news.xinhuanet.com/english/2016-07/11/c_135505467.htm|url-status=dead|archive-date=July 12, 2016|location=Fuzhou, China}}{{cite web|author=Liu Yuanhui|agency=Xinhua|publisher=CRI English|date=July 11, 2016|access-date=July 11, 2016|title=Typhoon Nepartak leaves six dead, eight missing in east China|url=http://english.cri.cn/12394/2016/07/11/2561s933717.htm|archive-url=https://web.archive.org/web/20160711112739/http://english.cri.cn/12394/2016/07/11/2561s933717.htm|url-status=dead|archive-date=July 11, 2016}} Overall, Nepartak killed a total of 86 people, mostly from Fujian Province, and caused a total of ¥9.99 billion (US$1.49 billion) of damage.{{cite web|script-title=zh:"尼伯特"重创福建福州 已致83人死亡19人失踪|url=http://www.chinanews.com/gn/2016/07-17/7942283.shtml|publisher=China News Service|access-date=July 18, 2016|language=zh|date=July 17, 2016}}{{cite web|script-title=zh:"尼伯特"致福建69死6失踪 直接经济损失近百亿|url=http://www.chinanews.com/gn/2016/07-15/7939740.shtml|publisher=China News Service|access-date=July 15, 2016|language=zh|date=July 15, 2016}}

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{{Infobox tropical cyclone small

| Basin = WPac

| Formed = July 15

| Dissipated = July 20

| Image = 03W 2016-07-17 0430Z.jpg

| Track = 03W 2016 track.png

| Type1 = nwpdepression

| 10-min winds = 30

| 1-min winds = 25

| Pressure = 1006

}}

During July 14, a tropical disturbance developed about {{convert|400|km|mi|round=5|abbr=on}} to the west-northwest of Guam.{{cite web|date=July 14, 2016 |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans July 14, 2016 06z |agency=United States Joint Typhoon Warning Center |archive-url=https://archive.today/20240524002312/https://www.webcitation.org/6jRnKibkv?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201607141930.htm |archive-date=May 24, 2024 |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |url-status=dead }} At this time atmospheric convection surrounding the system was flaring, over the system's weak but developing low level circulation center. However, as a subtropical ridge of high pressure extended a significant amount of dry air over the disturbance, conditions were assessed to be marginally favorable for further development of the system. Over the next couple of days the system gradually developed further as it moved north-westwards and was classified as a tropical depression by the JMA during July 15.{{cite web|archive-date=May 24, 2024 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |agency=United States Joint Typhoon Warning Center |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans July 15, 2016 14z |archive-url=https://archive.today/20240524000303/https://www.webcitation.org/6j4znaK89?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201607161400.htm |access-date=July 31, 2016 |url-status=dead }}{{cite web|url=http://www.jma.go.jp/en/g3/ |title=JMA WWJP25 Warning and Summary July 15, 2016 00z |agency=Japan Meteorological Agency |archive-date=May 23, 2024 |access-date=July 31, 2016 |archive-url=https://archive.today/20240523225513/https://www.webcitation.org/6cQeTEJOn?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201510200000.htm |date=October 20, 2015 |url-status=dead }} After the system had consolidated further, it was classified as Tropical Depression 03W by the JTWC during July 17.{{cite web|archive-date=May 24, 2024 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |title=JTWC Prognostic Reasoning For Tropical Depression 03W July 17, 2016 09z |archive-url=https://archive.today/20240524000424/https://www.webcitation.org/6j5XWnRC9?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201607170900.htm |agency=United States Joint Typhoon Warning Center |access-date=July 17, 2016 |url-status=dead }} However, the system weakened during that day as it moved polewards, along the western edge of the subtropical ridge of high pressure, into an area of increasing vertical wind shear. As a result, the JTWC expected the system to quickly dissipate and issued their final advisory later that day.{{cite web|title=Tropical Depression 03W Warning July 17, 2016 15z |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |archive-url=https://archive.today/20240524000343/https://www.webcitation.org/6j5XMGNAm?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607171500.htm |date=July 17, 2016 |agency=United States Joint Typhoon Warning Centre |archive-date=May 24, 2024 |url-status=dead }} However, over the next couple of days the system continued to move northwards and impacted the Ryukyu Islands, before it was last noted by the JMA during July 20.{{cite web|url=http://www.jma.go.jp/en/g3/ |title=JMA WWJP25 Warning and Summary July 20, 2016 06z |archive-date=May 24, 2024 |access-date=August 2, 2016 |date=July 20, 2016 |archive-url=https://archive.today/20240524002351/https://www.webcitation.org/6jRnUS837?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201607200600.htm |agency=Japan Meteorological Agency |url-status=dead }}{{cite web|author=Young, Steve|title=Monthly Global Tropical System Tracks - July 2016|publisher=Australian Severe Weather|date=August 20, 2016|access-date=August 20, 2016|url=http://australiasevereweather.com/cyclones/2017/trak1607.htm}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = July 22

| Dissipated = July 24

| Image = Lupit 2016-07-24 0245Z.jpg

| Track = Lupit 2016 track.png

| 10-min winds = 40

| 1-min winds = 40

| Pressure = 1000

}}

During July 21, a subtropical disturbance developed at the tailend of a mid-latitude trough of low pressure, about {{convert|775|km|mi|round=5|abbr=on}} to the east of Iwo-To.{{cite web|date=July 22, 2016 |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans July 22, 2016 06z |agency=United States Joint Typhoon Warning Center |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |archive-url=https://archive.today/20240523231845/https://www.webcitation.org/6jH1XqTww?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201607220600.htm |archive-date=May 23, 2024 |url-status=dead }} Over the next day, deep atmospheric convection developed over the system's elongated low level circulation center, before it was classified as a tropical depression by the JMA during July 22.{{cite report|title=Tropical Storm Lupit |url=http://www.wis-jma.go.jp/cms/warning/2016/08/23/typhoon-best-track-2016-08-23t060000z/ |type=RSMC Tropical Cyclone Best Track |access-date=August 24, 2016 |url-status=live |publisher=Japan Meteorological Agency |archive-url=https://archive.today/20240522191527/https://www.webcitation.org/6jzup68EF?url=http://gwydir.demon.co.uk/advisories/AXPQ20-RJTD_201608230600.htm |archive-date=May 22, 2024 |date=August 23, 2016 }} Over the next day, as the storm moved north-northeastwards around a subtropical ridge of high pressure, its structure improved as it developed a warm core and consolidated.{{cite web|archive-date=May 24, 2024 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |title=JTWC Prognostic Reasoning For Tropical Depression 04W July 23, 2016 15z |archive-url=https://archive.today/20240524001026/https://www.webcitation.org/6jH0v3mkg?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201607231500.htm |agency=United States Joint Typhoon Warning Center |access-date=August 6, 2016 |url-status=dead }} The hybrid system was subsequently classified as Tropical Storm 04W by the JTWC during July 23, before the JMA named it Lupit later that day. Over the next day, Lupit peaked with sustained winds of {{convert|75|km/h|mph|abbr=on}}, as it went through an extratropical transition and took on frontal characteristics.{{cite web|archive-date=May 24, 2024 |url=https://metoc.ndbc.noaa.gov/ProductFeeds-portlet/img/jtwc/products/wp0716prog.txt |title=JTWC Prognostic Reasoning For Tropical Depression 04W July 24, 2016 03z |archive-url=https://archive.today/20240524001026/https://www.webcitation.org/6jH0v3mkg?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201607231500.htm |agency=United States Joint Typhoon Warning Center |access-date=August 6, 2016 |url-status=dead }} Lupit subsequently became extratropical during July 24, before it dissipated during July 26, as it moved into the Sea of Okhotsk.

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = July 25

| Dissipated = July 28

| Image = Mirinae 2016-07-27 1900Z.jpg

| Track = Mirinae 2016 track.png

| 10-min winds = 55

| 1-min winds = 65

| Pressure = 980

}}

{{Main|Tropical Storm Mirinae (2016)}}

Mirinae was first noted as a tropical depression during July 25, as it moved off the west coast of Luzon into the South China Sea, about {{convert|300|km|mi|round=5|abbr=on}} to the east of the Paracel Islands.{{cite web|url-status=live |publisher=Hong Kong Observatory |title=Severe Tropical Storm Mirinae (1603) July 25-28, 2016 |date=August 12, 2016 |url=http://www.weather.gov.hk/informtc/mirinae/report.htm |access-date=August 17, 2016 |archive-url=https://web.archive.org/web/20160817123817/http://www.weather.gov.hk/informtc/mirinae/report.htm |archive-date=August 17, 2016 }}{{cite web|date=July 25, 2016 |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans July 25, 2016 02z |archive-date=May 23, 2024 |agency=United States Joint Typhoon Warning Center |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |archive-url=https://archive.today/20240523000517/https://www.webcitation.org/6jH0DJPqB?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201607250200.htm |url-status=dead }} The next day, it was named Mirinae after it became a tropical storm. Mirinae subsequently weakened slightly as it made landfall later that day, near Wanning and crossed Hainan Island. It re-intensified on moving into the Gulf of Tonkin.{{cite web|script-title=zh:台风公报|url=http://www.nmc.cn/publish/typhoon/warning.html|publisher=National Meteorological Center|access-date=July 26, 2016|archive-url=https://web.archive.org/web/20160726144859/http://www.nmc.cn/publish/typhoon/warning.html|archive-date=July 26, 2016|language=zh|date=July 26, 2016}} The system reached its peak intensity as a severe tropical storm on July 27, with 10-minute sustained winds of {{convert|95|km/h|mph|abbr=on}}. The system made landfall about {{convert|110|km|mi|round=5|abbr=on}} to the south of Hanoi in northern Vietnam later that day.{{cite web|archive-date=May 23, 2024 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |access-date=August 17, 2016 |title=JTWC Prognostic Reasoning For Tropical Storm 05W July 27, 2016 15z |archive-url=https://archive.today/20240523000717/https://www.webcitation.org/6jK4lyxQf?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201607271500.htm |agency=United States Joint Typhoon Warning Center |url-status=dead }} Mirinae subsequently weakened gradually over northern Vietnam, before it dissipated to the north of Hanoi. On mainland Vietnam, a weather station in Văn Lý (Nam Định) recorded sustained winds of {{convert|33|m/s|km/h mph|0|abbr=on|order=out|round=}} with gusts reaching {{convert|40|m/s|km/h mph|0|abbr=on|order=out|round=}}{{Cite web |last=Bảo Anh |date=September 6, 2024 |editor-first= |title=Các cơn bão mạnh gây thiệt hại nặng nề ở Việt Nam những năm gần đây |trans-title=Strong typhoon have caused significant damage in Vietnam in recent years |url=https://nhandan.vn/nhung-con-bao-manh-gay-thiet-hai-nang-ne-o-viet-nam-nhung-nam-gan-day-post828912.html |url-status=live |access-date=April 20, 2025 |website=Nhân Dân |language=vi}}, while another station in Ba Lạt (Thái Bình) recorded wind gusts of {{convert|47|m/s|km/h mph|0|abbr=on|order=out|round=}}.{{cite conference |author=Vietnam's National Hydro-Meteorological Service |date=October 27, 2016 |title=Member Report: Socialist Republic of Vietnam |url=http://www.typhooncommittee.org/11IWS/docs/Members%20Report/Country%20Report%202016%20ngay%2012thang10.pdf |conference=ESCAP/WMO Typhoon Committee |publisher=ESCAP/WMO Typhoon Committee |pages=1–2 |archive-url=https://web.archive.org/web/20161030060828/http://www.typhooncommittee.org/11IWS/docs/Members%20Report/Country%20Report%202016%20ngay%2012thang10.pdf |archive-date=October 30, 2016 |access-date=October 30, 2016 |conference-url=http://www.typhooncommittee.org/11IWS/ |url-status=dead}}

In Hainan, economic losses caused by the storm reached 300 million yuan (US$45 million).{{cite web|url=http://news.xinhuanet.com/english/2016-08/10/c_135583432.htm|archive-url=https://web.archive.org/web/20160810154051/http://news.xinhuanet.com/english/2016-08/10/c_135583432.htm|url-status=dead|archive-date=August 10, 2016|access-date=November 13, 2016|title=Natural disasters kill 612 in China in July|agency=Xinhua|date=August 10, 2016}} By July 29, the storm had left five people dead and five others missing in Vietnam. Severe damage to infrastructure was reported in Northern Vietnam, with damage to power lines causing blackouts and power cuts in some areas. Mirinae also sank 12 boats, destroyed the roofs of 1,425 houses and uprooted about 5,000 trees.{{cite web|url=http://tuoitrenews.vn/society/36248/ten-killed-missing-as-storm-mirinae-pounds-northern-vietnam |title=Ten killed, missing as storm Mirinae pounds northern Vietnam |website=Tuổi Trẻ News |access-date=July 31, 2016}} Damages in Vietnam amounted to ₫7.229 trillion ($323.9 million).

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = July 29

| Dissipated = August 3

| Image = Nida 2016-08-01 0515Z.jpg

| Track = Nida 2016 track.png

| 10-min winds = 60

| 1-min winds = 80

| Pressure = 975

}}

{{Main|Tropical Storm Nida (2016)}}

During July 28, a tropical depression developed about {{convert|1020|km|mi|round=5|abbr=on}} to the east-southeast of Manila in the Philippines.{{cite web|date=July 28, 2016 |url=http://www.jma.go.jp/en/g3/ |title=JMA WWJP25 Warning and Summary July 28, 2016 12z |publisher=Japan Meteorological Agency |archive-url=https://archive.today/20240523002202/https://www.webcitation.org/6jLWIChGc?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201607281200.htm |archive-date=May 23, 2024 |access-date=August 1, 2016 |url-status=dead }}{{cite web|archive-date=May 23, 2024 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans July 28, 2016 13z |publisher=United States Joint Typhoon Warning Center |archive-url=https://archive.today/20240523002121/https://www.webcitation.org/6jLW1sGGj?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201607281230.htm |access-date=August 1, 2016 |url-status=dead }} Over the next day as the system moved north-northwestwards under the influence of a subtropical ridge of high pressure, deep convection started wrapping into the system's low level circulation center.{{cite web|title=Tropical Cyclone Formation Alert July 29, 2016 02z |archive-date=May 23, 2024 |access-date=August 1, 2016 |publisher=United States Joint Typhoon Warning Center |url=http://www.wis-jma.go.jp/d/o/PGTW/Alphanumeric/Warning/Tropical_cyclone/20160729/013000/A_WTPN21PGTW290130_C_RJTD_20160729013203_3.txt |archive-url=https://archive.today/20240523002324/https://www.webcitation.org/6jRkZpQEp?url=http://www.wis-jma.go.jp/d/o/PGTW/Alphanumeric/Warning/Tropical_cyclone/20160729/013000/A_WTPN21PGTW290130_C_RJTD_20160729013203_3.txt |url-status=dead }} During that day PAGASA assigned the local name Carina.{{cite web |url-status=dead |title=Severe Weather Bulletin #1: Tropical Cyclone Alert: Tropical Depression Carina |url=http://www.pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/248-tropical-cyclones/tropical-cyclone-warning-for-shipping/carina-2016-shipping/2741-carina1 |archive-url=https://web.archive.org/web/20160806180939/http://www.pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/248-tropical-cyclones/tropical-cyclone-warning-for-shipping/carina-2016-shipping/2741-carina1 |date=July 29, 2016 |access-date=August 1, 2016 |publisher=Philippine Atmospheric, Geophysical and Astronomical Services Administration |archive-date=August 6, 2016 }}

On July 31, Nida made landfall over the area between Baggao and Gattaran of the Cagayan province in the Philippines at 13:20 PST (05:20 UTC) as a severe tropical storm.{{cite web|url=https://twitter.com/dost_pagasa/status/759647447790395392|title=At 1:20 pm today, #CarinaPH has made landfall over Cabutunan point (Baggao-Gattaran area).|date=July 31, 2016|website=Twitter|publisher=PAGASA|access-date=August 2, 2016}} At 03:35 CST on August 2 (19:35 UTC on August 1), Nida made landfall over Dapeng Peninsula of Shenzhen, Guangdong, China as a severe tropical storm.{{cite web|url=http://www.nmc.cn/publish/weather-bulletin/index.htm|title=今年第4号台风"妮妲"今日凌晨在广东深圳登陆|date=August 1, 2016|publisher=National Meteorological Center|archive-url=https://web.archive.org/web/20160802023236/http://www.nmc.cn/publish/weather-bulletin/index.htm|archive-date=August 2, 2016|access-date=August 2, 2016}}

While it lashes the Northeastern part of the Philippines, the provinces of Isabela, Cagayan, Quirino Province, Abra, Mt. Province, Benguet, Kalinga Province, and Ifugao Province reported that some of their major roads was not passable due to landslides. Despite the local governments of the said areas reported that there are no casualties, they still reported that some of them are injured during the typhoon.{{cite web|title='Carina sweeps CAR; zero casualty noted|url=http://www.sunstar.com.ph/baguio/local-news/2016/08/01/carina-sweeps-car-zero-casualty-noted-488774|publisher=SunStar Baguio|accessdate=August 30, 2016|date=August 1, 2016|archive-date=September 11, 2016|archive-url=https://web.archive.org/web/20160911230842/http://www.sunstar.com.ph/baguio/local-news/2016/08/01/carina-sweeps-car-zero-casualty-noted-488774|url-status=dead}} Damages in Ilocos Norte were estimated at ₱19.38 million (US$411,000).{{cite news|author=Kim Lorenzo|url=https://news.abs-cbn.com/news/08/02/16/carina-leaves-p19-m-worth-of-damage-in-ilocos-norte|title='Carina' leaves P19-M worth of damage in Ilocos Norte|publisher=ABS-CBN News|date=August 2, 2016|accessdate=August 30, 2016}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 2

| Dissipated = August 9

| Image = Omais 2016-08-06 0345Z.jpg

| Track = Omais 2016 track.png

| 10-min winds = 60

| 1-min winds = 65

| Pressure = 975

}}

During August 2, the JMA started to monitor a tropical depression that had developed within a favourable environment for further development, about {{convert|565|km|mi|round=5|abbr=on}} to the northeast of Hagåtña, Guam.{{cite report|title=Severe Tropical Storm Lupit |url=http://www.wis-jma.go.jp/cms/warning/2016/09/15/typhoon-best-track-2016-09-15t070000z/ |type=RSMC Tropical Cyclone Best Track |access-date=September 17, 2016 |url-status=live |date=September 15, 2016 |publisher=Japan Meteorological Agency |archive-url=https://archive.today/20240522100715/https://www.webcitation.org/6kXpVUGFq?url=http://gwydir.demon.co.uk/advisories/AXPQ20-RJTD_201609150700.htm |archive-date=May 22, 2024 }}{{cite web|date=August 2, 2016 |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans August 2, 2016 06z |agency=United States Joint Typhoon Warning Center |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |archive-url=https://archive.today/20240524002916/https://www.webcitation.org/6jT8DV0Hn?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201608020600.htm |archive-date=May 24, 2024 |access-date=September 17, 2016 |url-status=dead }} The system had a broad and weak low level circulation centre, which had atmospheric convection flaring around the system's outer edge. Over the next couple of days the system slowly moved north-eastwards, before it was classified as Tropical Storm 07W by the JTWC and named Omais by the JMA during August 4.https://www.webcitation.org/6jWExC12G?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608041500.htm

A high-pressure system kept Omais to the east of Japan producing hot and steamy conditions across Japan approximately about 1000 people were taken to hospital due to heat stroke as the heat index climbed well into the 40s.{{cite web |url=https://westernpacificweather.com/2016/08/07/tropical-storm-omais-skirts-tokyo-and-central-japan-hot-mess-in-the-tropics-for-next-week/ |title = Westpacwx.com {{!}} Tropical Storm Omais Skirts Tokyo and Central Japan, Hot Mess in the Tropics for Next Week |access-date=2017-06-13 |archive-url=https://web.archive.org/web/20160809223010/http://www.westernpacificweather.com/2016/08/07/tropical-storm-omais-skirts-tokyo-and-central-japan-hot-mess-in-the-tropics-for-next-week/ |archive-date=2016-08-09 |url-status=dead }}

On August 9, Omais transitioned to an extratropical cyclone as it moved over cooler waters of the northwestern Pacific Ocean, Omais fully dissipated on August 10.{{cite web|url=https://phys.org/news/2016-08-nasa-tropical-storm-omais.html|title=NASA measures winds of Tropical Storm Omais}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 7

| Dissipated = August 15

| Image = Conson 2016-08-14 0255Z.jpg

| Track = Conson 2016 track.png

| 10-min winds = 45

| 1-min winds = 50

| Pressure = 985

}}

On August 7, the JMA started to monitor a tropical depression that had developed about {{convert|390|km|mi|round=5|abbr=on}} to the west of Wake Island.{{cite report|title=Tropical Storm Conson |url=http://www.wis-jma.go.jp/cms/warning/2016/09/15/typhoon-best-track-2016-09-15t080000z/ |type=RSMC Tropical Cyclone Best Track |access-date=September 15, 2016 |date=September 15, 2016 |url-status=live |publisher=Japan Meteorological Agency |archive-url=https://archive.today/20240522191604/https://www.webcitation.org/6kXpZdRdd?url=http://gwydir.demon.co.uk/advisories/AXPQ20-RJTD_201609150800.htm |archive-date=May 22, 2024 }} Over the next day the system gradually developed further as it moved south-westwards, before the JTWC classified it as Tropical Depression 08W during August 8.{{cite web|archive-date=May 24, 2024 |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |title=JTWC Prognostic Reasoning For Tropical Depression 08W August 8, 2016 09z |access-date=September 21, 2016 |archive-url=https://archive.today/20240524000825/https://www.webcitation.org/6jgPdbZBH?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608080900.htm |agency=United States Joint Typhoon Warning Center |url-status=dead }} Later that day, the JMA upgraded 08W to a tropical storm, naming it Conson.{{cite news |title=TS 1606 CONSON (1606) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608081800.htm |date=August 8, 2016 |access-date=August 11, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524000507/https://www.webcitation.org/6jgMazdv7?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608081800.htm |archive-date=May 24, 2024 }} Despite some moderate wind shear, Conson slowly intensified and later reached severe tropical storm strength on August 10.{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 02 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608092100.htm |date=August 9, 2016 |access-date=August 11, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524000746/https://www.webcitation.org/6jgPbJSFS?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608092100.htm |archive-date=May 24, 2024 }}{{cite news |title=STS 1606 CONSON (1606) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608100000.htm |date=August 10, 2016 |access-date=August 11, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524000547/https://www.webcitation.org/6jgMXR6xo?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608100000.htm |archive-date=May 24, 2024 }} The JTWC later stated that deep convection was forming near the center of Conson,{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 09 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608100900.htm |date=August 10, 2016 |access-date=August 11, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524000626/https://www.webcitation.org/6jgPacVlm?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608100900.htm |archive-date=May 24, 2024 }} however shortly thereafter, convection became disorganized.{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 10 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608101500.htm |date=August 10, 2016 |access-date=August 11, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524000708/https://www.webcitation.org/6jgPaGoxz?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608101500.htm |archive-date=May 24, 2024 }}

By August 11, convection once re-intensified again, however its LLCC became exposed, causing the JTWC to lower its intensity to lower-end of tropical storm strength.{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 13 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608110900.htm |date=August 11, 2016 |access-date=August 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524001509/https://www.webcitation.org/6jjfmtV4n?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608110900.htm |archive-date=May 24, 2024 }} The JMA also downgraded Conson to a tropical storm.{{cite news |title=TS 1606 CONSON (1606) DOWNGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608110000.htm |date=August 11, 2016 |access-date=August 13, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524001228/https://www.webcitation.org/6jjep6ec6?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608110000.htm |archive-date=May 24, 2024 }} During the next day, satellite image showed that the convective structure of Conson was beginning to deteriorate as it started to interact with drier air, suppressing convection.{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 18 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608121500.htm |date=August 12, 2016 |access-date=August 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524001427/https://www.webcitation.org/6jjfkEcXG?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608121500.htm |archive-date=May 24, 2024 }} The center of Conson became much broader and exposed early on August 13.{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 20 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608130300.htm |date=August 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524001347/https://www.webcitation.org/6jjfiohwX?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608130300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} While moving northwestward, Conson became better defined than before, however its convection was more shallow as it started to interact will cooler sea-surface temperatures and drier air.{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 22 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608131500.htm |date=August 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524001307/https://www.webcitation.org/6jjfhQAZ7?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608131500.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} By August 14, the JTWC issued their final warning on Conson as it started to undergo its extratropical transition with a result of a strong wind shear and the interaction of the mid-latitude baroclinic zone.{{cite web |title=PROGNOSITC REASONING FOR TROPICAL STORM 08W (CONSON) NR 25 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608140900.htm |date=August 14, 2016 |access-date=August 15, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524001912/https://www.webcitation.org/6jmE4zvDE?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608140900.htm |archive-date=May 24, 2024 }}{{cite web |title=TROPICAL STORM 08W (CONSON) WARNING NR 026 |url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201608141500.htm |date=August 14, 2016 |access-date=August 15, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524001829/https://www.webcitation.org/6jmE0kQZK?url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201608141500.htm |archive-date=May 24, 2024 }} The JMA tracked Conson until it fully transitioned into an extratropical cyclone on August 15 and made landfall near Nemuro Peninsula. Its remnants were tracked until midday of August 16.

