User:Tavantius/sandbox3

{{Most active typhoon seasons}}

The 1967 Pacific typhoon season took place during the neutral phase of the El Niño–Southern Oscillation,{{cite web |title=Past Events |url=https://psl.noaa.gov/enso/past_events.html |author=Physics Science Laboratory |publisher=National Oceanic and Atmospheric Administration |access-date=20 September 2024}} with a weak and short-lived La Niña developing during the summer.{{cite web |author1=Physics Science Laboratory |title=El Nino and La Nina Years: NOAA Physical Sciences Laboratory |url=https://psl.noaa.gov/enso/climaterisks/years/top24enso.html |publisher=National Oceanic and Atmospheric Administration |access-date=14 October 2024}} During a La Niña, a westward shift in the formation of tropical cyclones and the location of the subtropical ridge occurs, which is correlated to an increased chance for systems to make landfall in China and be more intense when striking the Philippines.{{cite journal |author1=M. C. Wu |author2=W. L. Chang |author3=W. M. Leung |year=2003 |title=Impacts of El Nino-Southern Oscillation Events on Tropical Cyclone Landfalling Activity in the Western North Pacific |journal=Journal of Climate |volume=17 |issue=6 |pages=1419–1428 |bibcode=2004JCli...17.1419W |citeseerx=10.1.1.461.2391 |doi=10.1175/1520-0442(2004)017<1419:IOENOE>2.0.CO;2 |issn=0894-8755}} As a result, by named storms, the season is the third-most active on record.{{cite journal |last1=Zhang |first1=Xinchang |last2=Zhong |first2=Shanshan |last3=Wu |first3=Zhiwei |last4=Li |first4=Yun |title=Seasonal prediction of the typhoon genesis frequency over the Western North Pacific with a Poisson regression model |journal=Climate Dynamics |date=December 2018 |volume=51 |issue=11-12 |pages=4589 |doi=10.1007/s00382-017-3654-5 |url=https://aos.fudan.edu.cn/_upload/article/files/de/00/ac0f97ef4cd487f80d097be45bb9/c654bf69-c642-49a9-933f-c2e321b83d1a.pdf}} This was represented with an above-average ACE index of approximately 140.6 units, making it by ACE, the fifteenth-most active as of 2024.{{cite web| title=Real-Time Tropical Cyclone North Atlantic Ocean Statistics|url=http://tropical.atmos.colostate.edu/Realtime/|publisher=Colorado State University|location=Fort Collins, Colorado|access-date=September 29, 2024}} This number represents sum of the squares of the maximum sustained wind speed (knots) for all named storms while they are at least tropical storm intensity, divided by 10,000. Therefore, tropical depressions are not included.{{cite web |title=CSU Hurricane Seasonal Forecasting |url=https://tropical.colostate.edu/forecasting.html |publisher=Colorado State University |access-date=14 October 2024 |location=Fort Collins, Colorado}}

In 1967, the Airborne Early Warning Squadron One (VW-1) flew 4,692.6 hours in the Western Pacific.{{cite web |last1=Roth |first1=F. H. |title=OPNAV Report 5750-1 |url=https://vw1assoc.org/OPNAV_Report_5750-1.html |publisher=Airborne Early Warning Squadron One |access-date=24 October 2024 |date=1968}} Many systems during the season tracked inconsistently, causing there to be significant forecast errors, however many late-season storms were consistent movers and easily

predictable, lessening these errors.{{cite journal |last1=Geraldson |first1=E. Lee |title=A COMPARISON OF THE ACCURACY OF OBJECTIVE TECHNIQUES FOR FORECASTING TYPHOON MOVEMENT DURING 1967 |journal=Monthly Weather Review |date=September 1968 |volume=96 |issue=9 |pages=649–953 |doi=10.1175/1520-0493(1968)096<0649:ACOTAO>2.0.CO;2 |url=https://journals.ametsoc.org/view/journals/mwre/96/9/1520-0493_1968_096_0649_acotao_2_0_co_2.xml |access-date=26 October 2024 |language=EN |issn=1520-0493}}

American astronaut and senator Harrison Schmitt noted that during Apollo 17, the ship may have flown over Violet as a tropical storm.{{cite book |last1=Schmitt |first1=Harrison |title=America's Uncommon Sense |date=7 December 2017 |url=https://www.americasuncommonsense.com/1-apollo-17-diary-of-the-12th-man/b-chapters-1-9/6-chapter-5-30-seconds-and-counting/ |access-date=18 October 2024 |chapter=30 Seconds and Counting}}

File:SarahandWanda1967.png on September 20. Sarah (right) and Wanda (left)]]

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=CMA TD 01 1967 path.png

|Formed=January 12

|Dissipated=January 14

|1-min winds=29

|Pressure=1004

}}

On January 9, the China Meteorological Administration noted that a tropical disturbance had formed east of Leyte.{{cite web|title=1967 Tropical Depression UNNAMED (1967009N07144)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967009N07144|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=12 October 2024|location=Asheville, North Carolina}} As the disturbance tracked westwards, it filled up. However, at 18:00 UTC on January 12, it developed into a tropical depression with a minimum pressure of {{cvt|1004|hPa|inHg}} and sustained winds near {{cvt|25|kn|mph km/h|order=out|round=5}}. Further development occurred, and six hours later, it peaked with sustained winds of {{cvt|29|kn|mph km/h|order=out|round=5}}. However, this trend was short-lived, as on 15:00 UTC on January 13, it began weakening. As a result, it degenerated back into a tropical disturbance at 06:00 UTC the next day, making landfall in Samar, Philippines six hours later. Further weakening, the remnants made their second landfall in Panay, Philippines on 00:00 UTC the next day before dissipating soon after.

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=Ruby Feb 4 1967.png

|Track=Ruby 1967 path.png

|Formed=January 28

|Dissipated=February 6

|1-min winds=40

|Pressure=996

}}

On January 28, a tropical depression formed well east of the Philippines with a minimum pressure of {{cvt|996|hPa|inHg}}.{{cite web|title=1967 Tropical Storm RUBY (1967028N05140)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967028N05140|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=12 October 2024|location=Asheville, North Carolina}} Slowly recurving northwards as the depression's circulation became increasingly disorganized,{{sfn|Mariners Weather Log|1967|p=112}} on February 1, it crossed into the Philippine Area of Responsibility, causing it to be named Auring by the Philippine Atmospheric, Geophysical, and Astronomical Services Administration (PAGASA).{{cite report |url=http://www.typhoon2000.ph/stormstats/1963-1988_PTC.txt |title=PAGASA Tropical Cyclone Names 1963–1988 |last1=Padua |first1=Michael V. |date=November 6, 2008 |publisher=Typhoon 2000 |access-date=June 5, 2017 |format=TXT}} Slow development occurred, and after it underwent a cyclonic loop, it developed into a tropical storm on February 5, simuntaneously peaking with sustained winds of {{Cvt|40|kn|mph km/h|order=out|round=5}} and being named Ruby by the Joint Typhoon Warning Center. However, soon after, it degenerated into a gale-force remnant low two days later, east of Mindanao, Philippines. These remnants tracked towards the Philippines prior to dissipating on February 9.

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{{main|Typhoon Sally (1967)}}