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 12

| Dissipated = August 17

| Image = Chanthu 2016-08-17 0355Z.jpg

| Track = Chanthu 2016 track.png

| 10-min winds = 55

| 1-min winds = 45

| Pressure = 980

}}

During August 11, the JMA started to track a tropical depression, whereas the JTWC issued a Tropical Cyclone Formation Alert, as it was located about {{convert|695|km|mi|abbr=on}} west-northwest of Guam.{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-11T06:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/11/marine-weather-warning-for-gmdss-metarea-xi-2016-08-11t060000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 11, 2016|date=August 11, 2016}}{{cite web |url=http://gwydir.demon.co.uk/advisories/WTPN21-PGTW_201608112130.htm# |title=Archived copy |access-date=2016-08-13 |archive-url=https://archive.today/20240524001630/https://www.webcitation.org/6jjgYoMmG?url=http://gwydir.demon.co.uk/advisories/WTPN21-PGTW_201608112130.htm |archive-date=2024-05-24 |url-status=dead }} After meandering eastwards, the JTWC designated the system as 09W, while the JMA immediately upgraded 09W to a tropical storm and assigned it the name Chanthu on August 13.{{cite web |title=Tropical Depression 09W (Nine) Warning Nr 001 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608130900.htm |date=August 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524001548/https://www.webcitation.org/6jjgcABDk?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608130900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite news |title=TS 1607 CHANTHU (1607) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608131800.htm |date=August 13, 2016 |access-date=August 15, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524001949/https://www.webcitation.org/6jmIgwnw0?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608131800.htm |archive-date=May 24, 2024 }} The JTWC followed suit early on August 14.{{cite web |title=Prognostic Reasoning for Tropical Storm 09W (Chanthu) Warning Nr 03 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608140300.htm |date=August 14, 2016 |access-date=August 15, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002150/https://www.webcitation.org/6jmK3zhUO?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608140300.htm |archive-date=May 24, 2024 }} With an improving LLCC, Chanthu rapidly developed into a severe tropical storm from the JMA,{{cite web |title=Prognostic Reasoning for Tropical Storm 09W (Chanthu) Warning Nr 06 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608141500.htm |date=August 14, 2016 |access-date=August 15, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002110/https://www.webcitation.org/6jmK3AWjM?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608141500.htm |archive-date=May 24, 2024 }}{{cite news |title=STS 1607 CHANTHU (1607) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608141800.htm |date=August 14, 2016 |access-date=August 15, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524002031/https://www.webcitation.org/6jmIqroLA?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608141800.htm |archive-date=May 24, 2024 }} as it was later located over in an area of favorable environments of strengthening.{{cite web |title=Prognostic Reasoning for Tropical Storm 09W (Chanthu) Warning Nr 09 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608150900.htm |date=August 15, 2016 |access-date=August 19, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002714/https://www.webcitation.org/6jsmt3zS4?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608150900.htm |archive-date=May 24, 2024 }} Despite a high chance of strengthening and a well-defined LLCC, Chanthu stopped generating convection as the JMA downgraded it to a tropical storm.{{cite web |title=Prognostic Reasoning for Tropical Storm 09W (Chanthu) Warning Nr 12 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608160300.htm |date=August 16, 2016 |access-date=August 19, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002634/https://www.webcitation.org/6jsms0etp?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608160300.htm |archive-date=May 24, 2024 }}{{cite news |title=TS 1607 CHANTHU (1607) DOWNGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608151800.htm |date=August 15, 2016 |access-date=August 17, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524002234/https://www.webcitation.org/6jq1l5f4L?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608151800.htm |archive-date=May 24, 2024 }}

Later that day, flaring convection was associated with its LLCC as it was beginning its extratropical transition while interacting with mid-latitude flow.{{cite web |title=Prognostic Reasoning for Tropical Storm 09W (Chanthu) Warning Nr 15 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608162100.htm |date=August 16, 2016 |access-date=August 19, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002553/https://www.webcitation.org/6jsmqx7yF?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608162100.htm |archive-date=May 24, 2024 }} Therefore, early on August 17, Chanthu once again reached severe tropical storm strength as it attained its peak intensity with a minimal pressure of 980 millibars (28.94 inHg), while east of the Japanese archipelago of Honshu.{{cite news |title=STS 1607 CHANTHU (1607) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608141800.htm |date=August 17, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524002031/https://www.webcitation.org/6jmIqroLA?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201608141800.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Shortly thereafter, the JTWC issued its final warning on Chanthu.{{cite web |title=Tropical Storm 09W (Chanthu) Warning Nr 016 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608170300.htm |date=August 17, 2016 |access-date=August 19, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002754/https://www.webcitation.org/6jsmypDYz?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608170300.htm |archive-date=May 24, 2024 }} The JMA issued its final warning a few hours later as it made landfall over Cape Erimo of Hokkaido, Japan, at peak intensity.{{cite web|script-title=ja:平成２８年 台風第７号に関する情報 第４２号|url=http://www.jma.go.jp/jp/typh/D20160817084155748.html|agency=Japan Meteorological Agency|access-date=August 17, 2016|archive-url=https://web.archive.org/web/20160817085400/http://www.jma.go.jp/jp/typh/D20160817084155748.html|archive-date=August 17, 2016|language=ja|date=August 17, 2016}}

Agricultural damage in Japan were at ¥9.49 billion (US$94.7 million).{{cite news|url=http://www.maff.go.jp/j/saigai/typhoon/160816.html|script-title=ja:平成28年台風第7号による被害状況|language=ja|publisher=Ministry of Agriculture, Forestry and Fisheries|date=April 14, 2017|access-date=April 16, 2017}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 15

| Dissipated = August 20

| Image = Dianmu 2016-08-18 0610Z.jpg

| Track = Dianmu 2016 track.png

| 10-min winds = 40

| 1-min winds = 40

| Pressure = 980

}}

{{main|Tropical Storm Dianmu (2016)}}

On August 15, a tropical depression developed about {{convert|305|km|mi|round=5|abbr=on}} to the southeast of Hong Kong.{{cite report|title=Tropical Storm Dianmu |url=http://www.wis-jma.go.jp/cms/warning/2016/09/21/typhoon-best-track-2016-09-21t050000z/ |type=RSMC Tropical Cyclone Best Track |access-date=September 21, 2016 |date=September 21, 2016 |url-status=live |publisher=Japan Meteorological Agency |archive-url=https://archive.today/20240522100637/https://www.webcitation.org/6kge97bMz?url=http://gwydir.demon.co.uk/advisories/AXPQ20-RJTD_201609210400.htm |archive-date=May 22, 2024 }} During the course of August 17, enhanced satellite imagery showed that Dianmu was rapidly organizing with deep flaring convection surrounding its LLCC.{{cite web |title=Prognostic Reasoning for Tropical Depression 11W (Dianmu) Warning Nr 03 |url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201608181500.htm |date=August 18, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002434/https://www.webcitation.org/6jrRCPk9f?url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201608181500.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Dianmu made landfall in Haiphong and Thái Bình Province in northern Vietnam.{{cite web |title=Tropical Storm 11W (Dianmu) Warning Nr 006 |url=http://gwydir.demon.co.uk/advisories/WTPN33-PGTW_201608190900.htm |date=August 19, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002835/https://www.webcitation.org/6jsy0Dj7z?url=http://gwydir.demon.co.uk/advisories/WTPN33-PGTW_201608190900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite web|title=Tropical Storm Dianmu hits northern Vietnam|url=http://tuoitrenews.vn/society/36624/in-photos-tropical-storm-dianmu-hits-northern-vietnam|access-date=August 19, 2016|work=Tuổi Trẻ News|date=28 March 2013}} While overland, the system gradually weakened into a tropical depression, before it degenerated into an area of low pressure during August 20 while over Myanmar.

In the province of Hainan, China, Dianmu's heavy rains brought the water level at the Longtang Dam on the Nandu River to a ten-year high of 13.35 metres. Hainan's capital, Haikou, experienced flooding in some areas. Over in Quảng Ninh, a total of 11 houses were collapsed and total damages in the city amounted to 3.5 billion VND (US$157,000).{{cite web | url=http://www.phapluatplus.vn/quang-ninh-bao-so-3-da-gay-thiet-hai-35-ty-dong-d21824.html | title=Quảng Ninh: Bão số 3 đã gây thiệt hại 3,5 tỷ đồng }}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 17

| Dissipated = August 23

| Image = Mindulle 2016-08-22 0345Z.jpg

| Track = Mindulle 2016 track.png

| 10-min winds = 65

| 1-min winds = 65

| Pressure = 975

}}

{{Main|Typhoon Mindulle (2016)}}

A tropical depression formed northwest of Guam on August 17.{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-17T12:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/17/marine-weather-warning-for-gmdss-metarea-xi-2016-08-17t120000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 17, 2016|date=August 17, 2016}} On August 19, the system became a tropical storm and was named Mindulle early on August 19.{{cite web|title=RSMC Tropical Cyclone Advisory 190600 |url=http://weather.noaa.gov/pub/data/raw/wt/wtpq22.rjtd..txt |agency=Japan Meteorological Agency |access-date=August 22, 2016 |archive-url=https://archive.today/20240523100630/https://www.webcitation.org/6jsznjh8k?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201608190600.htm |archive-date=May 23, 2024 |date=August 19, 2016 |url-status=dead }} However, an upper-level low to the north and the predecessor of Tropical Storm Kompasu to the northeast were stifling the development of poleward outflow.{{cite web|title=Prognostic Reasoning for Tropical Storm 10W (Mindulle) Warning Nr 07 |url=http://weather.noaa.gov/pub/data/raw/wd/wdpn32.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=August 22, 2016 |archive-url=https://archive.today/20240523100708/https://www.webcitation.org/6jt0SiC3W?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608190900.htm |archive-date=May 23, 2024 |date=August 19, 2016 |url-status=dead }}

Moving on the eastern edge of a relatively high-latitude monsoon gyre and being steered by the southern extension of the subtropical ridge anchored east of Japan, the intensification of Mindulle was limited on August 20, owing to modest dry air entrainment resulting in flaring convection near and surrounding the LLCC.{{cite web|title=Prognostic Reasoning for Tropical Storm 10W (Mindulle) Warning Nr 11 |url=http://weather.noaa.gov/pub/data/raw/wd/wdpn32.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=August 22, 2016 |archive-url=https://archive.today/20240523100828/https://www.webcitation.org/6juZ6pvY6?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608200900.htm |archive-date=May 23, 2024 |date=August 20, 2016 |url-status=dead }} Although Mindulle became a severe tropical storm when it was approximately {{convert|380|km|abbr=on}} northwest of Chichi-jima at around 15:00 JST (06:00 UTC) on August 21, outflow from Tropical Storm Lionrock to the west was inhibiting further development, as the distance between their centers was only about {{convert|600|km|abbr=on}} at that time.{{cite web|title=RSMC Tropical Cyclone Advisory 210600|url=http://weather.noaa.gov/pub/data/raw/wt/wtpq22.rjtd..txt |agency=Japan Meteorological Agency |access-date=August 22, 2016 |archive-url=https://archive.today/20240523100948/https://www.webcitation.org/6jwBeBv5w?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201608210600.htm |archive-date=May 23, 2024 |date=August 21, 2016 |url-status=dead}}{{cite web|title=Prognostic Reasoning for Tropical Storm 10W (Mindulle) Warning Nr 15 |url=http://weather.noaa.gov/pub/data/raw/wd/wdpn32.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=August 22, 2016 |archive-url=https://archive.today/20240523101110/https://www.webcitation.org/6jwCAIQ7Z?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608202100.htm |archive-date=May 23, 2024 |date=August 21, 2016 |url-status=dead }} With warm sea surface temperatures of between {{convert|30|and|31|C|F|lk=in}}, good equatorward and poleward outflow channels, as well as low vertical wind shear, Mindulle became a typhoon at around 03:00 JST on August 22 (18:00 UTC on August 21), when the center was located about {{convert|40|km|abbr=on}} east of Hachijō-jima.{{cite web|title=Prognostic Reasoning for Tropical Storm 10W (Mindulle) Warning Nr 17|url=http://weather.noaa.gov/pub/data/raw/wd/wdpn32.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=August 22, 2016 |archive-url=https://archive.today/20240523101029/https://www.webcitation.org/6jwC8mU1I?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201608212100.htm |archive-date=May 23, 2024 |date=August 21, 2016 |url-status=dead}}{{cite web|title=RSMC Tropical Cyclone Advisory 211800 |url=http://weather.noaa.gov/pub/data/raw/wt/wtpq22.rjtd..txt |agency=Japan Meteorological Agency |access-date=August 22, 2016 |archive-url=https://archive.today/20240523100908/https://www.webcitation.org/6jwBcfIZo?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201608211800.htm |archive-date=May 23, 2024 |date=August 21, 2016 |url-status=dead }} At around 12:30 JST (03:30 UTC), Mindulle made landfall over the area near Tateyama, Chiba.{{cite web|script-title=ja:平成２８年 台風第９号に関する情報 第３７号|url=http://www.jma.go.jp/jp/typh/D20160822034309477.html|agency=Japan Meteorological Agency|access-date=August 22, 2016|archive-url=https://web.archive.org/web/20160822035530/http://www.jma.go.jp/jp/typh/D20160822034309477.html|archive-date=August 22, 2016|language=ja|date=August 22, 2016}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 17

| Dissipated = August 30

| Image = Lionrock 2016-08-28 0350Z.png

| Track = Lionrock 2016 track.png

| 10-min winds = 90

| 1-min winds = 120

| Pressure = 940

}}

{{Main|Typhoon Lionrock (2016)}}

{{See also|2016 North Korean floods}}

The system that was to become Typhoon Lionrock was first noted as a hybrid disturbance on August 15, while it was located about {{convert|585|km|mi|round=5|abbr=on}} to the west of Wake Island.{{cite web|archive-date=May 22, 2024 |agency=United States Joint Typhoon Warning Center |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans August 15, 2016 01z |url=http://weather.noaa.gov/pub/data/raw/ab/abpw10.pgtw..txt |url-status=live |archive-url=https://archive.today/20240522221021/https://www.webcitation.org/6jmcBz2d1?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201608150100.htm |access-date=August 27, 2016 }} It developed into a tropical depression about {{convert|690|km|abbr=on}} northwest of Wake Island on August 16.{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-16T12:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/16/marine-weather-warning-for-gmdss-metarea-xi-2016-08-16t120000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 16, 2016|date=August 16, 2016}} At this time the disturbance had a broad and poorly organized low level circulation centre, which had some shallow bands of atmospheric convection wrapping loosely around it. Over the next day, the system moved northwards, while a TUTT cell created subsidence and high vertical windshear over the system. The JTWC considered the system to be subtropical at this time, as its structure was asymmetric, with deep convection displaced to the north and east of the system's low level circulation centre.{{cite web |title=SUBJ/SIGNIFICANT TROPICAL WEATHER ADVISORY FOR THE WESTERN AND SOUTH PACIFIC OCEANS REISSUED/170200Z-170600ZAUG2016// |url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201608170200.htm |website=WebCite query |access-date=1 September 2016 |url-status=dead |archive-url=https://archive.today/20240523082853/https://www.webcitation.org/6jrT1PFju?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201608170200.htm |archive-date=23 May 2024 }} From late August 20 to early August 22, the system had at least somewhat an interaction with Mindulle, taking an erratic and slow path for a bit. Restrengthening begun again quickly, with the system already starting to develop an eye in mid-August 23. In the middle of the 24th of August the system reached an initial peak as a Category 3-equivalent storm.

Lionrock entered the Philippine Area of Responsibility on August 25, 2016, and PAGASA assigned Dindo {{cite web|url=http://newsinfo.inquirer.net/809209/pagasa-typhoon-dindo-enters-par-lpa-over-east-of-ph|title=Typhoon 'Dindo' enteres PAR, LPA Over East of PH|date=August 27, 2016|publisher=Inquirer.net|access-date=August 24, 2016}} as the local name, while Lionrock had begun an eyewall replacement cycle early that day, weakening to a Category 2-equivalent storm. After two days, early on August 26, it finally completed the eyewall replacement cycle, but slow restrengthening occurred. Another two days passed until it reached its full peak as a Category 4-equivalent storm, which rapid weakening ensued after. On August 29, Lionrock turned towards the northwest due to a high-pressure system located east of Japan, putting it on an towards the northeastern region of the country.{{cite web|title=Powerful Typhoon Likely to Slam Northeastern Japan|url=http://jen.jiji.com/jc/i?g=eco&k=2016082900539|website=JIJI.com|publisher=JIJI Press|access-date=30 August 2016}} Lionrock made landfall near Ōfunato, a city in Iwate Prefecture, Japan.{{cite web|script-title=ja:平成２８年 台風第１０号に関する情報 第１１５号|url=http://www.jma.go.jp/jp/typh/D20160830090017754.html|agency=Japan Meteorological Agency|access-date=August 30, 2016|archive-url=https://web.archive.org/web/20160830092234/http://www.jma.go.jp/jp/typh/D20160830090017754.html|archive-date=August 30, 2016|language=ja|date=August 30, 2016}} This made Lionrock the first tropical cyclone to make landfall over the Pacific coast of the Tōhoku region of Japan since the Japan Meteorological Agency began record-keeping in 1951.{{cite news|title=Typhoon Hits Northern Japan, Threatening to Bring Floods|url=https://www.nytimes.com/aponline/2016/08/30/world/asia/ap-as-asia-storm.html?_r=0|agency=Associated Press|work=The New York Times|access-date=30 August 2016}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 18

| Dissipated = August 21

| Image = Kompasu 2016-08-20 0105Z.jpg

| Track = Kompasu 2016 track.png

| 10-min winds = 35

| 1-min winds = 40

| Pressure = 994

}}

On August 18, the JMA started to monitor a tropical depression that had developed, about {{convert|1300|km|mi|round=5|abbr=on}} to the northeast of Guam.{{cite report|title=Tropical Storm Kompasu |url=http://www.wis-jma.go.jp/cms/warning/2016/09/27/typhoon-best-track-2016-09-27t070000z/ |access-date=September 27, 2016 |url-status=live |type=RSMC Tropical Cyclone Best Track |publisher=Japan Meteorological Agency |archive-url=https://archive.today/20240524005049/https://www.webcitation.org/6kpoCJgGr?url=http://gwydir.demon.co.uk/advisories/AXPQ20-RJTD_201609270700.htm |archive-date=May 24, 2024 |date=September 27, 2016 }} The JTWC started issuing advisories by the next day as it was immediately classified as a tropical storm and the identifier of 13W.{{cite web |title=Tropical Storm 13W (Thirteen) Warning Nr 001 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608192100.htm |date=August 19, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003036/https://www.webcitation.org/6juZnu1dB?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608192100.htm |access-date=May 22, 2017 }} The JMA followed suit early on August 20, and was named Kompasu. Despite wind shear and an exposed LLCC, tightly curved banding was reported embedded within the northern extent of a very broad "monsoon gyre" circulation.{{cite web |title=Prognostic Reasoning for Tropical Storm 13W (Thirteen) Warning Nr 02 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608200300.htm |date=August 20, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524002958/https://www.webcitation.org/6jua7bgul?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608200300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Both agencies reported that Kompasu had reached its peak strength as a minimal tropical storm with a minimum barometric pressure of about 994 mbar.{{cite web |title=TS 1611 KOMPASU (1611) |url=http://gwydir.demon.co.uk/advisories/WTPQ23-RJTD_201608201200.htm |date=August 20, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524003117/https://www.webcitation.org/6juZWPP64?url=http://gwydir.demon.co.uk/advisories/WTPQ23-RJTD_201608201200.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Later that day, deep convection of Kompasu had rapidly decreased as it was located in marginally favorable environments with low wind shear and sea-surface temperatures of about 26 degrees Celsius.{{cite web |title=Prognostic Reasoning for Tropical Storm 13W (Kompasu) Warning Nr 05 |date=August 20, 2016 |archive-date=May 24, 2024 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608202100.htm |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003237/https://www.webcitation.org/6jwBTYRuP?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608202100.htm |access-date=May 22, 2017 }} On August 21, the JTWC downgraded Kompasu to a tropical depression and issued their final bulletin on the system.{{cite web |title=Tropical Depression 13W (Kompasu) Warning Nr 006 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608210300.htm |date=August 21, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003201/https://www.webcitation.org/6jwBOWg0o?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608210300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} The JMA did the same and issued its final advisory on Kompasu as it transitioned into an extratropical system.