{{Infobox tropical cyclone small

|Basin=WPac

|Image=Sally Mar 2 1967.png

|Track=Sally 1967 path.png

|Formed=February 28

|Dissipated=March 6

|1-min winds=85

|Pressure=980

}}

On February 28, a tropical depression with a minimum pressure of {{cvt|1006|hPa|inHg}} formed northeast of Manus Island in Papua New Guinea.{{cite web|title=1967 Typhoon SALLY (1967059N02145)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967059N02145|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=12 October 2024|location=Asheville, North Carolina}}{{sfn|Annual Typhoon Report|1967|p=84}} Tracking northwestwards during the next few days, development was slow to occur. However, on 12:00 UTC on March 1, the depression intensified into a tropical storm, being named Sally by the Joint Typhoon Warning Center. However, in the span of six hours that same day, Sally undergone rapid intensification, intensifying from a minimal tropical storm into a minimal typhoon with sustained winds of {{cvt|70|kn|mph km/h|order=out|round=5}}. Further intensification occurred, and on 00:00 UTC on March 2, Sally peaked with sustained winds of {{cvt|85|kn|mph km/h|order=out|round=5}} and a minimum pressure of {{cvt|980|hPa|inHg}}. Around that time, as Sally recurved to the west, it crossed into the Philippine Area of Responsibility, causing PAGASA to name it Bebeng. Soon after, Sally weakened into a tropical storm, making landfall just north of Mindanao 06:00 UTC on March 3 with sustained winds of {{cvt|60|kn|mph km/h|order=out|round=5}}. Rapid weakening occurred due to landfall, and as it made its second landfall in Leyte at 06:00 UTC the next day, it weakened into a tropical depression. As it exited the Philippine Area of Responsibility on March 5, it began recurving southwards. As a result, it dissipated the next day, near Borneo.

As Sally peaked in intensity, the island of Koror, which was around {{convert|180|NM|km}} east of the typhoon, suffered the brunt and was lashed by hurricane-force gusts which reached {{cvt|75|kn|mph km/h|order=out|round=5}}. As a result, around 80 percent of the island's buildings were destroyed or damaged.{{cite web |author1=National Climatic Data Center |title=Typhoon Sally, 28 February – 7 March |url=https://webapp1.dlib.indiana.edu/virtual_disk_library/index.cgi/4274123/FID1030/DATA/TROPIC/WNP_NAR/1967_2.NAR |publisher=Indiana University Bloomington |access-date=13 October 2024 |date=11 April 1995}} Additionally, three people died in Palau while another fifty were injured in the nation.{{cite news |last1=Samblan |first1=Niki |last2=Tman |first2=Luke |title=Typhoon Hits Palau |url=https://pacificdigitallibrary.org/cgi-bin/pdl?e=d-000off-pdl--00-2--0--010---4-------0-1l--10en-50---20-text---00-3-1-00bySR-0-0-000utfZz-8-00&a=d&cl=CL2.15&d=HASH4967b6cf10347a48e07393 |access-date=14 October 2024 |agency=Micronesian Reporter |issue=6 |volume=XIV |publisher=Pacific Digital Library |date=March 1967 |pages=10-14}} ([https://alekokau.wordpress.com/2012/12/02/palau-in-history-typhoon-sally-hits-palau/ Alt version]) In total, Sally caused USD$5 million in damage for the island of Palau. In the Philippines, Sally, the first March typhoon since 1948 to make landfall in the nation, caused one death and "considerable damage" to property, with Surigao receiving peak winds of {{cvt|65|kn|mph km/h|order=out|round=5}}.{{cite news |last1=Bueza |first1=Michael |title=How frequent are storms in the Philippines in March? |url=https://www.rappler.com/environment/87097-march-storms-frequency-par/ |access-date=13 October 2024 |work=Rappler |date=17 March 2015}}