Floods in Hokkaidō killed one person when a driver was stranded in his flooded car.{{cite news|newspaper=Saudi Gazette|title=Typhoon dumps heavy rain on northern Japan|access-date=August 28, 2016|url=http://saudigazette.com.sa/world/asia/typhoon-dumps-heavy-rain-northern-japan/}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 23

| Dissipated = August 24

| Image = 14W 2016-08-23 0311Z.jpg

| Track = 14W 2016 track.png

| 10-min winds = 30

| 1-min winds = 40

| Pressure = 1002

}}

During August 23, Tropical Depression 14W developed about {{convert|75|km|mi|round=5|abbr=on}} to the east of Andersen Air Force Base, Guam.{{cite web |title=Tropical Depression 14W (Fourteen) Warning Nr 001 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608230900.htm |date=August 23, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003401/https://www.webcitation.org/6jzyvMSg8?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608230900.htm |access-date=May 22, 2017 }} Moving northward on the next day, the LLCC of 14W became exposed with a deteriorating convective signature.{{cite web |title=Prognostic Reasoning for Tropical Depression 14W (Fourteen) Warning Nr 04 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608240300.htm |date=August 24, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003518/https://www.webcitation.org/6jzz2UKXW?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608240300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Flaring deep convection became disorganized into a weakly-defined center due to strong northerly wind shear; the JTWC assessed 14W's winds only at 25 knots.{{cite web |title=Prognostic Reasoning for Tropical Depression 14W (Fourteen) Warning Nr 05 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608240900.htm |date=August 24, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003437/https://www.webcitation.org/6jzz24oEz?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201608240900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Due to a rapidly decaying LLCC with minor bursts of convection, both the JMA and the JTWC issued its final warning on 14W later that same day.{{cite web |title=Tropical Depression 14W (Fourteen) Warning Nr 006 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608241500.htm |date=August 24, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003638/https://www.webcitation.org/6k1XNm9Ez?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608241500.htm |access-date=May 22, 2017 }}{{cite web |title=TD |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608240900.htm |date=August 24, 2016 |archive-date=May 24, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524003720/https://www.webcitation.org/6k1XRi8La?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201608240900.htm |access-date=May 22, 2017 }}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = August 31

| Dissipated = September 5

| Image = Namtheun 2016-09-02 0215Z.jpg

| Track = Namtheun 2016 track.png

| 10-min winds = 70

| 1-min winds = 100

| Pressure = 955

}}

A low-pressure area developed into a tropical depression southeast of Taiwan early on August 31.{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-31T00:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/31/marine-weather-warning-for-gmdss-metarea-xi-2016-08-31t000000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 31, 2016|date=August 31, 2016|archive-url=https://web.archive.org/web/20160918212402/http://www.wis-jma.go.jp/cms/warning/2016/08/31/marine-weather-warning-for-gmdss-metarea-xi-2016-08-31t000000z/|archive-date=2016-09-18|url-status=dead}} Later that day, the JTWC began issuing advisories on the system, assigning the designation of 15W.{{cite web |title=Tropical Depression 15W (Fifteen) Warning Nr 001 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608311500.htm |date=August 31, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003801/https://www.webcitation.org/6kB1WXW4W?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201608311500.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Early the next day, 15W had intensified into a tropical storm by both agencies, with the JMA prompting the name Namtheun.{{cite web |title=TS 1612 NAMTHEUN (1612) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609010000.htm |date=September 1, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524003839/https://www.webcitation.org/6kC6kg141?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609010000.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite web |title=Tropical Storm 15W (Namtheun) Warning Nr 004 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201609010900.htm |date=September 1, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524003924/https://www.webcitation.org/6kC6stV5d?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201609010900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} The PAGASA however started issuing advisories on Namtheun and considered it as a tropical depression and gave the local name Enteng.{{cite web|title=LPA develops into tropical depression|url=http://www.philstar.com/headlines/2016/09/01/1619404/lpa-develops-tropical-depression|date=September 1, 2016|publisher=Philstar}} Despite the overall structure of the storm being described to be "midget" with a very small but compact LLCC, Namtheun had begun a phase of rapid intensification and a pinhole eye developed; therefore, the JTWC upgraded Namtheun to a Category 1 typhoon.{{cite web |title=Prognostic Reasoning for Typhoon 15W (Namtheun) Warning Nr 05 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609011500.htm |date=September 1, 2016 |access-date=September 2, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524004242/https://www.webcitation.org/6kELD6BR0?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609011500.htm |archive-date=May 24, 2024 }} The JMA, though, upgraded Namtheun only to a severe tropical storm at that time.{{cite web |title=STS 1612 NAMTHEUN (1612) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609011200.htm |date=September 1, 2016 |access-date=September 2, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524004040/https://www.webcitation.org/6kEKkoVK7?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609011200.htm |archive-date=May 24, 2024 }} Later that day, PAGASA had declared that the storm had exited its area of responsibility as a severe tropical storm.{{cite web|title=Severe Tropical Storm Enteng leaves PAR|url=http://www.rappler.com/nation/special-coverage/weather-alert/144925-20160901-severe-tropical-storm-enteng-pagasa-forecast-1030pm|date=September 1, 2016|publisher=Rappler}}

By September 2, rapid intensification ensued as it was reported that Namtheun was located over a region of warm sea surface temperatures of 30 degrees Celsius with high ocean heat content,{{cite web |title=Prognostic Reasoning for Typhoon 15W (Namtheun) Warning Nr 07 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609020300.htm |date=September 2, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524004202/https://www.webcitation.org/6kELC26rf?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609020300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} therefore prompting the JMA to classify it to a typhoon.{{cite web |title=TY 1612 NAMTHEUN (1612) UPGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609020000.htm |date=September 2, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524004000/https://www.webcitation.org/6kEKilEKa?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609020000.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Namtheun developed a pinhole eye {{convert|8|nmi|abbr=on}} across and reached its peak strength as a Category 3 typhoon with 1-minute sustained winds of {{convert|185|km/h|abbr=on}}; the JMA though declared its 10-minute peak strength early on September 3 with a minimum barometric pressure of 955 millibars.{{cite web |title=Prognostic Reasoning for Typhoon 15W (Namtheun) Warning Nr 09 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609021500.htm |date=September 2, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524004121/https://www.webcitation.org/6kELAwu1S?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609021500.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite web|title=TY 1612 NAMTHEUN (1612)|date=September 3, 2016|agency=Japan Meteorological Agency}} By that time, Namtheun was depicted with significantly weakened structure and a dissipation of its eye, therefore the JTWC downgraded Namtheun rapidly to a strong Category 1.{{cite web |title=Prognostic Reasoning for Typhoon 15W (Namtheun) Warning Nr 12 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609030900.htm |date=September 3, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524004322/https://www.webcitation.org/6kFcdwm9B?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609030900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} On September 4, Namtheun had weakened to a tropical storm due to diminishing convection, caused by high southwesterly wind shear.{{cite web |title=Prognostic Reasoning for Tropical Storm 15W (Namtheun) Warning Nr 16 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609040900.htm |date=September 4, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524004403/https://www.webcitation.org/6kH6FwRsN?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609040900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} After making landfall over in Nagasaki, Kyushu, both the JMA and JTWC issued its final advisory as a tropical depression early on September 5.{{cite web |title=Tropical Depression 15W (Namtheun) Warning Nr 019 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201609050300.htm |date=September 5, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524004523/https://www.webcitation.org/6kIhMJyKB?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201609050300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite web |title=TD DOWNGRADED FROM TS 1612 NAMTHEUN (1612) |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609050000.htm |date=September 5, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524004442/https://www.webcitation.org/6kIhFrcBR?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609050000.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = September 5

| Dissipated = September 7

| Image = Malou 2016-09-06 0500Z.jpg

| Track = Malou 2016 track.png

| 10-min winds = 40

| Pressure = 1000

}}

On September 5, the JMA started to monitor a tropical depression, that had developed over the Japanese prefecture of Okinawa.{{cite web|title=Tropical Cyclone Advisory for Analysis and Forecast September 5, 2016 12z |url=http://www.wis-jma.go.jp/cms/warning/2016/09/05/tropical-cyclone-advisory-for-analysis-and-forecast-2016-09-05t120000z/ |agency=Japan Meteorological Agency |access-date=September 5, 2016 |date=September 5, 2016 |archive-url=https://archive.today/20240524004603/https://www.webcitation.org/6kIhqACjQ?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609051200.htm |archive-date=May 24, 2024 |url-status=live }} The depression was located within a favourable environment for further development, with very warm sea surface temperatures and low vertical wind shear. Over the next day the system moved north-eastwards towards the Japanese Mainland, before it was classified as a tropical storm and named Malou by the JMA during September 6.{{cite web|agency=Japan Meteorological Agency |title=Tropical Cyclone Advisory for Analysis and Forecast September 6, 2016 00z |url=http://www.wis-jma.go.jp/cms/warning/2016/09/05/tropical-cyclone-advisory-for-analysis-and-forecast-2016-09-06t000000z/ |date=September 6, 2016 |archive-date=May 24, 2024 |archive-url=https://archive.today/20240524004725/https://www.webcitation.org/6kLUX3c44?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609060000.htm |url-status=dead }} However, the JTWC classified Malou as a hybrid system, with both subtropical and tropical characteristics.{{cite web|title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans July 14, 2016 06z |agency=United States Joint Typhoon Warning Center |archive-url=https://archive.today/20240524004647/https://www.webcitation.org/6kLSukHBL?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201609060200.htm |url=https://metoc.ndbc.noaa.gov/jtwc |archive-date=May 24, 2024 |date=July 14, 2016 |url-status=dead }} They also noted that the convective development around the system's low level circulation centre was being hindered, as the subtropical westerlies were located over the system. During September 7, the system started to accelerate northwards, before the JMA issued their final advisory on the system as Malou became an extratropical cyclone.{{cite web|agency=Japan Meteorological Agency |title=Tropical Cyclone Advisory for Analysis and Forecast September 7, 2016 18z |url=http://www.wis-jma.go.jp/cms/warning/2016/09/07/tropical-cyclone-advisory-for-analysis-and-forecast-2016-09-07t180000z/ |date=September 7, 2016 |archive-date=May 24, 2024 |archive-url=https://archive.today/20240524004843/https://www.webcitation.org/6kND9FH46?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609071800.htm |url-status=dead }}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = September 8

| Dissipated = September 16

| Image = Meranti 2016-09-13 0800Z.jpg

| Track = Meranti 2016 path.png

| 10-min winds = 120

| 1-min winds = 170

| Pressure = 890

}}

{{Main|Typhoon Meranti}}

On September 8, a tropical depression formed{{cite web|title=RSMC Tropical Cyclone Advisory |agency=Japan Meteorological Agency |access-date=September 12, 2016 |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609091800.htm |archive-url=https://archive.today/20240523095746/https://www.webcitation.org/6kOn9Edr2?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201609081800.htm |archive-date=May 23, 2024 |url-status=dead }} in a region of low wind shear, steered by ridges to the north and southwest, with warm water temperatures and outflow from the south.{{cite report|archive-url=https://archive.today/20240523095712/https://www.webcitation.org/6kOmybnCP?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609082100.htm |archive-date=May 23, 2024 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609082100.htm |title=Prognostic Reasoning for Tropical Depression 16W (Sixteen) Warning NR 001 |publisher=Joint Typhoon Warning Center |date=September 8, 2016 |access-date=September 12, 2016 |url-status=dead }} The system reached tropical storm strength by 06:00 UTC on September 10, receiving the name Meranti.{{cite web|title=TS 1614 (Meranti) Upgraded from TD |agency=Japan Meteorological Agency |access-date=September 12, 2016 |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609100600.htm |archive-url=https://archive.today/20240523095824/https://www.webcitation.org/6kQ6UxfVw?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609100600.htm |archive-date=May 23, 2024 |url-status=dead }}

Rainbands and a central dense overcast continued to evolve as the wind shear decreased.{{cite report|archive-url=https://archive.today/20240523095633/https://www.webcitation.org/6kOmxIzDr?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609091500.htm |archive-date=May 23, 2024 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609091500.htm |title=Prognostic Reasoning for Tropical Storm 16W (Meranti) Warning NR 009 |publisher=Joint Typhoon Warning Center |date=September 10, 2016 |access-date=September 12, 2016 |url-status=dead }} By early on September 12, Meranti reached typhoon status.{{cite web|title=TY 1614 (Meranti) Upgraded from TS |agency=Japan Meteorological Agency |access-date=September 12, 2016 |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609110600.htm |archive-url=https://archive.today/20240523095945/https://www.webcitation.org/6kRpOANwq?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609110600.htm |archive-date=May 23, 2024 |url-status=dead }} A small eye {{convert|9|km|abbr=on}} across developed within the spiraling thunderstorms, and Meranti started rapidly intensifying.{{cite report|archive-url=https://archive.today/20240523100146/https://www.webcitation.org/6kSzUrVXt?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609120300.htm |archive-date=May 23, 2024 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609120300.htm |title=Prognostic Reasoning for Typhoon 16W (Meranti) Warning NR 014 |publisher=Joint Typhoon Warning Center |date=September 12, 2016 |access-date=September 12, 2016 |url-status=dead }}

Meranti quickly attained estimated 1-minute sustained winds of {{convert|285|km/h|mph|abbr=on|round=10}}, equivalent to Category 5 on the Saffir–Simpson scale.{{cite report|archive-url=https://archive.today/20240523100426/https://www.webcitation.org/6kUmUUZ6v?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609121500.htm |archive-date=May 23, 2024 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609121500.htm |title=Prognostic Reasoning for Typhoon 16W (Meranti) Warning NR 016 |publisher=Joint Typhoon Warning Center |date=September 12, 2016 |access-date=September 12, 2016 |url-status=dead }} Meranti gradually reached its peak intensity on September 13 while passing through the Luzon Strait. The JMA estimated peak 10-minute sustained winds of {{convert|220|km/h|mph|abbr=on|round=10}} and a minimum barometric pressure of 890 hPa (mbar; 26.28 inHg),{{cite web|url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609131200.htm |archive-url=https://archive.today/20240523100306/https://www.webcitation.org/6kUm9MuAy?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609131200.htm |archive-date=May 23, 2024 |title=RSMC Tropical Cyclone Advisory |publisher=Japan Meteorological Agency |date=September 13, 2016 |access-date=September 17, 2016 |url-status=dead }} while the JTWC estimated peak 1-minute sustained winds of {{convert|315|km/h|mph|abbr=on|round=5}}. Based on the JMA pressure estimate, Meranti was among the most intense tropical cyclones. The JTWC wind estimate made Meranti the strongest tropical cyclone worldwide in 2016, surpassing Cyclone Winston, which had winds of {{convert|285|km/h|mph|abbr=on|round=10}} when it struck Fiji in February.{{cite web|author=Bob Hensen|author2=Jeff Masters|title=Taiwan, China Brace for Cat 5 Meranti; TS Ian Churns Through Open Atlantic|publisher=WeatherUnderground|access-date=September 13, 2016|date=September 13, 2016|url=https://www.wunderground.com/blog/JeffMasters/taiwan-china-brace-for-cat-5-meranti-ts-ian-churns-through-open-atla}}

Late on September 13, the storm made landfall on the {{convert|83|km2|abbr=on}} island of Itbayat in the Philippine province of Batanes while near its peak intensity.{{cite news|last1=Smith|first1=Nicola|title=Typhoon Meranti: fears for tiny Philippine island in eye of a megastorm|url=https://www.theguardian.com/world/2016/sep/14/typhoon-meranti-megastorm-philippine-island-eye-storm-itbayat|access-date=14 September 2016|work=The Guardian|date=14 September 2016|location=Taipei}} At around 03:05 CST on September 15 (19:05 UTC on September 14), Meranti made landfall over Xiang'an District, Xiamen in Fujian, China with measured 2-minute sustained winds of {{convert|173|km/h|mph|abbr=on}},{{cite web|script-title=zh:中央气象台15日3时20分发布台风登陆消息|url=http://www.nmc.cn/publish/typhoon/warning.html|publisher=National Meteorological Center|access-date=September 14, 2016|archive-url=https://web.archive.org/web/20160914193505/http://www.nmc.cn/publish/typhoon/warning.html|archive-date=September 14, 2016|language=zh|date=September 14, 2016}} making it the strongest typhoon to ever make landfall in China's Fujian Province.{{cite web|title=Typhoon Meranti lashes China after pounding Taiwan|url=http://www.seychellesnewsagency.com/articles/5920/Typhoon+Meranti+lashes+China+after+pounding+Taiwan|website=Seychelles News|agency=Agence France-Presse|access-date=15 September 2016}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = September 10

| Dissipated = September 12

| Image = 17W 2016-09-11 0345Z.jpg

| Track = 17W 2016 track.png

| Type1 = nwpdepression

| 1-min winds = 35

| Pressure = 1008

}}

During September 8, the JTWC started to monitor a tropical disturbance that had developed about {{convert|1210|km|mi|abbr=on|round=5}} to the west of Iwo To.https://www.webcitation.org/6kOnYNepD?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201609090300.htm Moving northward in a few days, the JTWC assessed that the system had strengthened into Tropical Depression 17W.{{cite web |title=Tropical Depression 17W (Seventeen) Waring Nr 001 |url=http://gwydir.demon.co.uk/advisories/WTPN52-PGTW_201609110300.htm |date=September 11, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005448/https://www.webcitation.org/6kSzh0tuz?url=http://gwydir.demon.co.uk/advisories/WTPN52-PGTW_201609110300.htm |access-date=May 22, 2017 }} Despite its LLCC remaining small, satellite imagery showed that 17W produced persistent convection and some spiral banding.{{cite web |title=Prognostic Reasoning for Tropical Depression 17W (Seventeen) Waring Nr 02 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201609110900.htm |date=September 11, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005606/https://www.webcitation.org/6kSzpiD1x?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201609110900.htm |access-date=May 22, 2017 }} Later, drier air surrounded the depression as it was now firmly embedded with the west-southwesterly flow ahead of the mid-latitude frontal zone.{{cite web |title=Prognostic Reasoning for Tropical Depression 17W (Seventeen) Waring Nr 03 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201609111500.htm |date=September 11, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005527/https://www.webcitation.org/6kSzpFNGq?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201609111500.htm |access-date=May 22, 2017 }} The JTWC issued their final advisory on 17W on September 12, as the system was rapidly deteriorating due to vertical wind shear, and weakened into a remnant low.{{cite web |title=Tropical Depression 17W (Seventeen) Waring Nr 004 |url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201609112100.htm |date=September 11, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005408/https://www.webcitation.org/6kSzdRyYv?url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201609112100.htm |access-date=May 22, 2017 }} {{citation needed span|Its remnants was later absorbed by a front near the International Date Line, late on September 14.|date=September 2016}}

In the JMA's post-analysis, 17W was recognized as a tropical depression, and the system was first noted on September 10.{{cite web|script-title=ja:日々の天気図 2016年9月|url=http://www.data.jma.go.jp/fcd/yoho/data/hibiten/2016/201609.pdf|publisher=Japan Meteorological Agency|access-date=December 22, 2016|language=ja}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = September 11

| Dissipated = September 13

| Image = Rai 2016-09-13 0340Z.jpg

| Track = Rai 2016 track.png

| 10-min winds = 35

| 1-min winds = 30

| Pressure = 996

}}

{{main|Tropical Storm Rai (2016)}}

On September 11, a tropical depression formed within an unfavourable environment for further development, about {{convert|860|km|mi|round=5|abbr=on}} to the northeast of Ho Chi Minh City, Vietnam.{{cite report|title=Tropical Storm Rai|type=RSMC Tropical Cyclone Best Track |url=http://www.wis-jma.go.jp/cms/warning/2016/10/24/typhoon-best-track-2016-10-24t000000z/ |access-date=October 30, 2016 |archive-date=May 23, 2024 |date=October 24, 2016 |publisher=Japan Meteorological Agency |archive-url=https://archive.today/20240523005813/https://www.webcitation.org/6lUgqdJCy?url=http://gwydir.demon.co.uk/advisories/AXPQ20-RJTD_201610240000.htm |url-status=live}}{{cite web|title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans September 11, 2016 00z |agency=United States Joint Typhoon Warning Center |date=September 11, 2016 |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |archive-url=https://archive.today/20240523005138/https://www.webcitation.org/6kRr8IPPR?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201609110000.htm |archive-date=May 23, 2024 |url-status=dead }} Satellite imagery then showed that the LLCC of 19W was broad and defined with some deep convective banding.{{cite web |title=Prognostic Reasoning for Tropical Depression 19W (Nineteen) Warning Nr 01 |url=http://gwydir.demon.co.uk/advisories/WDPN34-PGTW_201609120300.htm |date=September 12, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523005402/https://www.webcitation.org/6kT1Vas03?url=http://gwydir.demon.co.uk/advisories/WDPN34-PGTW_201609120300.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} Its LLCC became exposed, though its deep convection remained in place.{{cite web |title=Prognostic Reasoning for Tropical Depression 19W (Nineteen) Warning Nr 02 |url=http://gwydir.demon.co.uk/advisories/WDPN34-PGTW_201609120900.htm |date=September 12, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523005450/https://www.webcitation.org/6kT1VEz10?url=http://gwydir.demon.co.uk/advisories/WDPN34-PGTW_201609120900.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} Although the JMA declared that 19W had strengthened into a tropical storm,{{cite web |title=TS 1615 RAI (1615) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609121800.htm |date=September 12, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523005732/https://www.webcitation.org/6kUoVPaJS?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609121800.htm |access-date=May 22, 2017 }} the JTWC deemed the system to not have reached tropical storm intensity. Rai made landfall over Central Vietnam, about {{convert|94|km|mi|abbr=on}} southeast of the city of Da Nang.{{cite web|title=Tropical Depression 19W (Rai) Warning Nr 004 |url=http://gwydir.demon.co.uk/advisories/WTPN34-PGTW_201609122100.htm |date=September 12, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523005532/https://www.webcitation.org/6kUojagRG?url=http://gwydir.demon.co.uk/advisories/WTPN34-PGTW_201609122100.htm |access-date=May 22, 2017}} Rai degraded to a tropical depression six hours later.{{cite web |title=TD DOWNGRADED FROM TS 1615 RAI (1615) |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609130600.htm |date=September 13, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523005611/https://www.webcitation.org/6kUoTjE82?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609130600.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }}

Heavy rains in Central Vietnam and Northern Thailand caused flooding and the bursting of the Bung River 2 hydroelectricity plant in Quảng Nam province of Vietnam, which released 28 million cubic meters of water and washed away 2 workers.{{cite web|url=http://www.worldbulletin.net/asia-pacific/177364/dam-burst-sweeps-2-people-away-in-vietnam|archive-url=https://web.archive.org/web/20160915171309/http://www.worldbulletin.net/asia-pacific/177364/dam-burst-sweeps-2-people-away-in-vietnam|url-status=usurped|archive-date=September 15, 2016|title=Dam burst sweeps 2 people away in Vietnam|date=September 14, 2016|website=World Bulletin|access-date=17 September 2016}} Four ships were sunk along central Vietnam's coastline and 2 others were left stranded, while 5 houses were completely destroyed and 275 others had their roofs torn off.{{cite web|url=http://tuoitrenews.vn/society/37043/7-injured-280-houses-damaged-as-storm-rai-crosses-central-vietnam|title=7 injured, 280 houses damaged as Storm Rai crosses central Vietnam|date=September 14, 2016|access-date=September 17, 2016|newspaper=Tuổi Trẻ}} Most of the damage occurred in Nghệ An Province due to flooding, amounting to about ₫748 billion (US$33.6 million).{{cite web | url=http://www.tienphong.vn/xa-hoi/nghe-an-thiet-hai-nang-do-mua-lu-6-nguoi-chet-va-mat-tich-1053576.tpo | title=Nghệ an thiệt hại nặng do mưa lũ, 6 người chết và mất tích | date=22 September 2016 }} In total, Rai caused 12 deaths and damages amounting to ₫825 billion (US$37 million).{{cite web | url=http://vov.vn/tin-24h/bao-so-4-khien-12-nguoi-chet-27-nguoi-bi-thuong-551185.vov | title=Bão số 4 khiến 12 người chết, 27 người bị thương | date=17 September 2016 }}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = September 11

| Dissipated = September 20

| Image = Malakas 2016-09-16 1755Z.jpg

| Track = Malakas 2016 track.png

| 10-min winds = 95

| 1-min winds = 115

| Pressure = 930

}}

{{main|Typhoon Malakas (2016)}}

On September 11, a tropical depression formed approximately {{convert|36|mi|abbr=on|order=flip}} south of Hagåtña, Guam.https://www.webcitation.org/6kT0mULka?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201609110600.htm {{cite web |title=Tropical Depression 18W (Eighteen) Warning Nr 001 |url=http://gwydir.demon.co.uk/advisories/WTPN33-PGTW_201609112100.htm |date=September 11, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523083818/https://www.webcitation.org/6kSzzAn0o?url=http://gwydir.demon.co.uk/advisories/WTPN33-PGTW_201609112100.htm |access-date=May 22, 2017 }} On becoming a tropical storm, it was named Malakas.{{cite web |title=TS 1616 MALAKAS (1616) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609121800.htm |date=September 12, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523084103/https://www.webcitation.org/6kUnSIVXS?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609121800.htm |access-date=May 22, 2017 }} By September 13, Malakas had improved in its organization and became a severe tropical storm thereafter.{{cite web |title=STS 1616 MALAKAS (1616) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609131200.htm |date=September 13, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523084023/https://www.webcitation.org/6kUnQ4eP8?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609131200.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} At the same time, Malakas had entered the Philippine area of Responsibility, with PAGASA assigning the local name Gener.{{cite web |title=Severe Weather Bulletin #1: Severe Tropical Storm "GENER" (MALAKAS) |url=http://pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins |date=September 13, 2016 |agency=PAGASA |url-status=dead |archive-url=https://web.archive.org/web/20160831165623/http://pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins |archive-date=August 31, 2016 |access-date=December 5, 2016 }} Despite hindrance by the outflow of nearby Typhoon Meranti,{{cite web |title=Prognostic Reasoning for Tropical Storm 18W (Malakas) Warning Nr 08 |url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609131500.htm |date=September 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523084147/https://www.webcitation.org/6kUnxVohY?url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609131500.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} Malakas intensified into a typhoon.{{cite web |title=TY 1616 MALAKAS (1616) UPGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609131800.htm |date=September 13, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523084305/https://www.webcitation.org/6kWMrgLIO?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609131800.htm |access-date=May 22, 2017 }}

On September 16, Malakas rapidly intensified into a Category 4 typhoon.{{cite web |title=Prognostic Reasoning for Typhoon 18W (Malakas) Warning Nr 21 |url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609162100.htm |date=September 16, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523083701/https://www.webcitation.org/6kgZG7ZKh?url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609162100.htm |access-date=May 22, 2017 }} Malakas reached its peak intensity with 1-minute sustained winds of {{convert|215|km/h|mph|abbr=on|round=5}}, 10-minute sustained winds of {{convert|175|km/h|mph|abbr=on|round=5}}, and a pressure of {{convert|930|hPa|inHg|sigfig=4|abbr=on}} by the following day.{{cite web|title=TY 1616 MALAKAS (1616) |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609170000.htm |date=September 17, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523083216/https://www.webcitation.org/6kgYXkVUT?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609170000.htm |access-date=May 22, 2017}} Shortly thereafter, its eye became cloud-filled and ragged, signalling the onset of weakening.{{cite web |title=Prognostic Reasoning for Typhoon 18W (Malakas) Warning Nr 22 |url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609170300.htm |date=September 17, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523083619/https://www.webcitation.org/6kgZFZgAx?url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609170300.htm |access-date=May 22, 2017 }} After weakening to a Category 2 typhoon,{{cite web |title=Prognostic Reasoning for Typhoon 18W (Malakas) Warning Nr 25 |url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609172100.htm |date=September 17, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523083545/https://www.webcitation.org/6kgZEBrFa?url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609172100.htm |access-date=May 22, 2017 }} Malakas reintensified to a Category 3 typhoon by September 19.{{cite web |title=Prognostic Reasoning for Typhoon 18W (Malakas) Warning Nr 30 |url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609190300.htm |date=September 19, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523083418/https://www.webcitation.org/6kgZBgxGv?url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609190300.htm |access-date=May 22, 2017 }} Malakas then resumed weakening due to land interaction with Japan.{{cite web |title=Prognostic Reasoning for Typhoon 18W (Malakas) Warning Nr 32 |url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609191500.htm |date=September 19, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523083340/https://www.webcitation.org/6kgZAv8WD?url=http://gwydir.demon.co.uk/advisories/WDPN33-PGTW_201609191500.htm |access-date=May 22, 2017 }} By the following day, Malakas weakened below typhoon intensity,{{cite web |title=STS 1616 MALAKAS (1616) DOWNGRADED FROM TY |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609200600.htm |date=September 20, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523083057/https://www.webcitation.org/6kgYNpmGx?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609200600.htm |access-date=May 22, 2017 }} and became extratropical.{{cite web |title=DEVELOPED LOW FORMER 1616 MALAKAS (1616) |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609201200.htm |date=September 20, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523083014/https://www.webcitation.org/6kgYMylbQ?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201609201200.htm |access-date=May 22, 2017 }}

At around 00:00 JST on September 20 (15:00 UTC on September 19), Malakas made landfall over the Ōsumi Peninsula in Japan.{{cite web|script-title=ja:平成２８年 台風第１６号に関する情報 第８９号|url=http://www.jma.go.jp/jp/typh/D20160919151659763.html|agency=Japan Meteorological Agency|access-date=September 19, 2016|archive-url=https://web.archive.org/web/20160919170732/http://www.jma.go.jp/jp/typh/D20160919151659763.html|archive-date=September 19, 2016|language=ja|date=September 19, 2016}} It subsequently crossed Cape Muroto at around 11:00 JST (02:00 UTC) and made landfall over Tanabe at around 13:30 JST (04:30 UTC).{{cite web|script-title=ja:平成２８年 台風第１６号に関する情報 第１０２号|url=http://www.jma.go.jp/jp/typh/D20160920021557204.html|publisher=Japan Meteorological Agency|access-date=September 20, 2016|archive-url=https://web.archive.org/web/20160920140814/http://www.jma.go.jp/jp/typh/D20160920021557204.html|archive-date=September 20, 2016|language=ja|date=September 20, 2016}}{{cite web|script-title=ja:平成２８年 台風第１６号に関する情報 第１０６号|url=http://www.jma.go.jp/jp/typh/D20160920043746020.html|publisher=Japan Meteorological Agency|access-date=September 20, 2016|archive-url=https://web.archive.org/web/20160920140910/http://www.jma.go.jp/jp/typh/D20160920043746020.html|archive-date=September 20, 2016|language=ja|date=September 20, 2016}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = September 22

| Dissipated = September 29

| Image = Megi 2016-09-27 0525Z.jpg

| Track = Megi 2016 track.png

| 10-min winds = 85

| 1-min winds = 115

| Pressure = 945

}}

{{Main|Typhoon Megi (2016)}}

Megi originated as a tropical depression about {{convert|722|km|mi|abbr=on}} east-southeast of Guam on September 21.https://www.webcitation.org/6kgaB6tfZ?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609210000.htm https://www.webcitation.org/6kga5ZbMs?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201609210600.htm The depression became a tropical storm by on September 23.{{cite web|title=TS 1617 MEGI (1617) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609230000.htm |date=September 23, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240527233431/https://www.webcitation.org/6kjY4OhVB?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609230000.htm |archive-date=May 27, 2024 |access-date=May 22, 2017}} On the following day, Megi intensified to a severe tropical storm.{{cite web |title=STS 1617 MEGI (1617) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609231800.htm |date=September 23, 2016 |archive-date=September 24, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://www.webcitation.org/6kkxrMMo1?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609231800.htm |access-date=May 22, 2017 }} On developing an eye, Megi reached typhoon intensity.{{cite web|title=Prognostic Reasoning for Typhoon 20W (Megi) Warning Nr 07 |url=http://tgftp.nws.noaa.gov/data/raw/wd/wdpn31.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=September 27, 2016 |archive-url=https://archive.today/20240524004805/https://www.webcitation.org/6kmm52147?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609241500.htm |archive-date=May 24, 2024 |date=September 24, 2016 |url-status=dead }}{{cite web |title=TY 1617 MEGI (1617) UPGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609240600.htm |date=September 23, 2016 |archive-date=September 24, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://www.webcitation.org/6kkxpyosS?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609240600.htm |access-date=May 22, 2017 }} Shortly thereafter, Megi entered PAGASA's area of responsibility, and the local name Helen was assigned.{{cite web|title=Severe Weather Bulletin #1|url=http://www.pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/25-tropical-cyclones/2546-1-2|publisher=PAGASA|access-date=September 27, 2016|archive-url=https://web.archive.org/web/20160927164343/http://www.pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/25-tropical-cyclones/2546-1-2|archive-date=September 27, 2016|date=September 24, 2016}} After a day of slight intensification, Megi started to undergo an eyewall replacement cycle. From then on, Megi rapidly intensified as it neared the coast of Taiwan.{{cite web|title=Prognostic Reasoning for Typhoon 20W (Megi) Warning Nr 15 |url=http://tgftp.nws.noaa.gov/data/raw/wd/wdpn31.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=September 27, 2016 |archive-url=https://archive.today/20240524005249/https://www.webcitation.org/6kq4VYzeS?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609261500.htm |archive-date=May 24, 2024 |date=September 26, 2016 |url-status=dead }}{{cite web|title=Prognostic Reasoning for Typhoon 20W (Megi) Warning Nr 16 |url=http://tgftp.nws.noaa.gov/data/raw/wd/wdpn31.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=September 27, 2016 |archive-url=https://archive.today/20240524005206/https://www.webcitation.org/6kq4UqCgL?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609262100.htm |archive-date=May 24, 2024 |date=September 26, 2016 |url-status=dead }} Megi reached peak intensity as a Category 3 typhoon over Taiwan with 1-minute sustained winds of {{convert|205|km/h|mph|abbr=on|round=5}}, 10-minute sustained winds of {{convert|155|km/h|mph|abbr=on|round=5}}, and a minimum barometric pressure of 945 mbar late on September 26.{{cite web|title=RSMC Tropical Cyclone Advisory 261800 |url=http://tgftp.nws.noaa.gov/data/raw/wt/wtpq20.rjtd..txt |publisher=Japan Meteorological Agency |access-date=September 27, 2016 |archive-url=https://archive.today/20240523093658/https://www.webcitation.org/6kq4Hyl7g?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201609261800.htm |archive-date=May 23, 2024 |date=September 26, 2016 |url-status=dead }} Early on September 27, Megi made landfall over Hualien City,{{cite web|script-title=zh:海上陸上颱風警報第14報|url=http://cwb.gov.tw/V7/prevent/warning/w21.htm|publisher=Central Weather Bureau|access-date=September 27, 2016|archive-url=https://web.archive.org/web/20160927062841/http://cwb.gov.tw/V7/prevent/warning/w21.htm|archive-date=September 27, 2016|language=zh|date=September 27, 2016}} weakening due to land interaction.{{cite web|title=Prognostic Reasoning for Typhoon 20W (Megi) Warning Nr 19 |url=http://tgftp.nws.noaa.gov/data/raw/wd/wdpn31.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=September 27, 2016 |archive-url=https://archive.today/20240524005126/https://www.webcitation.org/6kq4TlADo?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201609271500.htm |archive-date=May 24, 2024 |date=September 27, 2016 |url-status=dead }} Megi made landfall over in Hui'an County of Quanzhou the next day.{{cite web|script-title=zh:台风"鲇鱼"已登陆福建 福建浙江台湾出现强风雨 闽浙赣粤等地将有暴雨或大暴雨|url=http://www.nmc.cn/publish/weather-bulletin/index.htm|publisher=National Meteorological Center|access-date=September 28, 2016|archive-url=https://web.archive.org/web/20160928015429/http://www.nmc.cn/publish/weather-bulletin/index.htm|archive-date=September 28, 2016|language=zh|date=September 28, 2016}} Megi continued deteriorating as it moved inland.{{cite web |title=Typhoon 20W (Megi) Warning Nr 020 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201609272100.htm |date=September 27, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005329/https://www.webcitation.org/6krPtTNee?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201609272100.htm |access-date=May 22, 2017 }}

In Taiwan, government officials announced that 814 school campuses across Taiwan were damaged, at an estimated cost of NT$161 million (US$4.17 million).{{cite web|title=Over NT$1.3 bil. in typhoon losses for agricultural sector|url=https://chinapost.nownews.com/20160930-3267|publisher=China Post|accessdate=September 30, 2016|date=September 30, 2016}} In all, 8 people were killed in Taiwan, and total economic losses were counted to be NT$3.36 billion (US$106.9 million).{{cite news|last1=Lin |first1=Yantong (林彥彤) |last2=Xiao |first2=Tingfang (蕭婷方) |last3=Lü |first3=Yixuan (呂伊萱)|url=http://news.ltn.com.tw/news/life/paper/1038369 |script-title=zh:梅姬農損已破33億 農委會將立法執行農業保險|language=zh|publisher=Liberty Times|date=October 4, 2016|accessdate=October 5, 2016}} Meanwhile, 44 people were killed in mainland China, and total damages were amounted to CNY9.7 billion (US$1.45 billion).{{cite conference|pages=1–2 |conference=ESCAP/WMO Typhoon Committee |title=Member Report: China |author=CMA |publisher=ESCAP/WMO Typhoon Committee |url=http://www.typhooncommittee.org/11IWS/docs/Members%20Report/2016%E5%B9%B4CHINA%20REPORT-10.24.pdf |date=October 27, 2016 |accessdate=October 30, 2016 |conference-url=http://www.typhooncommittee.org/11IWS/ |archive-date=March 6, 2017 |archive-url=https://web.archive.org/web/20170306093110/http://www.typhooncommittee.org/11IWS/docs/Members%20Report/2016%E5%B9%B4CHINA%20REPORT-10.24.pdf |url-status=dead }}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = September 24

| Dissipated = October 5

| Image = Chaba 2016-10-03 0445Z.jpg

| Track = Chaba 2016 track.png

| 10-min winds = 115

| 1-min winds = 150

| Pressure = 905

}}

{{main|Typhoon Chaba (2016)}}

On September 24, a weak tropical depression had developed approximately {{convert|1,445|km|mi|abbr=on}} east-northeast of Guam.{{cite web|url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201609260600.htm# |title=Archived copy |access-date=2016-09-26 |archive-url=https://archive.today/20240523031831/https://www.webcitation.org/6koCpmFB0?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201609260600.htm |archive-date=2024-05-23 |url-status=dead}}{{cite web |url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201609260000.htm# |title=Archived copy |access-date=2016-09-26 |archive-url=https://archive.today/20240524004925/https://www.webcitation.org/6koD7hwaz?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201609260000.htm |archive-date=2024-05-24 |url-status=dead }} The system reached tropical storm status and was assigned the name Chaba late the next day.{{cite web |title=TS 1618 CHABA (1618) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609271800.htm |date=September 27, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523031952/https://www.webcitation.org/6krQXD5M6?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609271800.htm |access-date=May 22, 2017 }} By September 30, Chaba had intensified into a severe tropical storm after deep convection had evolved into a banding feature, under very favorable conditions.{{cite web |title=Prognostic Reasoning for Tropical Storm 21W (Chaba) Warning Nr 08 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201609292100.htm |date=September 29, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523032111/https://www.webcitation.org/6kuUUmoA7?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201609292100.htm |access-date=May 22, 2017 }}{{cite web |title=STS 1618 CHABA (1618) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609300000.htm |date=September 30, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523032031/https://www.webcitation.org/6kuU9zNw4?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201609300000.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} During October 1, Chaba entered the Philippine area of responsibility, with PAGASA giving the local name Igme, as it started to move in a northwestward direction.{{cite web |title=Severe Weather Bulletin #1: Severe Tropical Storm "IGME" (CHABA) |url=http://pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/250-tropical-cyclones/severe-weather-bulletin/igme-2016-bulletin/2606-igme-2016-1 |date=October 1, 2016 |archive-date=October 2, 2016 |publisher=PAGASA |url-status=dead |archive-url=https://web.archive.org/web/20161002105026/http://www.pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/250-tropical-cyclones/severe-weather-bulletin/igme-2016-bulletin/2606-igme-2016-1 |access-date=May 22, 2017 }} Chaba became a typhoon after its organization and structure vastly improved.{{cite web |title=TY 1618 CHABA (1618) UPGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610011200.htm |date=October 1, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523032233/https://www.webcitation.org/6kw1Mxs3r?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610011200.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }}{{cite web |title=Prognostic Reasoning for Typhoon 21W (Chaba) Warning Nr 15 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610011500.htm |date=October 1, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523032352/https://www.webcitation.org/6kxTvOTkb?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610011500.htm |access-date=May 22, 2017 }} During the next day, Chaba began explosive intensification,{{cite web |title=Prognostic Reasoning for Typhoon 21W (Chaba) Warning Nr 17 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610020300.htm |date=October 2, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523032314/https://www.webcitation.org/6kxTucdTK?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610020300.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} reaching Category 5 super typhoon intensity with a sharp {{convert|5|nmi|abbr=on}} wide eye.{{cite web|title=Prognostic Reasoning for Super Typhoon 21W (Chaba) Warning Nr 22 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610030900.htm |date=October 3, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523032553/https://www.webcitation.org/6kzS2wW95?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610030900.htm |archive-date=May 23, 2024 |access-date=May 22, 2017}} Chaba reached its peak intensity with 10-minute sustained winds of {{convert|215|km/h|mph|abbr=on|round=5}}, while 1-minute sustained winds were at {{convert|280|km/h|mph|abbr=on|round=5}}, and the minimum central pressure was 905 mbar.{{cite web|title=TY 1618 CHABA (1618) |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610031200.htm |date=October 3, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523032434/https://www.webcitation.org/6kzRk2REs?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610031200.htm |archive-date=May 23, 2024 |access-date=May 22, 2017}} Thereafter, Chaba began to weaken as its core became asymmetric,{{cite web |title=Prognostic Reasoning for Typhoon 21W (Chaba) Warning Nr 23 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610031500.htm |date=October 3, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523032513/https://www.webcitation.org/6kzS2aULa?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610031500.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} due to strong wind shear.{{cite web |title=Prognostic Reasoning for Typhoon 21W (Chaba) Warning Nr 28 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610042100.htm |date=October 4, 2016 |archive-date=May 23, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523032839/https://www.webcitation.org/6l2Jn7Nh5?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610042100.htm |access-date=May 22, 2017 }} As it neared the coast of Busan, South Korea, Chaba transitioned into an extratropical cyclone.{{cite web |title=DEVELOPED LOW STS 1618 CHABA (1618) |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610051200.htm |date=October 5, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523032916/https://www.webcitation.org/6l2JWopfK?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610051200.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }}