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=ThereseMarch171967.jpg

|Track=Therese 1967 path.png

|Formed=March 15

|Dissipated=March 24

|1-min winds=60

|Pressure=992

}}

On March 15, a tropical depression with a minimum pressure of {{cvt|1004|hPa|inHg}} and sustained winds near {{cvt|30|kn|mph km/h|order=out|round=5}} formed near Ulithi.{{cite web|title=1967 Severe Tropical Storm THERESE (1967075N08148)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967075N08148|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=12 October 2024|location=Asheville, North Carolina}} Slowly developing, on 12:00 UTC the next day, the depression intensified into a tropical storm, being named Therese by the Joint Typhoon Warning Center. Further development was slow to occur, with Thelma not intensifying past {{cvt|40|kn|mph km/h|order=out|round=5}} until March 18. Around that time, Therese began recurving north-northwestwards, intensifying at a higher rate. As a result, on 00:00 UTC the next day, Therese peaked with sustained winds of {{cvt|60|kn|mph km/h|order=out|round=5}}, attaining a minimum pressure of {{cvt|992|hPa|inHg}} just six hours later. Around that time, Therese began weakening as it then tracked westwards. However, Therese suddenly re-intensified, having a secondary peak on March 20, with sustained winds of {{cvt|55|kn|mph km/h|order=out|round=5}} and a minimum pressure of {{cvt|992|hPa|inHg}}. This phase ended a few hours later, and as Therese tracked just south of the Marianas Islands, it began weakening. Therese was able to shortly re-intensify twice, however, the storm progressively weakened after that. During these phases, Therese began tracking northwestwards, becoming extratropical on March 24.{{sfn|Climatological Data|1967|p=24}} This cyclone weakened, becoming a high-pressure area east of the International Date Line on March 26 and dissipating.

Therese passed just {{cvt|45|mi|km}} northeast of Ulithi as a minimal tropical storm on March 18, producing heavy rainfall, peaking with 3-hour totals of {{cvt|1|in|cm}} in the atoll.{{sfn|Climatological Data|1967|p=24}} Therese's extratropical remnants passed near Marcus Island (now known as Minamitorishima), producing {{cvt|3.78|in|cm}} of rainfall and a peak gust of {{cvt|35|mph|km/h}} in the island.{{sfn|Climatological Data|1967|p=24}} This rain total helped contribute to the {{cvt|5.23|in|cm}} of rainfall recorded in the island during March, which at the time, was the highest the island recorded in the month.{{sfn|Climatological Data|1967|p=24}}

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=Violet Apr 5 1967.png

|Track=Violet 1967 path.png

|Formed=March 31

|Dissipated=April 12

|1-min winds=120

|Pressure=930

}}

At 18:00 UTC on March 31, due to an interaction between an easterly wave and a polar trough, a tropical depression with a minimum pressure of {{cvt|1000|hPa|inHg}} formed southwest of Truk Island (now known as Chuuk Lagoon).{{cite web|title=1967 Super Typhoon VIOLET (1967091N04151)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967091N04151|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=18 October 2024|location=Asheville, North Carolina}}{{cite web |author1=National Climatic Data Center |title=Typhoon Violet, 31 March – 12 April |url=https://webapp1.dlib.indiana.edu/virtual_disk_library/index.cgi/4274123/FID1030/DATA/TROPIC/WNP_NAR/1967_4.NAR |publisher=Indiana University Bloomington |access-date=13 October 2024 |date=11 April 1995}}{{sfn|Annual Typhoon Report|1967|p=84}} Undergoing rapid intensification during the next day, the system strengthened from a tropical depression with sustained winds of {{cvt|30|kn|mph km/h|order=out|round=5}} into a high-end tropical storm with sustained winds of {{cvt|55|kn|mph km/h|order=out|round=5}}, being named Violet by the Joint Typhoon Warning Center. Further development was slow to occur as the storm tracked northwest, with Violet not intensifying into a typhoon until 18:00 UTC the next day. Slowly developing, at 00:00 UTC on April 4, Violet initially peaked with sustained winds of {{cvt|80|kn|mph km/h|order=out|round=5}}, crossing into the Philippine Area of Responsibility later that day, causing PAGASA to name it Karing. Initially weakening slightly, Violet regained its former strength by the morning of April 5, slowing in its northwestward trajectory. Undergoing a second bout of rapid intensification, in just six hours, Violet strengthened from having sustained winds of {{cvt|90|kn|mph km/h|order=out|round=5}} to having peak sustained winds of {{cvt|120|kn|mph km/h|order=out|round=5}} and a minimum pressure of {{cvt|940|hPa|inHg}}. Weakening as it tracked northwestwards at a faster rate, at 03:00 UTC on April 8, Violet made landfall in northern Luzon with sustained winds of {{cvt|110|kn|mph km/h|order=out|round=5}} and a minimum pressure of {{cvt|946|hPa|inHg}}. Rapidly weakening due to landfall, as it exited Luzon on 18:00 UTC that same day, it became a tropical storm. Further weakening occurred as Violet recurved westward on April 10, and as it brushed southern Taiwan on April 11, it weakened into a tropical depression. This depression recurved northwards before being absorbed by a mid-latitude trough near the Ryukyu Islands on April 12.{{sfn|Climatological Data|1967|p=24}}