The storm left widespread damage across the southern regions of South Korea, killing at least 7 and leaving 4 others missing. Transportation was disrupted, with hundreds of flights canceled, while more than 200,000 households lost electricity. Chaba was the strongest typhoon to strike the country since Typhoon Sanba in 2012.{{cite web|title=Typhoon claims six lives in South Korea|url=http://www.thefinancialexpress-bd.com/2016/10/06/48453/Typhoon-claims-six-lives-in-South-Korea|date=October 6, 2016|publisher=Financial Times Bangladesh}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = October 4 (Entered basin)

| Dissipated = October 13

| Image = Songda 2016-10-12 0305Z.jpg

| Track = Songda 2016 track.png

| 10-min winds = 100

| 1-min winds = 130

| Pressure = 925

}}

{{Main|Typhoon Songda (2016)}}

A tropical disturbance entered the basin from the Central Pacific late on October 3 and on the following day, became a tropical depression approximately {{convert|1,333|km|mi|abbr=on}} east-southeast of Wake Island.https://www.webcitation.org/6l0las91y?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201610040230.htm https://www.webcitation.org/6l0lODaSv?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610040000.htm After moving westward for several days, 23W intensified into a tropical storm, with the JMA giving the name Songda.{{cite web|title=Tropical Storm 23W (Songda) Warning Nr 003 |url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201610082100.htm |date=October 8, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005730/https://www.webcitation.org/6l882pTlg?url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201610082100.htm |access-date=May 22, 2017}}{{cite web |title=TS 1620 SONGDA (1620) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610081200.htm |date=October 8, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523131553/https://www.webcitation.org/6l6vNUacy?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610081200.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} By October 9, an eye feature became apparent in microwave imagery,{{cite web |title=Prognostic Reasoning for Tropical Storm 23W (Songda) Warning Nr 06 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610091500.htm |date=October 9, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005849/https://www.webcitation.org/6lA4lhhhu?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610091500.htm |access-date=May 22, 2017 }} and Songda reached severe tropical storm intensity.{{cite web |title=STS 1620 SONGDA (1620) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610091800.htm |date=October 9, 2016 |archive-date=May 23, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523131834/https://www.webcitation.org/6lA44SRY5?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610091800.htm |access-date=May 22, 2017 }} Six hours later, Songda intensified into a typhoon.{{cite web |title=TY 1620 SONGDA (1620) UPGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610100000.htm |date=October 10, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523131754/https://www.webcitation.org/6lA43i7Ao?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610100000.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} Songda started to undergo rapid deepening, while forming a ragged eye.{{cite web |title=Prognostic Reasoning for Typhoon 23W (Songda) Warning Nr 09 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610100900.htm |date=October 10, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524005807/https://www.webcitation.org/6lA4keRCX?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610100900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}

Songda eventually reached its peak intensity as a Category 4 super typhoon, despite 25-30 kt vertical wind shear,{{cite web |title=Prognostic Reasoning for Super Typhoon 23W (Songda) Warning Nr 15 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610112100.htm |date=October 11, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523132119/https://www.webcitation.org/6lBdjn2og?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610112100.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} with 10-minute sustained winds of {{convert|185|km/h|mph|abbr=on|round=5}} and a minimum pressure of 925 mbar.{{cite web|title=TY 1620 SONGDA (1620) |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610120000.htm |date=October 12, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524005928/https://www.webcitation.org/6lCveE50L?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610120000.htm |archive-date=May 24, 2024 |access-date=May 22, 2017}} Shortly thereafter, Songda rapidly weakened as the wind shear increased further, and its eye became cloud-filled.{{cite web |title=Prognostic Reasoning for Typhoon 23W (Songda) Warning Nr 16 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610120300.htm |date=October 12, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524010009/https://www.webcitation.org/6lCvzoFYO?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610120300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} The JTWC issued its final advisory, classifying Songda as a rapidly-weakening Category 3-equivalent typhoon. The storm was embedded within the deep mid-latitude westerlies and located over waters cooler than {{convert|26|°C|°F|abbr=on}}.{{cite web|title=Typhoon 23W (Songda) Warning Nr 017 |url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201610120900.htm |date=October 12, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523132316/https://www.webcitation.org/6lCvtGhUA?url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201610120900.htm |archive-date=May 23, 2024 |access-date=May 22, 2017}} The JMA downgraded Songda to a severe tropical storm in its final advisory on October 13, and Songda subsequently transitioned into an extratropical cyclone.{{cite web |title=DEVELOPED LOW FORMER STS 1620 SONGDA (1620) |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610130600.htm |date=October 13, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523132359/https://www.webcitation.org/6lEVd883T?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610130600.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} The extratropical remnant of Songda went on to affect the west coast of North America with heavy rain and winds.

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = October 4

| Dissipated = October 14

| Image = Aere 2016-10-07 0250Z.jpg

| Track = Aere 2016 track.png

| 10-min winds = 60

| 1-min winds = 55

| Pressure = 975

}}

{{main|Tropical Storm Aere (2016)}}

Shortly after Songda's formation, another tropical depression developed well east to the Babuyan Group of Islands.https://www.webcitation.org/6l2JvOHFO?url=http://gwydir.demon.co.uk/advisories/WTPN21-PGTW_201610050130.htm https://www.webcitation.org/6l0lNTsMQ?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610041200.htm Later that day, PAGASA named the system Julian.{{cite web |title=Severe Weather Bulletin #1: Tropical Depression "JULIAN" |url=http://pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/253-tropical-cyclones/severe-weather-bulletin/julian-2016-bulletin/2624-1 |date=October 4, 2016 |archive-date=October 6, 2016 |publisher=PAGASA |url-status=dead |archive-url=https://web.archive.org/web/20161006150105/http://www.pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/253-tropical-cyclones/severe-weather-bulletin/julian-2016-bulletin/2624-1 |access-date=May 22, 2017 }} Despite Julian's disorganised structure, conditions were favourable for development, with light to moderate wind shear and very warm sea surface temperatures.{{cite web |title=Prognostic Reasoning for Tropical Depression 22W (Twenty-two) Warning Nr 02 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610052100.htm |date=October 5, 2016 |archive-date=May 22, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240522213113/https://www.webcitation.org/6l42QXyty?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610052100.htm |access-date=May 22, 2017 }} After a significant increase of convection, the system became a tropical storm, receiving the name Aere.{{cite web |title=TS 1619 AERE (1619) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610051800.htm |date=October 5, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240522212950/https://www.webcitation.org/6l422ceMG?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610051800.htm |archive-date=May 22, 2024 |access-date=May 22, 2017 }} Aere became a severe tropical storm the following day.{{cite web |title=STS 1619 AERE (1619) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610070600.htm |date=October 7, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240522213236/https://www.webcitation.org/6l5LMeSco?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610070600.htm |archive-date=May 22, 2024 |access-date=May 22, 2017 }} Shortly thereafter, Aere reached itspeak intensity with 10-minute winds of {{convert|110|km/h|mph|abbr=on|round=5}}, just shy of typhoon strength.{{cite web|title=STS 1619 AERE (1619) |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610071500.htm |date=October 7, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240522213156/https://www.webcitation.org/6l5LLYb5h?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610071500.htm |archive-date=May 22, 2024 |access-date=May 22, 2017}} Upwelling induced weakening, and Aere weakened to a tropical storm.{{cite web |title=Prognostic Reasoning for Tropical Storm 22W (Aere) Warning Nr 11 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610080300.htm |date=October 8, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240522213517/https://www.webcitation.org/6l6vAqK6F?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610080300.htm |archive-date=May 22, 2024 |access-date=May 22, 2017 }}{{cite web |title=TS 1619 AERE (1619) DOWNGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610081200.htm |date=October 8, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240522213436/https://www.webcitation.org/6l6uzOpCW?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610081200.htm |archive-date=May 22, 2024 |access-date=May 22, 2017 }} By October 10, Aere's LLCC became exposed due to southwesterly wind shear, and Aere degenerated to a tropical depression.{{cite web |title=TD DOWNGRADED FROM TS 1619 AERE (1619) |url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610100000.htm |date=October 10, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240522213641/https://www.webcitation.org/6lA3YsXyM?url=http://gwydir.demon.co.uk/advisories/WTPQ22-RJTD_201610100000.htm |archive-date=May 22, 2024 |access-date=May 22, 2017 }} The JMA tracked its remnants as it moved southwestward until it weakened to a low-pressure area late on October 11.https://www.webcitation.org/6lEblh9BU?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610111800.htm

On October 13, the well-marked low-pressure area of Aere re-generated into a tropical depression,https://www.webcitation.org/6lEbjqEur?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610130000.htm and was tracked by the JMA until it fully dissipated on October 14.https://www.webcitation.org/6lGDlySGs?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610140600.htm

Most of the damage was reported mainly in Vietnam, especially in the central region, where estimated damages for transport works were at 130 billion ₫ (US$5.83 million).{{cite web|title=Đường bộ thiệt hại 130 tỷ đồng do mưa lũ|url=http://www.baogiaothong.vn/duong-bo-thiet-hai-130-ty-dong-do-mua-lu-d172604.html|date=October 17, 2016|publisher=GIAO THÔNG PHÁT TRIỂN|access-date=October 17, 2016|archive-url=https://web.archive.org/web/20161018223155/http://www.baogiaothong.vn/duong-bo-thiet-hai-130-ty-dong-do-mua-lu-d172604.html|archive-date=October 18, 2016|url-status=dead}} A total of 25 houses were destroyed while 949 were damaged. In agriculture, 3.14 ha of rice and 11.5 ha of crops were damaged.{{cite web|title=25 người chết, 4 người mất tích do mưa lũ|url=http://tuoitre.vn/tin/chinh-tri-xa-hoi/20161017/25-nguoi-chet-4-nguoi-mat-tich-do-mua-lu/1189738.html|date=October 17, 2016|publisher=Chính trị – Xã hội}}{{cite web|title=Vietnam braces for Typhoon Sarika's arrival as number dead in flooding reaches 31|url=http://www.chinapost.com.tw/asia/vietnam/2016/10/19/481450/Vietnam-braces.htm|date=October 19, 2016|publisher=Chinapost}} In total, flooding by the storm caused ₫ 4.6 trillion (US$209 million) of damage.

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = October 13

| Dissipated = October 19

| Image = Sarika 2016-10-15 0510Z.jpg

| Track = Sarika 2016 track.png

| 10-min winds = 95

| 1-min winds = 115

| Pressure = 935

}}

{{Main|Typhoon Sarika}}

Sarika was first noted as a tropical depression located about {{convert|1200|km|abbr=on}} east-southeast of Manila, Philippines.https://www.webcitation.org/6lCwjwGrF?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610111800.htm https://www.webcitation.org/6lCw3XYue?url=http://gwydir.demon.co.uk/advisories/WTPN21-PGTW_201610112200.htm When 24W entered their area of responsibility, PAGASA assigned it the local name Karen.{{cite web|title=Severe Weather Bulletin #1: TROPICAL DEPRESSION "KAREN" |url=http://pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/263-tropical-cyclones/severe-weather-bulletin/karen-2016-bulletin/3061-1 |date=October 12, 2016 |archive-date=May 23, 2024 |publisher=PAGASA |url-status=dead |archive-url=https://archive.today/20240523131152/https://www.webcitation.org/6lEcClQkA?url=http://pagasa.dost.gov.ph/index.php/tropical-cyclones/weather-bulletins/263-tropical-cyclones/severe-weather-bulletin/karen-2016-bulletin/3061-1 |access-date=May 22, 2017}} By October 13, images depicted a broad LLCC; sea surface temperatures were high, at {{convert|31|°C|°F|abbr=on}}.{{cite web|title=Prognostic Reasoning for Tropical Depression 24W (Twenty-four) Warning Nr 04 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610130900.htm |date=October 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524010251/https://www.webcitation.org/6lEalAKZu?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610130900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017}} Hours later, the system became a tropical storm, with the JMA naming it as Sarika.{{cite web |title=Tropical Storm 24W (Twenty-four) Warning Nr 005 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201610131500.htm |date=October 13, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524010210/https://www.webcitation.org/6lEadd95F?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201610131500.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite web |title=TS 1621 SARIKA (1621) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610131200.htm |date=October 13, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524010332/https://www.webcitation.org/6lEaV7gVA?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610131200.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Sarika continued organizing and reached severe tropical storm intensity.{{cite web |title=STS 1621 SARIKA (1621) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610140000.htm |date=October 14, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524010451/https://www.webcitation.org/6lGC9hJsQ?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610140000.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Several hours later, Sarika started to form an eye feature as it became a typhoon.{{cite web |title=Prognostic Reasoning for Tropical Storm 24W (Sarika) Warning Nr 09 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610141500.htm |date=October 14, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524010533/https://www.webcitation.org/6lGCVbrFo?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610141500.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite web |title=TY 1621 SARIKA (1621) UPGRADED FROM STS |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610141200.htm |date=October 14, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524010410/https://www.webcitation.org/6lGC88tbW?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610141200.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} The storm eventually reached its peak intensity as a Category 4 typhoon with 1-minute sustained winds of {{convert|215|km/h|mph|abbr=on|round=5}} and a minimum barometric pressure of 935 mbar.{{cite web|title=Typhoon 24W (Sarika) Warning Nr 014 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201610152100.htm |date=October 15, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524011138/https://www.webcitation.org/6lIzKXWm5?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201610152100.htm |access-date=May 22, 2017}}{{cite web |title=TY 1621 SARIKA (1621) |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610151800.htm |date=October 15, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524010852/https://www.webcitation.org/6lHhrURgV?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610151800.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Early on October 16, Sarika made landfall over in Baler, Aurora.{{cite web|title=Typhoon Karen makes landfall in Aurora|url=http://www.rappler.com/nation/special-coverage/weather-alert/149304-20161016-typhoon-karen-pagasa-forecast-2am|date=October 16, 2016|publisher=Rappler}} Dramatic weakening occurred as Sarika traversed the islands.{{cite web |title=Prognostic Reasoning for Typhoon 24W (Sarika) Warning Nr 18 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610162100.htm |date=October 16, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524011857/https://www.webcitation.org/6lMGj1nQu?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201610162100.htm |access-date=May 22, 2017 }} After moving westward rapidly for two days, Sarika weakened to a severe tropical storm as it made landfall over in Hainan.{{cite web |title=STS 1621 SARIKA (1621) DOWNGRADED FROM TY |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610180900.htm |date=October 18, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524011818/https://www.webcitation.org/6lMF3cR8K?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610180900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Sarika continued weakening as it made its final landfall over the border of Vietnam and China, and dissipated later that day.{{cite web |title=TD DOWNgRADED FROM TS 1621 SARIKA (1621) |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610191200.htm |date=October 19, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524011939/https://www.webcitation.org/6lNcxnZ4N?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201610191200.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}https://www.webcitation.org/6lQpL4I1i?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610191800.htm

Nearly 13,000 homes were damaged or destroyed, and more than 200,000 people were displaced. Agricultural damage in the Philippines was severe, totaling ₱3.63 billion (US${{To USD round|3630|PHL|year=2016|sf=3}} million).{{#tag:ref|All currencies are in their 2016 values and are converted to United States dollars using data from the International Monetary Fund published by the World Bank.{{cite web |author=International Monetary Fund, International Financial Statistics |title=DEC alternative conversion factor (LCU per US$) |url=https://data.worldbank.org/indicator/PA.NUS.ATLS |publisher=World Bank |access-date=January 29, 2022 |year=2022}}|group="nb"}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = October 14

| Dissipated = October 21

| Image = Haima 2016-10-18 0000Z.jpg

| Track = Haima 2016 track.png

| 10-min winds = 115

| 1-min winds = 145

| Pressure = 900

}}

{{Main|Typhoon Haima}}

During October 14, the JMA and JTWC reported that a tropical depression had developed about {{convert|700|km|mi|round=5|abbr=on}} within the Caroline Islands to the south of Guam.{{cite web|archive-date=May 23, 2024|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt|agency=United States Joint Typhoon Warning Center|title=Prognostic Reasoning For Tropical Depression 25W Warning 1 October 14, 2016 21z|archive-url=https://archive.today/20240523062828/https://www.webcitation.org/6lHiwphDq?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610142100.htm|access-date=July 21, 2017|url-status=dead}}{{cite web |title= RSMC Tropical Cyclone Best Track: Typhoon Hamia |url= http://www.wis-jma.go.jp/cms/warning/2016/11/22/typhoon-best-track-2016-11-22t080000z/ |url-status= live |date= November 22, 2016 |agency= Japan Meteorological Agency |archive-url= https://archive.today/20240522103010/https://www.webcitation.org/6mCx8jqX3?url=http://gwydir.demon.co.uk/advisories/AXPQ20-RJTD_201611220800.htm |archive-date= May 22, 2024 |access-date= July 20, 2017 }} During that day the depressions low level circulation center rapidly consolidated, while bands of atmospheric convection built and wrapped into the center. As a result, both warning centers reported that the depression had developed into a tropical storm, early the next day with the JMA naming it as Haima.

Early on October 15, the depression intensified into a tropical storm and was assigned the name Haima.{{cite web |title=TS 1622 HAIMA (1622) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610150000.htm |date=October 15, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524010933/https://www.webcitation.org/6lHiSWuMT?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610150000.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} At this point of time, Haima was located in a very favorable environment with very high ocean heat content, very low wind shear and warm SSTs.{{cite web |title=Prognostic Reasoning for Tropical Storm 25W (Haima) Warning Nr 02 |url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610150300.htm |date=October 15, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240523062907/https://www.webcitation.org/6lHiwSxnD?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201610150300.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} Three hours later, Haima intensified into a severe tropical storm.{{cite web |title=STS 1622 HAIMA (1622) UPGRADED FROM TS |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610160000.htm |date=October 16, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240523063110/https://www.webcitation.org/6lIzXrNC6?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201610160000.htm |archive-date=May 23, 2024 |access-date=May 22, 2017 }} {{citation needed span|With very good radial outflow, and still being situated in an extremely favorable environment, Haima rapidly intensified into a Category 4 super typhoon. By the end of the time, PAGASA announced the Haima had entered their area of responsibility, assigning it the name Lawin. Haima continued to intensify, reaching Category 5 super typhoon status by late on October 18.|date=October 2016}} Super Typhoon Haima (Lawin) intensified further. PAGASA used the term "super typhoon" on Haima for the first time since it was introduced in May 2015 due to Typhoon Haiyan's ravage during 2013. PAGASA also raised Signal #5 in the provinces of Cagayan and Isabela, which made it a hazardous storm. Due to land interaction, Typhoon Haima weakened into a Category 4 storm and made landfall in Peñablanca, Cagayan. Typhoon Haima weakened after landfall in the Philippines and landed in Hong Kong as a weakened Category 1 storm, in which Signal no. 8 was raised. By October 22, Haima became extratropical and dissipated on October 26.

Total damages in the Philippines were at ₱3.74 billion (US$77.6 million).{{cite web|title=SitRep No.9 re Preparedness Measures & Effects of Super TY LAWIN (I.N. HAIMA)|url=http://www.ndrrmc.gov.ph/attachments/article/2946/Sitrep_No_09_re_Preparedness_Measures_and_Effects_of_Super_Typhoon_LAWIN_(HAIMA)_as_of_25OCT2016_0800H.pdf|access-date=October 25, 2016|publisher=NDRRMC}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = October 30

| Dissipated = November 7

| Image = Meari 2016-11-06 0312Z.jpg

| Track = Meari 2016 track.png

| 10-min winds = 75

| 1-min winds = 90

| Pressure = 960

}}

On October 31, the JMA started to track a tropical depression about {{convert|287|km|mi|abbr=on}} south of Guam.https://www.webcitation.org/6lhFdd5Ho?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610310000.htm https://www.webcitation.org/6lhFDBInP?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201610310600.htm Late on November 2, organization had increased as the JTWC upgraded the system to a tropical depression with the identifier of 26W.{{cite web|title=Tropical Depression 26W (Twenty-six) Warning Nr 001|url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611022100.htm|archive-url=https://archive.today/20240524011254/https://www.webcitation.org/6ljtTlwjG?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611022100.htm|url-status=dead|date=November 2, 2016|archive-date=May 24, 2024|publisher=Joint Typhoon Warning Center}} The JMA, however, had upgraded 26W to a tropical storm, giving the name Meari early on the next day.{{cite web|title=TS 1623 MEARI (1623) UPGRADED FROM TD|url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611030000.htm|archive-url=https://archive.today/20240524011217/https://www.webcitation.org/6ljtbKeI9?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611030000.htm|url-status=dead|archive-date=May 24, 2024|date=November 3, 2016|agency=Japan Meteorological Agency}} With a rapidly consolidating LLCC, the JTWC followed suit of upgrading to a tropical storm.{{cite web|title=Prognostic Reasoning for Tropical Storm 26W (Meari) Warning Nr 03|url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611030900.htm|archive-url=https://archive.today/20240524011735/https://www.webcitation.org/6lli5liUL?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611030900.htm|url-status=dead|date=November 3, 2016|archive-date=May 24, 2024|publisher=Joint Typhoon Warning Center}} By November 4, now moving northward, feeder bands were covering its very broad and compact LLCC and therefore Meari intensified into a severe tropical storm.{{cite web|title=Prognostic Reasoning for Tropical Storm 26W (Meari) Warning Nr 06|url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611040300.htm|archive-url=https://archive.today/20240524011657/https://www.webcitation.org/6lli2oGbA?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611040300.htm|url-status=dead|archive-date=May 24, 2024|date=November 4, 2016|publisher=Joint Typhoon Warning Center}}{{cite web|title=STS 1623 MEARI (1623) UPGRADED FROM TS|url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611040600.htm|archive-url=https://archive.today/20240524011617/https://www.webcitation.org/6llhVvYet?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611040600.htm|url-status=dead|archive-date=May 24, 2024|date=November 4, 2016|agency=Japan Meteorological Agency}} Hours later, deep convective banding with a central dense overcast (CDO) seen from satellite imagery prompted the JTWC and the JMA to upgrade Meari to a typhoon.{{cite web|title=Prognostic Reasoning for Typhoon 26W (Meari) Warning Nr 09|url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611042100.htm|archive-url=https://archive.today/20240524012138/https://www.webcitation.org/6lnkLSWh4?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611042100.htm|url-status=dead|date=November 4, 2016|archive-date=May 24, 2024|publisher=Joint Typhoon Warning Center}}{{cite web|title=TY 1623 MEARI (1623) UPGRADED FROM STS|url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611050000.htm|archive-url=https://archive.today/20240524012021/https://www.webcitation.org/6lnjcA8ol?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611050000.htm|url-status=dead|archive-date=May 24, 2024|date=November 5, 2016|agency=Japan Meteorological Agency}} On the next day, organization ensued with deep convection wrapping into its center and its CDO feature becoming more symmetric. Meari intensified into a Category 2 typhoon.{{cite web|title=Prognostic Reasoning for Typhoon 26W (Meari) Warning Nr 12|url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611051500.htm|archive-url=https://archive.today/20240524012056/https://www.webcitation.org/6lnkKLS14?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611051500.htm|url-status=dead|archive-date=May 24, 2024|date=November 5, 2016|publisher=Joint Typhoon Warning Center}} During the course of November 6, Meari reached peak intensity only as a Category 2 with 10-minute sustained winds of {{convert|155|km/h|mph|abbr=on|round=5}} and a minimum barometric pressure of 955 mbar.{{cite web|title=TY 1623 MEARI (1623)|url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611060600.htm|archive-url=https://archive.today/20240524012459/https://www.webcitation.org/6lqoSR2eJ?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611060600.htm|url-status=dead|date=November 6, 2016|archive-date=May 24, 2024|agency=Japan Meteorological Agency}}

Later that day, Meari started to move northeastward rapidly with a strong poleward outflow as it started to interact with high vertical wind shear.{{cite web|title=Prognostic Reasoning for Typhoon 26W (Meari) Warning Nr 16|url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611061500.htm|archive-url=https://archive.today/20240524012420/https://www.webcitation.org/6lqoryP2R?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611061500.htm|url-status=dead|date=November 6, 2016|archive-date=May 24, 2024|publisher=Joint Typhoon Warning Center}} The JTWC downgraded Meari to a Category 1.{{cite web|title=Prognostic Reasoning for Typhoon 26W (Meari) Warning Nr 17|url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611062100.htm|archive-url=https://archive.today/20240524012341/https://www.webcitation.org/6lqorbUjK?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611062100.htm|url-status=dead|date=November 6, 2016|archive-date=May 24, 2024|publisher=Joint Typhoon Warning Center}} On November 7, the JTWC issued its final advisory on Meari due to the fact that its convective structure had become frontal, therefore it had already transitioned into an extratropical cyclone.{{cite web|title=Typhoon Meari (26W) Warning Nr 019|url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611070900.htm|archive-url=https://archive.today/20240524012223/https://www.webcitation.org/6lqohFPBV?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611070900.htm|url-status=dead|archive-date=May 24, 2024|date=November 7, 2016|publisher=Joint Typhoon Warning Center}} The JMA followed suit three hours later.{{cite web|title=DEVELOPING LOW FORMER TY 1623 MEARI (1623)|url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611071200.htm|archive-url=https://archive.today/20240524012258/https://www.webcitation.org/6lqoOGx76?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611071200.htm|url-status=dead|archive-date=May 24, 2024|date=November 7, 2016|agency=Japan Meteorological Agency}} {{citation needed span|Meari's extratropical remnants was later absorbed by another but larger extratropical cyclone early on November 10.|date=November 2016}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = November 2

| Dissipated = November 6

| Image = JMA TD 43 2016-11-04 0620Z.jpg

| Track = JMA TD 45 2016 track.png

| 10-min winds = 30

| Pressure = 1004

}}

{{main|November 2016 Vietnam tropical depression}}

On November 2, a tropical depression formed west of Sabah, Malaysia.{{cite web | url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/search_day.pl?lang=en&year=2016&month=11&day=2 | title=Digital Typhoon: List of weather charts on November 02, 2016 (Wed) }} On November 5, it made landfall in southern Vietnam, and moved westwards until it dissipated on November 6.{{cite web |title=WWJP25 RJTD 051800 |url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201611051800.htm |date=November 5, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240522203315/https://www.webcitation.org/6lnkinDHW?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201611051800.htm |archive-date=May 22, 2024 |access-date=May 22, 2017 }}

The depression exacerbated the torrential rains and heavy flooding that had impacted central and southern Vietnam since mid October,{{cite web | url=http://dantri.com.vn/xa-hoi/chu-dong-doi-pho-voi-mua-lu-va-ap-thap-nhiet-doi-20161103214734774.htm | title=Chủ động đối phó với mưa lũ và áp thấp nhiệt đới | date=3 November 2016 }}{{cite web | url=http://vov.vn/tin-24h/mua-lu-mien-trung-14-nguoi-chet-5-nguoi-mat-tich-566786.vov | title=Mưa lũ miền Trung: 14 người chết, 5 người mất tích | date=6 November 2016 }}{{cite web | url=http://infonet.vn/mien-trung-36-nguoi-chet-mat-tich-bi-thuong-do-mua-lu-post213083.info | title=Miền Trung: 36 người chết, mất tích, bị thương do mưa lũ }} damaging more than 20,000 homes.{{cite web|title=Vietnam floods: deaths reported, tens of thousands of homes destroyed|url=https://www.theguardian.com/world/2016/oct/16/vietnam-floods-deaths-reported-tens-of-thousands-of-homes-destroyed|date=October 16, 2016|work=The Guardian}} A total of 15 people were killed and total damage reached ₫1.073 trillion (US$48.1 million) in Vietnam from November 1, though a total of 35 have been killed since the flooding from October. Residents say that the country had their worst flooding since 2011.{{cite web|title=Vietnam Braces for Typhoon Sarika After Deadly Flooding|url=https://www.wsj.com/articles/vietnam-braces-for-typhoon-sarika-after-deadly-flooding-1476598264|date=October 15, 2016|access-date=October 16, 2016|publisher=Wall Street Journal}}

{{Clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = November 8

| Dissipated = November 13

| Image = Ma-on 2016-11-11 0310Z.jpg

| Track = Ma-on 2016 track.png

| 10-min winds = 35

| 1-min winds = 35

| Pressure = 1002

}}

On November 8, the JMA started to track a tropical depression that had formed several nautical miles to the east of the Mariana Islands.https://www.webcitation.org/6lsKKo4tn?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201611081800.htm Later that day, the JTWC had started initiating advisories giving it the designation 27W.{{cite web |title=Tropical Depression 27W (Twenty-seven) Warning Nr 001 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611092100.htm |date=November 9, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524012940/https://www.webcitation.org/6lwNSghIF?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611092100.htm |access-date=May 22, 2017 }} During the next day, the JMA upgraded 27W to a tropical storm, naming it Ma-on, due to deep curved convection despite the system's LLCC being exposed.{{cite web |title=TS 1624 MA-ON (1624) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611100600.htm |date=November 10, 2016 |archive-date=May 24, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524012743/https://www.webcitation.org/6lwMjFKzQ?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611100600.htm |access-date=May 22, 2017 }}{{cite web |title=Prognostic Reasoning for Tropical Depression 27W (Ma-on) Warning Nr 03 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611100900.htm |date=November 10, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524012900/https://www.webcitation.org/6lwNg3jKi?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611100900.htm |access-date=May 22, 2017 }} The JTWC followed suit, upgrading it to a tropical storm after the system became more symmetrical with deep convection over in an area of low wind shear.{{cite web |title=Prognostic Reasoning for Tropical Storm 27W (Ma-on) Warning Nr 06 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611110300.htm |date=November 11, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524012822/https://www.webcitation.org/6lwNeoJgS?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611110300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Later that day, Ma-on reached its maximum intensity with 10-minute sustained winds of {{convert|75|km/h|mph|abbr=on|round=5}} and a minimum pressure of 1002 mbar.{{cite web |title=TS 1624 MA-ON (1624) UPGRADED FROM TD |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611110000.htm |date=November 11, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524012706/https://www.webcitation.org/6lwMgyb86?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611110000.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} Despite additional strengthening being forecast, its LLCC became exposed as favorable conditions started to deteriorate.{{cite web |title=Prognostic Reasoning for Tropical Storm 27W (Ma-on) Warning Nr 08 |url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611111500.htm |date=November 11, 2016 |archive-date=May 24, 2024 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524013145/https://www.webcitation.org/6lyBotnfG?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611111500.htm |access-date=May 22, 2017 }} Both agencies downgraded Ma-on to a tropical depression and issued their final advisories,{{cite web |title=Tropical Depression 27W (Ma-on) Warning Nr 011 |url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611120900.htm |date=November 12, 2016 |publisher=Joint Typhoon Warning Center |url-status=dead |archive-url=https://archive.today/20240524013103/https://www.webcitation.org/6lyBgLDtq?url=http://gwydir.demon.co.uk/advisories/WTPN31-PGTW_201611120900.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}{{cite web |title=TD DOWNGRADED FROM TS 1624 MA-ON (1624) |url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611120600.htm |date=November 12, 2016 |agency=Japan Meteorological Agncy |url-status=dead |archive-url=https://archive.today/20240524013221/https://www.webcitation.org/6lyBQxPWC?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201611120600.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }} although, the JMA tracked Ma-on until November 13.

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = November 9

| Dissipated = November 12

| Image = TD 28W 2016-11-10 0225Z.jpg

| Track = 28W 2016 track.png

| 1-min winds = 25

| Pressure = 1008

| Type1 = nwpdepression

}}

During November 9, the JMA reported that a tropical depression had developed, about {{convert|455|km|mi|round=5|abbr=on}} to the east-northeast of Kwajalein Atoll in the Marshall Islands.{{cite web|title=Monthly Global Tropical System Tracks — November 2016|publisher=Australian Severe Weather|date=December 11, 2016|access-date=July 20, 2016|author=Young, Steve|url=http://australiasevereweather.com/cyclones/2017/trak1611.htm}} Over the next couple of days, the system moved westwards through the Marshall Islands, where it gradually consolidated further within a favourable environment for further development.{{cite web |url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/ab/abwpweb.txt |agency=United States Joint Typhoon Warning Center |title=Prognostic Reasoning For Tropical Depression 28W Warning 1 November 11, 2016 03z |archive-url=https://archive.today/20161111133223/https://www.webcitation.org/6lwM3XJbc?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201611092330.htm |archive-date=2016-11-11 |access-date=July 20, 2017}} During November 11, the JTWC initiated advisories and designated the system as Tropical Depression 28W, after atmospheric convection had started to wrap into the weekly defined low level circulation centre. However, as the system was located within an area of low to moderate vertical wind shear, atmospheric convection associated with the system quickly dissipated.{{cite web|archive-date=May 24, 2024|agency=United States Joint Typhoon Warning Center|access-date=July 20, 2017|url-status=dead|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/warnings/|title=Prognostic Reasoning For Tropical Depression 28W Warning 2 November 11, 2016 09z|archive-url=https://archive.today/20240524013021/https://www.webcitation.org/6lwOVJkiW?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201611110900.htm}} The system subsequently degenerated into a tropical wave, before it was last noted by both warning centers during November 12.{{cite web|archive-date=May 24, 2024|agency=United States Joint Typhoon Warning Center|access-date=July 20, 2017|url-status=dead|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/warnings/|title=Tropical Depression 28W Warning 6 November 12, 2016 09z|archive-url=https://archive.today/20240524013301/https://www.webcitation.org/6lyCWWjWZ?url=http://gwydir.demon.co.uk/advisories/WTPN32-PGTW_201611120900.htm}}

{{clear}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = November 23

| Dissipated = November 28

| Image = Tokage 2016-11-26 0210Z.png

| Track = Tokage 2016 track.png

| 10-min winds = 50

| 1-min winds = 80

| Pressure = 992

}}

During November 23, PAGASA started to monitor a tropical depression that had developed about {{convert|420|km|mi|round=5|abbr=on}} to the east of Hinatuan, Surigao del Sur.{{cite report|title=Severe Weather Bulletin No. 01 re Tropical Depression "MARCE"|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_1_re_TD_MARCE_issued_on_23NOV2016.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 23, 2016|access-date=February 9, 2019}} The JMA, however, tracked the depression on November 24.{{cite web|title=bst2016.txt|url=https://www.jma.go.jp/jma/jma-eng/jma-center/rsmc-hp-pub-eg/Besttracks/bst2016.txt|publisher=Japan Meteorological Agency|access-date=February 9, 2019|archive-date=October 1, 2018|archive-url=https://web.archive.org/web/20181001115555/http://www.jma.go.jp/jma/jma-eng/jma-center/rsmc-hp-pub-eg/Besttracks/bst2016.txt|url-status=dead}} The JTWC would

shortly follow suit, designating it as "29W".{{cite web|title=bwp292016.txt|url=https://ftp.emc.ncep.noaa.gov/wd20vxt/hwrf-init/decks/bwp292016.dat|publisher=National Oceanic and Atmospheric Administration|date=November 14, 2017|access-date=February 9, 2019}} Over the rest of the day, the depression was gradually organizing under favorable conditions, before the PAGASA reported that Tropical Depression "Marce" had made landfall over Siargao Island around 12:00 UTC (8:00 p.m. PST) of the same day.{{cite report|title=Severe Weather Bulletin No. 10 re Tropical Depression "MARCE"|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_10_re_TD_MARCE_issued_on_24NOV2016_2000H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 24, 2016|access-date=February 9, 2019}} The JTWC would also follow suit shortly. On 12:00 UTC of November 25, the JMA reported that "Marce" became a tropical storm while traversing the Visayan Sea, naming it as "Tokage". Around 21:00 UTC of the same day, the PAGASA reported that "Marce" became a tropical storm while nearing Panay Island.{{cite report|title=Severe Weather Bulletin No. 13 re Tropical Storm "MARCE"|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_13_re_TS_MARCE_issued_on_25NOV2016_0500H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 25, 2016|access-date=February 9, 2019}} Tokage would emerge into the Mindoro Strait while making its second landfall and traverse on the Calamian Islands.{{cite report|title=Severe Weather Bulletin No. 17 re Tropical Storm "MARCE"|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_17_re_TS_MARCE_issued_on_25NOV2016_1700H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 25, 2016|access-date=February 9, 2019}}{{cite report|title=Severe Weather Bulletin No. 19 re Tropical Storm "MARCE"|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_18_re_TS_MARCE_issued_on_25NOV2016_2000H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 25, 2016|access-date=February 9, 2019}}{{cite report|title=Severe Weather Bulletin No. 19 re Tropical Storm "MARCE"|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_19_re_TS_MARCE_issued_on_25NOV2016_2300H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 26, 2016|access-date=February 9, 2019}} Shortly after emerging into the South China Sea on November 26,{{cite report|title=Severe Weather Bulletin No. 20 re Tropical Storm "MARCE"|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_20_re_TS_MARCE_issued_on_26NOV2016_0200H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 26, 2016|access-date=February 9, 2019}} JMA reported that Tokage briefly reached its peak intensity of {{convert|95|km/h|kn|abbr=in}} and a pressure of 992 hpa. The JTWC would follow suit, upgrading Tokage to a category 1 typhoon, reaching its peak intensity of {{convert|135|km/h|kn|abbr=in}} and a pressure of 967 hPa, while weakening to a tropical storm at 12:00 UTC the same day. Around 03:00 UTC (11:00 a.m PST) of November 26, PAGASA reported that Tokage slightly intensified while the storm is re-intensifying in the South China Sea.{{cite report|title=Severe Weather Bulletin No. 22 re Tropical Storm "MARCE" (I.N. TOKAGE)|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_22_re_TS_MARCE_TOKAGE_issued_on_26NOV2016_1100H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 26, 2016|access-date=February 9, 2019}} On the next day, the JTWC reported that Tokage has regained its category 1 status, and had made its secondary peak intensity with {{convert|145|km/h|kn|abbr=in}} and a pressure of 963 hPa. Afterwards, Tokage rapidly weakened below typhoon intensity on 12:00 UTC the same day, below tropical storm intensity at 18:00 UTC, and both agencies discontinued advisories on 00:00 UTC of November 28. The PAGASA, however, discontinued advisories for Tropical Depression "Marce" 3 hours later, around 11 a.m. PST.{{cite report|title=Severe Weather Bulletin No. 26 re Tropical Depression "MARCE" (I.N. TOKAGE)|url=http://ndrrmc.gov.ph/attachments/article/2967/SWB_No_26_re_TD_MARCE_issued_on_28NOV2016_1100H.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 28, 2016|access-date=February 9, 2019}}

A total of 2,980 families were affected during Tokage's passing, and only 712 families evacuated to their designated evacuation centers and 67 families were served outside. A total of 46 municipalities and 9 cities on the regions Mimaropa, 6, 7, 8, 10, NIR and CAR suspended their classes during the storm, a total of 32 flights were cancelled, a total of 6 transmission lines were affected in Visayas, 2 landslides were reported on Sogod, Southern Leyte and Baybay, Leyte, 8 flooding incidents were reported around Oriental Mindoro, Romblon, and Negros Occidental. A total of 16 houses were destroyed during the storm (totally or partially), 40 hectares of palay to tillering stage and 15 hectares in ripening stage were damaged on some parts of Iloilo, and a total of ₱1,500,000 (US$28,788) as reported damages to infrastructure. In response, the DSWD provided a total of ₱24,9049.57 ($47,79.58 USD) to the affected families on Surigao del Norte and Surigao del Sur.{{cite report|title=SitRep No. 04 Preparedness Measures and Effects for Tropical Storm "MARCE" (I.N. TOKAGE)|url=http://www.ndrrmc.gov.ph/attachments/article/2968/Sitrep_No_4_re_Preparedness_Measures_and_Effects_of_TS_Marce_TOKAGE_as_of_26NOV2016.pdf|publisher=National Disaster Risk Reduction and Management Council|date=November 27, 2016|access-date=February 9, 2019}}

{{clear}}

{{Main|Typhoon Nock-ten}}

{{Infobox tropical cyclone small

| Basin = WPac

| Formed = December 20

| Dissipated = December 28

| Image = Nock-ten 2016-12-25 0210Z (gallery).jpg

| Track = Nock-ten 2016 track.png

| 10-min winds = 105

| 1-min winds = 140

| Pressure = 915

}}

Nock-ten was first noted as a tropical depression on December 21,{{cite web|title=RSMC Tropical Cyclone Advisory 210000 |url=http://tgftp.nws.noaa.gov/data/raw/wt/wtpq20.rjtd..txt |publisher=Japan Meteorological Agency |access-date=December 27, 2016 |archive-url=https://archive.today/20240524013424/https://www.webcitation.org/6mvD1Cpfo?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201612210000.htm |archive-date=May 24, 2024 |date=December 21, 2016 |url-status=dead }} and quickly organized into a tropical storm.{{cite web|title=RSMC Tropical Cyclone Advisory 211800 |url=http://tgftp.nws.noaa.gov/data/raw/wt/wtpq20.rjtd..txt |publisher=Japan Meteorological Agency |access-date=December 27, 2016 |archive-url=https://archive.today/20240523114115/https://www.webcitation.org/6mwqDyTf7?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201612211800.htm |archive-date=May 23, 2024 |date=December 21, 2016 |url-status=dead }} The system reached severe tropical storm intensity the following day,{{cite web|title=RSMC Tropical Cyclone Advisory 221800 |url=http://tgftp.nws.noaa.gov/data/raw/wt/wtpq20.rjtd..txt |publisher=Japan Meteorological Agency |access-date=December 27, 2016 |archive-url=https://archive.today/20240523114234/https://www.webcitation.org/6myrj3WqR?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201612221800.htm |archive-date=May 23, 2024 |date=December 22, 2016 |url-status=dead }} and then typhoon intensity the day after.{{cite web|title=RSMC Tropical Cyclone Advisory 231200 |url=http://tgftp.nws.noaa.gov/data/raw/wt/wtpq20.rjtd..txt |publisher=Japan Meteorological Agency |access-date=December 27, 2016 |archive-url=https://archive.today/20240523114153/https://www.webcitation.org/6myrh66jd?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201612231200.htm |archive-date=May 23, 2024 |date=December 23, 2016 |url-status=dead }} Around this time, a well-defined eye formed,{{cite web|title=Prognostic Reasoning for Typhoon 30W (Nock-ten) Warning Nr 10 |url=http://tgftp.nws.noaa.gov/data/raw/wd/wdpn31.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=December 27, 2016 |archive-url=https://archive.today/20240524013545/https://www.webcitation.org/6mysJ3EoV?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201612231500.htm |archive-date=May 24, 2024 |date=December 23, 2016 |url-status=dead }} and the storm began rapidly intensifying.{{cite web|title=Prognostic Reasoning for Typhoon 30W (Nock-ten) Warning Nr 11 |url=http://tgftp.nws.noaa.gov/data/raw/wd/wdpn31.pgtw..txt |publisher=Joint Typhoon Warning Center |access-date=December 27, 2016 |archive-url=https://archive.today/20240524013502/https://www.webcitation.org/6mysIixwj?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201612232000.htm |archive-date=May 24, 2024 |date=December 23, 2016 |url-status=dead }} Nock-ten reached its peak intensity as a Category 5-equivalent super typhoon with 1-minute sustained winds of {{convert|260|km/h|mph|abbr=on|round=5}}{{cite web |url=https://science.nrlmry.navy.mil/geoips/tcdat/tc16/WPAC/30W.NOCK-TEN/trackfile.txt |title=30W.NOCK-TEN Track File |publisher=Naval Research Laboratory |access-date=December 27, 2016 |archive-date=December 24, 2016 |archive-url=https://web.archive.org/web/20161224235422/http://www.nrlmry.navy.mil/tcdat/tc16/WPAC/30W.NOCK-TEN/trackfile.txt |url-status=live }} on December 25, becoming the strongest tropical cyclone recorded on Christmas Day anywhere in the world since at least 1960 in terms of 1-minute sustained winds. Shortly thereafter, land interaction imparted weakening, with warming cloud tops,{{cite web|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/warnings/wp3016prog.txt |title=Prognostic Reasoning for Typhoon 30W (Nock-ten) Warning Nr 17 |publisher=Joint Typhoon Warning Center |archive-url=https://archive.today/20240524013623/https://www.webcitation.org/6n1lOaoXK?url=http://gwydir.demon.co.uk/advisories/WDPN31-PGTW_201612250900.htm |archive-date=May 24, 2024 |url-status=dead}} and the typhoon made its first landfall over Catanduanes{{cite web|title=At 06:30 PM today, Typhoon #NinaPH has made landfall over Catanduanes.|url=https://twitter.com/dost_pagasa/status/812972339683991552|website=Twitter|publisher=PAGASA|access-date=December 27, 2016|date=December 25, 2016}} as a Category 4-equivalent super typhoon with 1-minute sustained winds of {{convert|250|km/h|mph|abbr=on|round=5}}. Nock-ten emerged into the South China Sea as a minimal typhoon,{{cite web|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/warnings/wp3016prog.txt|title=Prognostic Reasoning for Typhoon 30W (Nock-ten) Warning Nr 21 |date=December 26, 2016 |archive-url=https://archive.today/20240524013824/https://www.webcitation.org/6n4o36MB0?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201612260900.htm |archive-date=May 24, 2024 |access-date=December 27, 2016 |url-status=dead}}{{cite web|title=RSMC Tropical Cyclone Advisory 260900 |url=http://tgftp.nws.noaa.gov/data/raw/wt/wtpq20.rjtd..txt |publisher=Japan Meteorological Agency |access-date=December 27, 2016 |archive-url=https://archive.today/20240524013703/https://www.webcitation.org/6n4lmUbgH?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201612260900.htm |archive-date=May 24, 2024 |date=December 26, 2016 |url-status=dead }} where strong vertical wind shear associated with a cold surge event led to continued weakening,{{cite web|url=http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/warnings/wp3016prog.txt |title=Prognostic Reasoning for Tropical Storm 30W (Nock-ten) Warning Nr 24 |date=December 27, 2016 |archive-url=https://archive.today/20240524013745/https://www.webcitation.org/6n4o0MOjV?url=http://gwydir.demon.co.uk/advisories/WDPN32-PGTW_201612270300.htm |archive-date=May 24, 2024 |access-date=December 27, 2016 |url-status=dead }} with the low-level circulation center becoming exposed. The JMA issued its final advisory on the system late on December 27,{{cite web|title=RSMC Tropical Cyclone Advisory 271800 |url=http://tgftp.nws.noaa.gov/data/raw/wt/wtpq20.rjtd..txt |publisher=Japan Meteorological Agency |access-date=December 27, 2016 |archive-url=https://archive.today/20240523114316/https://www.webcitation.org/6n4lj0NIn?url=http://gwydir.demon.co.uk/advisories/WTPQ20-RJTD_201612271800.htm |archive-date=May 23, 2024 |date=December 27, 2016 |url-status=dead }} and the JTWC followed suit early on December 28.