As Violet slowly intensified, on April 2 and 3, Woleai reported peak winds of {{cvt|35|mph|km/h}} while Ulithi reported peak winds of {{cvt|36|mph|km/h}}.{{sfn|Climatological Data|1967|p=36}} However, Yap saw a daily total {{cvt|6|in|cm}} of rain from Violet, reporting peak gusts of {{cvt|32|mph|km/h}}.{{sfn|Climatological Data|1967|p=36}} In the Philippines, where Violet made landfall, 4 people died in Luzon alone. The SS Silver Peak, a Panamanian vessel, was run aground by Violet near Minamitorishima, causing the 31st Marine Expeditionary Unit and the USS Seminole to rescue the 28 crewmen of the ship.{{cite web |title=31st MEU History |url=https://www.31stmeu.marines.mil/About/History.aspx |publisher=31st Marine Expeditionary Unit |access-date=18 October 2024}}{{cite book |last1=Mooney |first1=James L. |title=Dictionary of American Naval Fighting Ships |date=1 January 1976 |volume=VI |publisher=United States Naval History Division |page=438 |url=https://www.google.com/books/edition/Dictionary_of_American_Naval_Fighting_Sh/mxQzAAAAMAAJ |language=en}} A weakening Violet prompted the Hong Kong Observatory (HKO) to hoist Standby Signal No. 1, making it the earliest issued typhoon warning until Typhoon Maysak caused the Observatory to hoist the same signal on April 3, 2015.{{cite news |last1=Ying-kit |first1=Lai |title=Typhoon Maysak set to trigger earliest Hong Kong storm signal since records began |url=https://www.scmp.com/news/hong-kong/article/1755158/typhoon-maysak-could-see-earliest-hong-kong-storm-signal-hoisted |access-date=18 October 2024 |publisher=South China Morning Post |date=3 April 2015 |language=en}}

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=Wilda May 9 1967.png

|Track=Wilda 1967 path.png

|Formed=May 8

|Dissipated=May 13

|1-min winds=40

|Pressure=1004

}}

On May 8, a tropical depression with a minimum pressure of {{cvt|1006|hPa|inHg}} formed southwest of Yap.{{cite web|title=1967 Tropical Storm WILDA (1967128N06137)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967128N06137|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=20 October 2024|location=Asheville, North Carolina}}{{sfn|Mariners Weather Log|1967|p=214}} Recurving northwestwards, further development of the depression was slow to occur. The next day, the depression crossed into the Philippine Area of Responsibility, being named Diding by PAGASA. However, on 12:00 UTC on May 10, the depression suddenly intensified and simultaneously peaked with sustained winds of {{cvt|40|kn|mph km/h|order=out|round=5}}, causing the JTWC to name it Wilda. Tracking westward, Wilda began weakening, becoming a tropical depression 18 hours later. Further weakening occurred as Wilda tracked southwards, and at 06:00 UTC on May 13, the depression dissipated.{{sfn|Mariners Weather Log|1967|p=214}}

Wilda produced {{cvt|11.88|in|mm}} of rainfall in Yap, becoming the fifth-wettest cyclone to impact the island.{{Tropical Cyclone Point Maxima}}

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=CMA TD 07 1967 path.png

|Formed=June 6

|Dissipated=June 8

|1-min winds=29

|Pressure=1002

|WarningCenter=CMA

}}

On June 2, the China Meteorological Administration noted that a tropical disturbance had formed near Chuuk Lagoon.{{cite web|title=1967 Tropical Depression UNNAMED (1967154N07154)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967154N07154|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=20 October 2024|location=Asheville, North Carolina}} Tracking westnorthwestwards throughout the next few days, the disturbance did not deepen much. However, at 12:00 UTC on June 5, the disturbance suddenly deepened, attaining a minimum pressure of {{cvt|1002|hPa|inHg}} prior to filling rapidly. Assuming a more northwestward track, the disturbance passed between Yap and the Northern Marianas that same day. Further development occurred, and 24 hours later, the disturbance developed into a tropical depression with sustained winds of {{cvt|29|kn|mph km/h|order=out|round=5}}, later attaining a minimum pressure of {{cvt|1002|hPa|inHg}} 12 hours later. Never intensifying further, on June 8, the depression degenerated back into a tropical disturbance, dissipating later that day.