{{clear}}

• On June 22, the JMA started to monitor a broad tropical depression that had developed about {{convert|190|km|mi|round=5|abbr=on}} to the southwest of Manila in the Philippines.{{cite web|title=List of weather charts on June 22, 2016 (WED)|url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/search_day.pl?lang=en&year=2016&month=6&day=22|date=June 22, 2016|access-date=October 4, 2024|publisher=Digital Typhoon}}{{cite report|url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201606230600.html |publisher=United States Joint Typhoon Warning Center |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans June 23, 2016 06z |url-status=dead |archive-url=https://www.webcitation.org/6mVa2pxKv?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201606230600.htm |archive-date=December 4, 2016 }} The system was located within a favourable environment for further development, but was not expected to significantly develop any further, as an upper-level low was expected to move over the system. The system moved northwestwards, before it weakened to a remnant low-pressure area on June 24.{{cite web|title=List of weather charts on June 24, 2016 (FRI)|url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/search_day.pl?lang=en&year=2016&month=6&day=24|date=June 24, 2016|access-date=October 4, 2024|publisher=Digital Typhoon}} However, the system's remnants were tracked until they made landfall on central Vietnam on June 27. The system was responsible for some heavy rainfall in Central and Southern Vietnam.{{cite web|title=THÔNG BÁO VÀ DỰ BÁO KHÍ HẬU THÁNG VIII, IX, X NĂM 2016|url=http://www.imh.ac.vn/files/doc/TBDBKH_T7_2016_final.pdf|website=imh.ac.vn|publisher=Vietnam Institute of Meteorology, Hydrology and Climate Change|access-date=September 3, 2016|date=July 11, 2016|language=vi|archive-url=https://web.archive.org/web/20160903015702/http://www.imh.ac.vn/files/doc/TBDBKH_T7_2016_final.pdf |archive-date=September 3, 2016}}
• The JMA upgraded a low-pressure area east of Taiwan to a tropical depression on August 6.{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-06T12:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/06/marine-weather-warning-for-gmdss-metarea-xi-2016-08-06t120000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 6, 2016|date=August 6, 2016|archive-date=2016-09-11|archive-url=https://web.archive.org/web/20160911224520/http://www.wis-jma.go.jp/cms/warning/2016/08/06/marine-weather-warning-for-gmdss-metarea-xi-2016-08-06t120000z/|url-status=dead}} The system made landfall over eastern China on August 9.
• On August 10, the JMA reported that a tropical depression had developed, about {{convert|300|km|mi|round=5|abbr=on}} to the southeast of Ishigaki Island.{{cite web|url=http://www.jma.go.jp/en/g3/|title=JMA WWJP25 Warning and Summary August 10, 2016 00z |archive-date=May 24, 2024 |access-date=August 12, 2016 |date=August 10, 2016 |agency=Japan Meteorological Agency |archive-url=https://archive.today/20240524000946/https://www.webcitation.org/6jgRjmEst?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201608100000.htm |url-status=dead}}{{cite web|date=August 10, 2016 |title=Significant Tropical Weather Advisory for the Western and South Pacific Oceans August 10, 2016 06z |archive-date=May 24, 2024 |agency=United States Joint Typhoon Warning Center |archive-url=https://archive.today/20240524000905/https://www.webcitation.org/6jgRb4hfv?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201608100600.htm |url=https://metoc.ndbc.noaa.gov/web/guest/jtwc |url-status=dead }} Over the next day the system moved north-westwards, within a marginal environment for further development, before it passed over northern Taiwan and moved into the East China Sea.{{cite web|url=http://www.jma.go.jp/en/g3/ |title=JMA WWJP25 Warning and Summary August 11, 2016 00z |agency=Japan Meteorological Agency |archive-date=May 24, 2024 |access-date=August 12, 2016 |date=August 11, 2016 |archive-url=https://archive.today/20240524001105/https://www.webcitation.org/6jiTvPJMF?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201608110000.htm |url-status=dead }}{{cite web|url=http://www.jma.go.jp/en/g3/ |date=August 11, 2016 |agency=Japan Meteorological Agency |archive-date=May 24, 2024 |archive-url=https://archive.today/20240524001147/https://www.webcitation.org/6jiUVnkYo?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201608110600.htm |access-date=August 12, 2016 |title=JMA WWJP25 Warning and Summary August 11, 2016 06z |url-status=dead }} The system subsequently continued moved westwards, before it was last noted as it made landfall on southern China later that day.{{cite web|url=http://www.jma.go.jp/en/g3/ |title=JMA WWJP25 Warning and Summary August 11, 2016 12z |agency=Japan Meteorological Agency |archive-date=May 22, 2024 |access-date=August 12, 2016 |archive-url=https://archive.today/20240522121949/https://www.webcitation.org/6ji3SXqap?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201608111200.htm |date=August 11, 2016 |url-status=dead }}
• During August 12, a tropical depression developed near the coast of Taiwan, about {{convert|160|km|mi|round=5|abbr=on}} to the southeast of Taipei.{{cite web|url=http://www.jma.go.jp/en/g3/|title=JMA WWJP25 Warning and Summary August 12, 2016 18z |agency=Japan Meteorological Agency |archive-date=May 24, 2024 |access-date=August 13, 2016 |archive-url=https://archive.today/20240524001749/https://www.webcitation.org/6jjUTpxyN?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201608121800.htm |date=August 12, 2016 |url-status=dead}} The system subsequently made landfall on the island, before it was last noted during the next day as it dissipated over Taiwan.{{cite web|url=http://www.jma.go.jp/en/g3/ |access-date=August 13, 2016 |title=JMA WWJP25 Warning and Summary August 13, 2016 00z |archive-date=May 24, 2024 |date=August 13, 2016 |archive-url=https://archive.today/20240524001710/https://www.webcitation.org/6jjUTfpgu?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201608130000.htm |agency=Japan Meteorological Agency |url-status=dead }}
• A tropical depression briefly appeared over the Gulf of Tonkin early on August 16.{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-16T00:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/16/marine-weather-warning-for-gmdss-metarea-xi-2016-08-16t000000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 16, 2016|date=August 16, 2016}}
• On August 23, a tropical depression developed over the South China Sea. {{citation needed span|text=However, the next day, it weakened to a low-pressure area.|date=August 2016}}
• Another tropical depression briefly formed northeast of the Mariana Islands on August 24.https://www.webcitation.org/6jzz6vTfu?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201608240600.htm
• A tropical depression formed north of Wake Island early on August 30, and it became extratropical on the next day.{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-30T00:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/30/marine-weather-warning-for-gmdss-metarea-xi-2016-08-30t000000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 30, 2016|date=August 30, 2016}}{{cite web|title=Marine Weather Warning for GMDSS Metarea XI 2016-08-31T06:00:00Z|url=http://www.wis-jma.go.jp/cms/warning/2016/08/31/marine-weather-warning-for-gmdss-metarea-xi-2016-08-31t060000z/|website=WIS Portal – GISC Tokyo|agency=Japan Meteorological Agency|access-date=August 31, 2016|date=August 31, 2016}}
• On September 10, the JMA had briefly monitored a tropical depression to the east of Okinawa.
• On October 15, the JMA reported that a tropical depression had entered the basin from the Central Pacific.https://www.webcitation.org/6lHjLsTns?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610150600.htm The system moved in a westward direction until dissipating several hours later on the same day.https://www.webcitation.org/6lHjLXVeU?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201610151200.htm
• On November 1, the JMA started to track a tropical depression about {{convert|704|km|mi|abbr=on}} east of Andersen Air Force Base, Guam.https://www.webcitation.org/6lhFCnrKY?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201611010600.htm https://www.webcitation.org/6lhFpz1dI?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201611010000.htm Later that same day, the JMA started issuing advisories on the depression whilst the JTWC had issued a Tropical Cyclone Formation Alert,https://www.webcitation.org/6ljuX8S5t?url=http://gwydir.demon.co.uk/advisories/WTPN21-PGTW_201611012300.htm {{cite web|title=TD |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201611011800.htm |date=November 1, 2016 |archive-date=May 24, 2024 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524011534/https://www.webcitation.org/6llhClHgN?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201611011800.htm |access-date=May 22, 2017}} though they canceled it early on November 2.https://www.webcitation.org/6ljuOnNGc?url=http://gwydir.demon.co.uk/advisories/ABPW10-PGTW_201611022330.htm The system moved northward until the JMA issued its final advisory as it interacted with the outer rainbands of the nearby Typhoon Meari and became extratropical on November 5.{{cite web |title=TD |url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201611040300.htm |date=November 4, 2016 |agency=Japan Meteorological Agency |url-status=dead |archive-url=https://archive.today/20240524011454/https://www.webcitation.org/6llh4a6D8?url=http://gwydir.demon.co.uk/advisories/WTPQ21-RJTD_201611040300.htm |archive-date=May 24, 2024 |access-date=May 22, 2017 }}
• During December 10, the JMA started to monitor a tropical depression that had developed about {{convert|415|km|mi|round=5|abbr=on}} to the southeast of Ho-Chi-Minh City in Southern Vietnam.{{cite web|url=http://www.jma.go.jp/en/g3/|date=December 10, 2016 |title=JMA WWJP25 Warning and Summary December 10, 2016 12z |agency=Japan Meteorological Agency |archive-date=May 24, 2024 |access-date=December 18, 2016 |archive-url=https://archive.today/20240524013342/https://www.webcitation.org/6menY9wuQ?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201612101200.htm |url-status=dead}} Over the next couple of days, the system moved slowly westwards without developing any further, before it made landfall on and dissipated over Southern Vietnam during December 13. The depression had caused torrential rains and heavy flooding since mid December in Central and Southern Vietnam, where at least 24 people were killed and total damages had reached to at least ₫1.21 trillion (US$53.4 million) in Vietnam.http://phongchongthientai.vn/resources/files/ccsfc21121610404501--bao-cao-nhanh-ngay-20-12-2016.doc/{{Dead link|date=September 2018 |bot=InternetArchiveBot |fix-attempted=yes }}
• On December 27, the JMA briefly monitored on a tropical depression located near Chuuk, which dissipated later on the same day.https://www.webcitation.org/6n4oTaxWo?url=http://gwydir.demon.co.uk/advisories/WWJP25-RJTD_201612270600.htm

{{Tropical cyclone naming}}

Within the Northwest Pacific Ocean, both the Japan Meteorological Agency (JMA) and the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assign names to tropical cyclones that develop in the Western Pacific, which can result in a tropical cyclone having two names.{{cite web|title=Monthly Tropical Cyclone Summary December 1999 |access-date=October 1, 2013 |url-status=live |author=Padgett, Gary |publisher=Australian Severe Weather |url=http://www.australiasevereweather.com/cyclones/2000/summ9912.htm |archive-url=https://web.archive.org/web/20120211074501/http://australiasevereweather.com/cyclones/2000/summ9912.htm |archive-date=February 11, 2012 }} The Japan Meteorological Agency's RSMC Tokyo — Typhoon Center assigns international names to tropical cyclones on behalf of the World Meteorological Organization's Typhoon Committee, should they be judged to have 10-minute sustained windspeeds of {{convert|65|km/h|mph|round=5|abbr=on}}.{{cite web|title=Typhoon Committee Operational Manual 2013 |url=http://www.wmo.int/pages/prog/www/tcp/documents/TCP-23EDITION2013.pdf |archive-url=https://web.archive.org/web/20130801020116/http://www.wmo.int/pages/prog/www/tcp/documents/TCP-23EDITION2012.pdf |publisher=World Meteorological Organization |archive-date=August 1, 2013 |pages=37–38 |date=February 21, 2013 |author=The Typhoon Committee |access-date=October 1, 2013 |url-status=dead }} PAGASA names to tropical cyclones which move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N and 25°N even if the cyclone has had an international name assigned to it. The names of significant tropical cyclones are retired, by both PAGASA and the Typhoon Committee. Should the list of names for the Philippine region be exhausted then names will be taken from an auxiliary list of which the first ten are published each season. Unused names are marked in {{tcname unused}}.

{{main|List of retired Pacific typhoon names}}

During the season 26 tropical storms developed in the Western Pacific and each one was named by the JMA, when the system was judged to have 10-minute sustained windspeeds of {{convert|65|km/h|mph|round=5|abbr=on}}. The JMA selected the names from a list of 140 names, that had been developed by the 14 members nations and territories of the ESCAP/WMO Typhoon Committee.{{cite journal|author=Zhou, Xiao|author2=Lei, Xiaotu|year=2012|title=Summary of retired typhoons within the Western North Pacific Ocean|volume=1|issue=1|publisher=The Economic and Social Commission for Asia and the Pacific/World Meteorological Organization's Typhoon Committee|pages=23–32|issn=2225-6032|journal=Tropical Cyclone Research and Review|access-date=December 21, 2014|url=http://tcrr.typhoon.gov.cn/EN/article/downloadArticleFile.do?attachType=PDF&id=7|doi=10.6057/2012TCRR01.03|archive-url=https://web.archive.org/web/20170812172856/http://tcrr.typhoon.gov.cn/EN/article/downloadArticleFile.do?attachType=PDF&id=7|archive-date=August 12, 2017|url-status=dead}} During the season, the name Rai was used for the first time after it replaced the name Fanapi in the 2010 season.

After the season the Typhoon Committee retired the names Meranti, Sarika, Haima and Nock-ten from the naming lists, and in February 2018, the names were subsequently replaced with Nyatoh, Trases, Mulan, and Hinnamnor for future seasons, respectively.{{cite web|url=http://www.typhooncommittee.org/tc-retired-tropical-name-list/|title=List of Retired Tropical Cyclone Names {{!}} Typhoon Committee|website=www.typhooncommittee.org|access-date=2018-03-04}}

{{main|List of retired Philippine typhoon names}}

During the season PAGASA used its own naming scheme for the 14 tropical cyclones, that either developed within or moved into their self-defined area of responsibility.{{cite web|title=Philippine Tropical Cyclone Names|access-date=April 18, 2015|agency=PAGASA|url=http://www.pagasa.dost.gov.ph/index.php/learning-tools/94-weather/278-philippine-tropical-cyclone-names|url-status=dead|archive-url=https://web.archive.org/web/20161228042559/http://www.pagasa.dost.gov.ph/index.php/learning-tools/94-weather/278-philippine-tropical-cyclone-names|archive-date=December 28, 2016}}{{cite news|title=PHL ends 2015 with less typhoons; to decommission 2 killer cyclones |access-date=December 22, 2015 |newspaper=The Philippine Star |url=http://www.philstar.com/headlines/2015/12/22/1535360/pagasa-less-typhoons-year-due-el-nino |archive-url=https://web.archive.org/web/20160313101946/http://www.philstar.com/headlines/2015/12/22/1535360/pagasa-less-typhoons-year-due-el-nino |url-status=live |archive-date=March 13, 2016 |author=Patricia Lourdes Viray }} The names were taken from a list of names, that was last used during 2012 and were used again during 2020. All of the names are the same except for Pepito, which replaced the name Pablo after it was retired. The name Gardo was replaced by Gomer after Gardo was added to PAGASA's main list replacing Glenda, which was retired after the 2014 season.

After the season the names Karen, Lawin and Nina were retired by PAGASA, as they had caused over ₱1 billion in damages. They were subsequently replaced on the list with the names Kristine, Leon and Nika{{cite web|title=Philippine Tropical Cyclone Names|url=http://pagasa.dost.gov.ph/index.php/learning-tools/94-weather/278-philippine-tropical-cyclone-names|publisher=PAGASA|date=January 2017|access-date=January 17, 2017|archive-url=https://web.archive.org/web/20161228042559/http://www.pagasa.dost.gov.ph/index.php/learning-tools/94-weather/278-philippine-tropical-cyclone-names|archive-date=2016-12-28|url-status=dead}} for the 2020 Pacific typhoon season.

{{clear}}

This table will list all the storms that developed in the northwestern Pacific Ocean west of the International Date Line and north of the equator during 2016. It will include their intensity, duration, name, areas affected, deaths, and damage totals. Classification and intensity values will be based on estimations conducted by the JMA. All damage figures will be in 2016 USD. Damages and deaths from a storm will include when the storm was a precursor wave or an extratropical cyclone.

{{Pacific areas affected (Top)|year=2016}}

|-

| 01W || {{Sort|20160525|May 25–27}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|000|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1000|{{convert|1000|hPa|inHg|sigfig=4|abbr=on}}}} || South China || {{ntsp|9140000||$}} || {{Sort|0|None}} || {{cite conference|pages=1–2 |conference=ESCAP/WMO Typhoon Committee |title=Member Report: China |author=CMA |publisher=ESCAP/WMO Typhoon Committee |url=http://www.typhooncommittee.org/11IWS/docs/Members%20Report/2016%E5%B9%B4CHINA%20REPORT-10.24.pdf |date=October 27, 2016 |access-date=October 30, 2016 |conference-url=http://www.typhooncommittee.org/11IWS/ |archive-date=March 6, 2017 |archive-url=https://web.archive.org/web/20170306093110/http://www.typhooncommittee.org/11IWS/docs/Members%20Report/2016%E5%B9%B4CHINA%20REPORT-10.24.pdf |url-status=dead }}

|-

| TD || {{Sort|20160622|June 22–23}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TD}}|{{Sort|1006|{{convert|1006|hPa|inHg|sigfig=4|abbr=on}}}} || Vietnam || {{ntsh|0}} None || {{Sort|0|None}} ||

|-

| Ambo || {{Sort|20160625|June 25–28}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TD}}|{{Sort|1004|{{convert|1004|hPa|inHg|sigfig=4|abbr=on}}}} || Philippines, South China || {{ntsh|0}} None || {{Sort|0|None}} ||

|-

| Nepartak (Butchoy) || {{Sort|20160702|July 2–10}} || bgcolor=#{{storm colour|VITY}}|{{Sort|3|Violent typhoon}} || bgcolor=#{{storm colour|VITY}}|{{Sort|205|{{convert|205|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|VITY}}|{{Sort|0900|{{convert|900|hPa|inHg|sigfig=4|abbr=on}}}} || Caroline Islands, Mariana Islands, Philippines, Ryukyu Islands, Taiwan, East China || {{ntsp|1886000000||$}} || 111 ||{{cite web|title=Report on TC's Key Activities and Main Events in the Region, 2016|url=http://www.typhooncommittee.org/49th/Docs49/item%206/6.1%20REport%20TC%20Chair.pdf|date=January 9, 2017|publisher=ESCAP/WMO Typhoon Committee}}

|-

| 03W || {{Sort|20160715|July 15–20}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|000|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1006|{{convert|1006|hPa|inHg|sigfig=4|abbr=on}}}} || Ryukyu Islands || {{ntsh|0}} None || {{Sort|0|None}} ||

|-

| Lupit || {{Sort|20160722|July 22–24}} || bgcolor=#{{storm colour|TS}}|{{Sort|1|Tropical storm}} || bgcolor=#{{storm colour|TS}}|{{Sort|075|{{convert|75|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TS}}|{{Sort|1000|{{convert|1000|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{Sort|0|None}} || {{Sort|0|None}} ||

|-

| Mirinae || {{Sort|20160725|July 25–28}} || bgcolor=#{{storm colour|STS}}|{{Sort|2|Severe tropical storm}} || bgcolor=#{{storm colour|STS}}|{{Sort|100|{{convert|100|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|STS}}|{{Sort|0980|{{convert|980|hPa|inHg|sigfig=4|abbr=on}}}} || South China, Vietnam, Laos, Thailand || {{ntsp|380580000||$}} || {{nts|7}} || [http://phongchongthientai.mard.gov.vn/FileUpload/2019-08/PcUlNnBeEWxflgyd2016-00.%20Thiet%20hai%20nam%202016_31.12.2017_ra%20soat%20cap%20nhat.pdf 2016 VIETNAM REPORT]{{cite web|title=Phó Thủ tướng chỉ đạo ứng phó thiên tai, bão lũ|url=http://baochinhphu.vn/Doi-song/Pho-Thu-tuong-chi-dao-ung-pho-thien-tai-bao-lu/283617.vgp |publisher=Vietnam Government|access-date=August 8, 2016|language=vi|date=August 8, 2016}}

|-

| Nida (Carina) || {{Sort|20160729|July 29 – August 3}} || bgcolor=#{{storm colour|STS}}|{{Sort|2|Severe tropical storm}} || bgcolor=#{{storm colour|STS}}|{{Sort|110|{{convert|110|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|STS}}|{{Sort|0975|{{convert|975|hPa|inHg|sigfig=4|abbr=on}}}} || Philippines, Taiwan, China, Hong Kong, Vietnam || {{ntsp|316400000||$}} || {{nts|6}} || {{cite web|url=http://thoughtleadership.aonbenfield.com/Documents/20160908-ab-analytics-if-august-global-recap.pdf|title=Global Catastrophe Recap August 2016|website=thoughtleadership.aonbenfield.com|publisher=Aon Benfield|access-date=September 8, 2017|archive-date=July 19, 2017|archive-url=https://web.archive.org/web/20170719062342/http://thoughtleadership.aonbenfield.com/Documents/20160908-ab-analytics-if-august-global-recap.pdf|url-status=dead}}

|-

| Omais || {{Sort|20160802|August 2–9}} || bgcolor=#{{storm colour|STS}}|{{Sort|2|Severe tropical storm}} || bgcolor=#{{storm colour|STS}}|{{Sort|110|{{convert|110|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|STS}}|{{Sort|0975|{{convert|975|hPa|inHg|sigfig=4|abbr=on}}}} || Mariana Islands, Japan, Russia || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20160806|August 6–9}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}}|| bgcolor=#{{storm colour|TD}}|{{Sort|0998|{{convert|998|hPa|inHg|sigfig=4|abbr=on}}}} || Ryukyu Islands, East China || {{ntsh|0}} None || None ||

|-

| Conson || {{Sort|20160807|August 7–14}} || bgcolor=#{{storm colour|TS}}|{{Sort|1|Tropical storm}} || bgcolor=#{{storm colour|TS}}|{{Sort|085|{{convert|85|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TS}}|{{Sort|0985|{{convert|985|hPa|inHg|sigfig=4|abbr=on}}}} || Japan, Russia || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20160810|August 10–13}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}}|| bgcolor=#{{storm colour|TD}}|{{Sort|0996|{{convert|996|hPa|inHg|sigfig=4|abbr=on}}}} || Ryukyu Islands, Taiwan, East China || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20160810|August 10–12}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}}|| bgcolor=#{{storm colour|TD}}|{{Sort|1010|{{convert|1010|hPa|inHg|sigfig=4|abbr=on}}}} || Midway Atoll || {{ntsh|0}} None || None ||

|-

| Chanthu || {{Sort|20160812|August 12–17}} || bgcolor=#{{storm colour|strong}}|{{Sort|2|Severe tropical storm}} || bgcolor=#{{storm colour|strong}}|{{Sort|100|{{convert|100|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|strong}}|{{Sort|0980|{{convert|980|hPa|inHg|sigfig=4|abbr=on}}}} || Japan, Russian Far East || {{ntsp|94700000||$}} || None ||

|-

| TD || {{Sort|20160812|August 12–13}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}}|| bgcolor=#{{storm colour|TD}}|{{Sort|1002|{{convert|1002|hPa|inHg|sigfig=4|abbr=on}}}} || Taiwan || {{ntsh|0}} None || None ||

|-

| Dianmu || {{Sort|20160815|August 15–19}} || bgcolor=#{{storm colour|TS}}|{{Sort|1|Tropical storm}} || bgcolor=#{{storm colour|TS}}|{{Sort|075|{{convert|75|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TS}}|{{Sort|0980|{{convert|980|hPa|inHg|sigfig=4|abbr=on}}}} || China, Vietnam, Laos, Thailand, Myanmar, Bangladesh, India || {{ntsp|570057000||$}} || {{sort|023|23}} || {{cite web|title=Tình hình kinh tế — xã hội 8 tháng năm 2016|publisher=General Statistics of Vietnam|access-date=September 3, 2016|archive-date=September 3, 2016|language=vi|url=http://www.gso.gov.vn/Default.aspx?tabid=621&ItemID=16035|archive-url=https://web.archive.org/web/20160903033655/http://www.gso.gov.vn/Default.aspx?tabid=621&ItemID=16035 }}

|-

| TD || {{Sort|20160815|August 15–16}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|0996|{{convert|996|hPa|inHg|sigfig=4|abbr=on}}}} || South China, Vietnam || {{ntsh|0}} None || None ||

|-

| Mindulle || {{Sort|20160817|August 17–23}} || bgcolor=#{{storm colour|TY}}|{{Sort|3|Strong typhoon}} || bgcolor=#{{storm colour|TY}}|{{Sort|120|{{convert|120|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TY}}|{{Sort|0975|{{convert|975|hPa|inHg|sigfig=4|abbr=on}}}} || Mariana Islands, Japan || {{ntsp|448300000||$}} || {{sort|003|3}} ||

|-

| Lionrock (Dindo) || {{Sort|20160817|August 17–30}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|3|Very strong typhoon}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|165|{{convert|165|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|VSTY}}|{{Sort|0940|{{convert|940|hPa|inHg|sigfig=4|abbr=on}}}} || Japan, Russia, Northeast China, North Korea || {{ntsp|3938000000||$}} || {{sort|550|550}} ||{{cite web|title=Global Catastrophe Recap October 2016|url=http://thoughtleadership.aonbenfield.com/Documents/20161109-ab-analytics-if-october-global-recap.pdf|website=Aon Benfield|access-date=17 November 2016|archive-date=18 November 2016|archive-url=https://web.archive.org/web/20161118040804/http://thoughtleadership.aonbenfield.com/Documents/20161109-ab-analytics-if-october-global-recap.pdf|url-status=dead}}

|-

| Kompasu || {{Sort|20160818|August 18–21}} || bgcolor=#{{storm colour|TS}}|{{Sort|1|Tropical storm}} || bgcolor=#{{storm colour|TS}}|{{Sort|065|{{convert|65|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TS}}|{{Sort|0994|{{convert|994|hPa|inHg|sigfig=4|abbr=on}}}} || Japan, Russian Far East || {{ntsh|0}} None || {{sort|001|1}} ||

|-

| TD || {{Sort|20160823|August 23–24}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1000|{{convert|1000|hPa|inHg|sigfig=4|abbr=on}}}} || Philippines || {{ntsh|0}} None || None ||

|-

| 14W || {{Sort|20160824|August 24}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TD}}|{{Sort|1002|{{convert|1002|hPa|inHg|sigfig=4|abbr=on}}}}|| Mariana Islands || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20160824|August 24}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1000|{{convert|1000|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20160825|August 27}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1004|{{convert|1004|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20160830|August 30–31}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1004|{{convert|1004|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh|0}} None || None ||

|-

| Namtheun (Enteng) || {{Sort|20160831|August 31 – September 5}} || bgcolor=#{{storm colour|TY}}|{{Sort|3|Strong typhoon}} || bgcolor=#{{storm colour|TY}}|{{Sort|130|{{convert|130|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TY}}|{{Sort|0955|{{convert|955|hPa|inHg|sigfig=4|abbr=on}}}} || Taiwan, South Korea, Japan || {{ntsh|0}} None || None ||

|-

| Malou || {{Sort|20160905|September 5–7}} || bgcolor=#{{storm colour|TS}}|{{Sort|1|Tropical storm}} || bgcolor=#{{storm colour|TS}}|{{Sort|075|{{convert|75|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TS}}|{{Sort|1000|{{convert|1000|hPa|inHg|sigfig=4|abbr=on}}}}|| Japan || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|2016907|September 7–8}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|0998|{{convert|998|hPa|inHg|sigfig=4|abbr=on}}}} || Japan || {{ntsh|0}} None || None ||

|-

| Meranti (Ferdie) || {{Sort|20160909|September 8–16}} || bgcolor=#{{storm colour|VITY}}|{{Sort|3|Violent typhoon}} || bgcolor=#{{storm colour|VITY}}|{{Sort|220|{{convert|220|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VITY}}|{{Sort|0890|{{convert|890|hPa|inHg|sigfig=4|abbr=on}}}} || Philippines, Taiwan, Mainland China, South Korea || {{ntsp|4792000000||$}} || {{sort|047|47}} || {{cite web|title=Death toll rises to 15 after typhoon batters China, Taiwan|url=http://www.ctvnews.ca/world/death-toll-rises-to-15-after-typhoon-batters-china-taiwan-1.3076411|date=September 17, 2016|publisher=CTVNews}}{{cite web|title=SitRep No. 9 re Preparedness Measures and Effects of Typhoon FERDIE (MERANTI)|url=http://www.ndrrmc.gov.ph/attachments/article/2913/SitRep_No_09_re_Preparedness_Measures_and_Effects_of_Typhoon_FERDIE_(MERANTI)_Covering_the_0600H_20SEP2016_to_0600H_21SEP2016.pdf|date=September 21, 2016|publisher=NDRRMC}}

|-

| TD || {{Sort|20160909|September 9–10}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1008|{{convert|1008|hPa|inHg|sigfig=4|abbr=on}}}} || None || None || None ||

|-

| TD || {{Sort|20160910|September 10}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1008|{{convert|1008|hPa|inHg|sigfig=4|abbr=on}}}} || Taiwan || None || None ||

|-

| 17W || {{Sort|20160910|September 10–12}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|{{convert|55|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|TD}}|{{Sort|1000|{{convert|1000|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh|0}} None || None ||

|-

| Rai || {{Sort|20160911|September 11–13}} || bgcolor=#{{storm colour|TS}}|{{Sort|1| Tropical storm}} || bgcolor=#{{storm colour|TS}}|{{Sort|065|{{convert|65|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|TS}}|{{Sort|0996|{{convert|996|hPa|inHg|sigfig=4|abbr=on}}}} || Vietnam, Laos, Thailand, Cambodia || {{ntsp|73960000||$}} || {{sort|014|14}} ||

|-

| Malakas (Gener) || {{Sort|20160911|September 11–20}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|3|Very strong typhoon}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|175|{{convert|175|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|0930|{{convert|930|hPa|inHg|sigfig=4|abbr=on}}}} || Mariana Islands, Taiwan, Japan || {{ntsp|300000000||$}} || {{sort|001|1}} || {{cite web |url=http://www.yomiuri.co.jp/local/kagoshima/news/20161014-OYTNT50058.html |title=農業被害総額７７億円 台風１６号 : 地域 : 読売新聞（Yomiuri Online） |access-date=2016-10-16 |archive-date=2016-10-18 |archive-url=https://web.archive.org/web/20161018222405/http://www.yomiuri.co.jp/local/kagoshima/news/20161014-OYTNT50058.html |url-status=dead }}{{cite web |url=http://www.sankei.com/affairs/news/160921/afr1609210027-n1.html |title=台風１６号、２０府県で被害 ２人死亡、住宅被害も - 産経ニュース |access-date=2016-10-16 |archive-date=2016-10-22 |archive-url=https://web.archive.org/web/20161022023539/http://www.sankei.com/affairs/news/160921/afr1609210027-n1.html |url-status=dead }}

|-

| Megi (Helen) || {{Sort|20160922|September 22–29}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|3|Very strong typhoon}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|155|{{convert|155|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|VSTY}}|{{Sort|0945|{{convert|945|hPa|inHg|sigfig=4|abbr=on}}}}|| Caroline Islands, Ryukyu Islands, Taiwan, South China, East China || {{ntsp|1567000000||$}} || {{sort|052|52}} || {{cite web|url=http://www.cna.com.tw/news/firstnews/201610020180-1.aspx|title=颱風梅姬農損逾25億 嘉義雲林最慘重|date=2 October 2016 |publisher=中央社|access-date=2016-10-02}}{{in lang|zh-tw}}

|-

| Chaba (Igme) || {{Sort|20160924|September 24 – October 5}} || bgcolor=#{{storm colour|VITY}}|{{Sort|3|Violent typhoon}} || bgcolor=#{{storm colour|VITY}}|{{Sort|215|{{convert|215|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|VITY}}|{{Sort|0905|{{convert|905|hPa|inHg|sigfig=4|abbr=on}}}}|| Mariana Islands, South Korea, Japan, Russian Far East || {{ntsp|129000000||$}} || {{sort|010|10}} || {{cite news|url=https://www.koreatimes.co.kr/www/news/nation/2016/10/116_215496.html|title=Typhoon Chaba leaves hundreds of victims|author=Kim, Bo-eun|date=6 October 2016|newspaper=Korea Times|access-date=7 October 2016}}{{cite web|url=http://thoughtleadership.aonbenfield.com/Documents/20161109-ab-analytics-if-october-global-recap.pdf|title=Global Catastrophe Recap October 2016|website=thoughtleadership.aonbenfield.com|publisher=Aon Benfield|access-date=November 9, 2017|archive-date=February 14, 2017|archive-url=https://web.archive.org/web/20170214111722/http://thoughtleadership.aonbenfield.com/Documents/20161109-ab-analytics-if-october-global-recap.pdf|url-status=dead}}

|-

| Songda || {{Sort|20161004|October 4–13}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|3|Very strong typhoon}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|185|{{convert|185|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|0925|{{convert|925|hPa|inHg|sigfig=4|abbr=on}}}} || Pacific Northwest || {{ntsh|0}} None || None ||

|-

| Aere (Julian) || {{Sort|20161004|October 4–14}} || bgcolor=#{{storm colour|STS}}|{{Sort|2|Severe tropical storm}} || bgcolor=#{{storm colour|STS}}|{{Sort|110|{{convert|110|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|STS}}|{{Sort|0975|{{convert|975|hPa|inHg|sigfig=4|abbr=on}}}} || Philippines, Taiwan, South China, Vietnam, Laos, Thailand, Cambodia || {{ntsp|209000000||$}} || {{sort|037|37}} ||

|-

| Sarika (Karen) || {{Sort|20161013|October 13–19}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|3|Very strong typhoon}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|175|{{convert|175|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VSTY}}|{{Sort|0935|{{convert|935|hPa|inHg|sigfig=4|abbr=on}}}} || Philippines, South China, Vietnam || {{ntsp|894000000||$}} || {{Sort|001|1}} || {{cite web|title=SitRep_No_08_re_Preparedness_Measures_and_Effects_of_Typhoon_KAREN|url=http://www.ndrrmc.gov.ph/attachments/article/2941/SitRep_No_08_re_Preparedness_Measures_and_Effects_of_Typhoon_KAREN_SARIKA_covering_the_period_190600H_to_200800H_October_2016.pdf|access-date=October 20, 2016|publisher=NDRRMC}}{{Dead link|date=May 2019 |bot=InternetArchiveBot |fix-attempted=yes }}{{cite web|url=http://www.chinanews.com/gj/2016/10-20/8038167.shtml|title=台风暴雨灾害致越南60人伤亡|website=中国新闻网|publisher=China Press|access-date=October 20, 2016}}{{cite web|url= http://www.weather.com.cn/index/gjtq/06/1358947.shtml|title="莎莉嘉"袭击菲律宾 造成6人死亡26名渔民失踪|website=中国天气网|publisher=China Meterelogical Agency|access-date=October 20, 2016}}

|-

| Haima (Lawin) || {{Sort|20161014|October 14–21}} || bgcolor=#{{storm colour|VITY}}|{{Sort|3|Violent typhoon}} || bgcolor=#{{storm colour|VITY}}|{{Sort|215|{{convert|215|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VITY}}|{{Sort|0900|{{convert|900|hPa|inHg|sigfig=4|abbr=on}}}} || Caroline Islands, Philippines, Taiwan, China, South China, Hong Kong, East China, Japan || {{ntsp|972200000||$}} || {{sort|019|19}} || {{cite web|title=SitRep No.9 re Preparedness Measures & Effects of Super TY LAWIN (I.N. HAIMA)|url=http://www.ndrrmc.gov.ph/attachments/article/2946/Sitrep_No_09_re_Preparedness_Measures_and_Effects_of_Super_Typhoon_LAWIN_HAIMA_as_of_25OCT2016_0800H.pdf|access-date=October 25, 2016|publisher=NDRRMC}}{{cite web|title=Typhoon Haima leaves one dead in Hong Kong as city counts the cost|url=http://www.scmp.com/news/hong-kong/health-environment/article/2038960/its-finally-here-heavy-rain-and-stronger-winds|date=October 21, 2016|publisher=South China Morning Post}}{{cite web|title='Lawin': 18 dead, 40 thousand people still in shelters|url=http://newsinfo.inquirer.net/829899/lawin-18-dead-40-thousand-people-still-in-shelters|date=October 22, 2016|publisher=Inquirer}}

|-

| TD || {{Sort|20161015|October 15}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1008|{{convert|1008|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh|0}} None || None ||

|-

| Meari || {{Sort|20161030|October 30 – November 7}} || bgcolor=#{{storm colour|TY}}|{{Sort|3|Strong typhoon}} || bgcolor=#{{storm colour|TY}}|{{Sort|140|{{convert|140|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TY}}|{{Sort|0960|{{convert|960|hPa|inHg|sigfig=4|abbr=on}}}} || Mariana Islands || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20161031|October 31}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1008|{{convert|1008|hPa|inHg|sigfig=4|abbr=on}}}} || Mariana Islands || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20161101|November 1–5}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|TD}}|{{Sort|0998|{{convert|998|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh|0}} None || None ||

|-

| TD || {{Sort|20161102|November 2–6}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TD}}|{{Sort|1004|{{convert|1004|hPa|inHg|sigfig=4|abbr=on}}}} || Borneo, Vietnam, Cambodia || {{ntsp|111800000||$}} || {{sort|015|15}} || {{cite web|title=Death Toll From Floods in Central Coastal Vietnam Reaches 15|url=http://www.rfa.org/english/news/vietnam/death-toll-from-floods-in-central-coastal-vietnam-reaches-15-11092016155927.html|date=November 9, 2016|publisher=Radio Free Asia}}{{cite web | url=http://thanhnien.vn/thoi-su/mua-lu-cuon-troi-hon-1000-ti-dong-763151.html | title=Mưa lũ 'cuốn trôi' hơn 1.000 tỉ đồng | date=8 November 2016 }}

|-

| Ma-on || {{Sort|20161108|November 8–13}} || bgcolor=#{{storm colour|TS}}|{{Sort|1|Tropical storm}} || bgcolor=#{{storm colour|TS}}|{{Sort|065|{{convert|65|km/h|mph|abbr=on|round=5}}}}|| bgcolor=#{{storm colour|TS}}|{{Sort|1002|{{convert|1002|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh}} None || None ||

|-

| 28W || {{Sort|20161109|November 9–12}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|000|Not specified}} || bgcolor=#{{storm colour|TD}}|{{Sort|1008|{{convert|1008|hPa|inHg|sigfig=4|abbr=on}}}} || Marshall Islands || {{ntsh|0}} None || None ||

|-

| Tokage (Marce) || {{Sort|20161124|November 24–28}} || bgcolor=#{{storm colour|STS}}|{{Sort|2|Severe tropical storm}} || bgcolor=#{{storm colour|STS}}|{{Sort|095|{{convert|95|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|STS}}|{{Sort|0992|{{convert|992|hPa|inHg|sigfig=4|abbr=on}}}} || Philippines, Vietnam || {{ntsp|30000||$}} || {{sort|001|1}} || {{cite web|title=Sitrep No. 04 re Preparedness Measures and Effects for TS MARCE (TOKAGE)|url=http://www.ndrrmc.gov.ph/attachments/article/2968/SitRep_No_04_re_Preparedness_Measures_and%20_Effects_for_Tropical_Storm_MARCE_(I.N%20TOKAGE)_26November2016_2000H.pdf|date=November 27, 2016|publisher=NDRRMC}}

|-

| TD || {{Sort|20161210|December 10–13}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|055|{{convert|55|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|TD}}|{{Sort|1004|{{convert|1004|hPa|inHg|sigfig=4|abbr=on}}}} || Vietnam || {{ntsp|146190000||$}} || {{sort|031|31}} || {{cite web |url=http://vnexpress.net/tin-tuc/thoi-su/24-nguoi-chet-do-mua-lu-mien-trung-tuan-qua-3515652.html |title=24 người chết do mưa lũ miền Trung tuần qua - VnExpress |access-date=2016-12-19 |archive-date=2016-12-19 |archive-url=https://web.archive.org/web/20161219215154/http://vnexpress.net/tin-tuc/thoi-su/24-nguoi-chet-do-mua-lu-mien-trung-tuan-qua-3515652.html |url-status=dead }}

|-

| Nock-ten (Nina) || {{Sort|20161220|December 20–28}} || bgcolor=#{{storm colour|VITY}}|{{Sort|3|Violent typhoon}} || bgcolor=#{{storm colour|VITY}}|{{Sort|195|{{convert|195|km/h|mph|abbr=on|round=5}}}} || bgcolor=#{{storm colour|VITY}}|{{Sort|0915|{{convert|915|hPa|inHg|sigfig=4|abbr=on}}}} || Caroline Islands, Philippines, Vietnam || {{ntsp|123000000||$}} || {{sort|013|13}} || {{cite web|url=http://www.ndrrmc.gov.ph/attachments/article/2975/Sitrep_No_13_re_Preparedness_Measures_and_Effects_of_TY_NINA_NOCK-TEN_as_of_09JAN2017_0800H.pdf|archive-url=https://web.archive.org/web/20200504160427/http://www.ndrrmc.gov.ph/attachments/article/2975/Sitrep_No_13_re_Preparedness_Measures_and_Effects_of_TY_NINA_NOCK-TEN_as_of_09JAN2017_0800H.pdf|url-status=dead|archive-date=May 4, 2020|title=Sitrep_No_13_re_Preparedness_Measures_and_Effects_of_TY_NINA_NOCK-TEN|date=January 9, 2017}}

|-

| TD || {{Sort|20161227|December 27}} || bgcolor=#{{storm colour|TD}}|{{Sort|0|Tropical depression}} || bgcolor=#{{storm colour|TD}}|{{Sort|045|Not specified}}|| bgcolor=#{{storm colour|TD}}|{{Sort|1004|{{convert|1004|hPa|inHg|sigfig=4|abbr=on}}}} || None || {{ntsh|0}} None || None ||

|-

{{TC Areas affected (Bottom)|TC's=51 systems|dates=May 25 – December 28|winds={{convert|220|km/h|mph|abbr=on|round=5}}|pres={{convert|890|hPa|inHg|sigfig=4|abbr=on}}|damage={{ntsp|16961550000||$}}|deaths=942|Refs=}}

{{Portal|Tropical cyclones}}

• Weather of 2016
• Tropical cyclones in 2016
• Pacific typhoon season
• 2016 Atlantic hurricane season
• 2016 Pacific hurricane season
• 2016 North Indian Ocean cyclone season
• South-West Indian Ocean cyclone seasons: 2015–16, 2016–17
• Australian region cyclone seasons: 2015–16, 2016–17
• South Pacific cyclone seasons: 2015–16, 2016–17

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{{Reflist|30em}}

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{{TC Decades|Year=2010|basin=Pacific|type=typhoon}}

{{Tropical cyclone season|2016}}

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Category:Pacific typhoon seasons

Category:Articles which contain graphical timelines

2016 WPac