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=Etang21June1967.jpg

|Track=Etang 1967 path.png

|Formed=June 20

|Dissipated=June 23

|Type=TD

|Pressure=1004

|WarningCenter=SSHWS

|

}}

At 06:00 UTC on June 20, a tropical depression with a minimum pressure of {{cvt|1006|hPa|inHg}} formed well east of the Philippines.{{cite web |title=Asia Pacific Surface Analysis |url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/show.pl?type=as&id=19670620_1&lang=en |website=Digital Typhoon |publisher=National Institute of Informatics |access-date=21 October 2024 |date=20 June 1967}} Despite opening into a trough later that same day as it tracked westward,{{cite web |title=Asia Pacific Surface Analysis |url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/show.pl?type=as&id=19670620_2&lang=en |website=Digital Typhoon |publisher=National Institute of Informatics |access-date=21 October 2024 |date=20 June 1967}} it regenerated on June 21, attaining a minimum pressure of {{cvt|1004|hPa|inHg}}.{{cite web |title=Asia Pacific Surface Analysis |url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/show.pl?type=as&id=19670621_2&lang=en |website=Digital Typhoon |publisher=National Institute of Informatics |access-date=21 October 2024 |date=21 June 1967}} However, as it recurved northwestwards, it degenerated back into a trough on June 22.{{cite web |title=Asia Pacific Surface Analysis |url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/show.pl?type=as&id=19670622_1&lang=en |website=Digital Typhoon |publisher=National Institute of Informatics |access-date=21 October 2024 |date=22 June 1967}} Around that time, the depression crossed into the Philippine Area of Responsibility, being named Etang by PAGASA. Further weakening occurred, and as it filled up in Luzon early the next day,{{cite web |title=Asia Pacific Surface Analysis |url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/show.pl?type=as&id=19670623_1&lang=en |website=Digital Typhoon |publisher=National Institute of Informatics |access-date=21 October 2024 |date=23 June 1967}} PAGASA stopped monitoring the depression as it dissipated soon after.{{cite web |title=Asia Pacific Surface Analysis |url=http://agora.ex.nii.ac.jp/cgi-bin/weather-chart/show.pl?type=as&id=19670623_2&lang=en |website=Digital Typhoon |publisher=National Institute of Informatics |access-date=21 October 2024 |date=23 June 1967}}

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=AnitaJun271967ESSA5.jpg

|Track=Anita 1967 path.png

|Formed=June 24

|Dissipated=July 1

|1-min winds=80

|Pressure=975

}}

On June 24, a tropical depression with a minimum pressure of {{Cvt|1008|hPa|inHg}} formed well east of the Philippines.{{cite web|title=1967 Typhoon ANITA (1967175N10142)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967175N10142|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=22 October 2024|location=Asheville, North Carolina}} Slowly deepening throughout the next few days as it tracked west-northwestward, on June 26, it crossed into the Philippine Area of Responsibility, being named Gening by PAGASA. Further development occurred, and on 12:00 UTC that same day, the depression intensified into a tropical storm, being named Anita by the Joint Typhoon Warning Center. As this occurred, Anita intensified at a faster rate and tracked northwestwards, becoming a typhoon at 00:00 UTC on June 28. Further intensification occurred, and later that day, as Anita passed through the Babuyan Channel (now known as the Luzon Strait),{{sfn|Mariners Weather Log|1967|p=187}} it brushed the coast of northern Luzon with sustained winds of {{cvt|70|kn|mph km/h|order=out|round=5}}. Shortly after, at 06:00 uTC on June 29, Anita peaked with sustained winds of {{cvt|80|kn|mph km/h|order=out|round=5}} and a minimum pressure of {{cvt|975|hPa|inHg}}, exiting the Philippine Area of Responsibility later that day. However, as it approached the southern coast of China, it weakened, making landfall just south of Shan–T'ou (now known as Shantou) on 06:00 UTC the next day as a weakening tropical storm.{{sfn|Mariners Weather Log|1967|p=187}} Rapidly weakening as it tracked inland,{{sfn|Mariners Weather Log|1967|p=187}} just six hours later, it became a tropical depression, later dissipating early on July 1.

As Anita approached Hong Kong, officials issued typhoon warnings for coastal areas near the nation.{{cite news |title=Typhoon Alert On |url=https://books.google.com/books?id=8zdWAAAAIBAJ |access-date=23 October 2024 |agency=Thomson Reuters |issue=47 |volume=85 |publisher=The Spokesman-Review |date=30 June 1967 |page=13 |language=en}} In the Philippines, at least twenty people died due in Ilocos Norte.{{cite news |title=Typhoon kills 20 people |url=https://eresources.nlb.gov.sg/newspapers/digitised/article/straitstimes19670704-1.2.16.3 |access-date=21 October 2024 |agency=United Press International |publisher=The Straits Times |date=4 July 1967 |page=2}} Heavy rainfall from Anita produced mudslides that collapsed a gold and copper mine in Baguio, trapping forty-three miners.{{cite news |title=Dirty Undershirt Satisfies Hunger |url=https://books.google.com/books?id=rVdYAAAAIBAJ |access-date=23 October 2024 |agency=United Press International |issue=247 |publisher=Spokane Daily Chronicle |date=5 July 1967 |location=Spokane, Washington |page=2 |language=en}}{{cite news |title=Hope Fades for Trapped 41 Miners |url=https://books.google.com/books?id=8zdWAAAAIBAJ |access-date=23 October 2024 |agency=Associated Press |issue=47 |volume=85 |publisher=The Spokesman-Review |date=30 June 1967 |page=13 |language=en}} Of those miners, twenty-seven survived, eight went missing, and eight died. These mudslides affected the town of Dingras, where two families were buried alive due to the mud. Heavy rainfall produced by Anita caused a Thai Airways International jetliner to crash into Kowloon Bay, killing 24 people.{{cite news |title=15 Americans Among Dead In Jet Crash |url=https://books.google.com/books?id=ytMbAAAAIBAJ |access-date=21 October 2024 |issue=9 |volume=84 |publisher=The Pittsburgh Press |date=1 July 1967 |page=2 |language=en}}

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{{Infobox tropical cyclone small

|Basin=WPac

|Image=CMA TD 07 1967 path.png

|Formed=June 26

|Dissipated=June 26

|1-min winds=29

|Pressure=1001

|WarningCenter=CMA

}}

On June 24, the China Meteorological Administration noted that a tropical disturbance had formed in the South China Sea, just east of Vietnam.{{cite web|title=1967 Tropical Depression UNNAMED (1967176N13111)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967176N13111|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=25 October 2024|location=Asheville, North Carolina}} As the weak disturbance deepened slowly, it began tracking northeast then northwest the next day. Retaining its intensity, later that day, it passed through the Paracel Islands, tracking northwards soon after. However, as it recurved northeastwards on June 26, the disturbance suddenly developed into a tropical depression. Further intensification occurred, and on 06:00 UTC that same day, it peaked with sustained winds of {{cvt|29|kn|mph km/h|order=out|round=5}} and a minimum pressure of {{cvt|1001|hPa|inHg}}. However, rapid weakening occurred, and just six hours later, the depression degenerated into a tropical disturbance, dissipating soon after.

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{{main|1967 Southern Japan floods}}

{{Infobox tropical cyclone small

|Basin=WPac

|Image=Sat196707060456zBillie.png

|Track=Billie 1967 path.png

|Formed=June 29

|Dissipated=July 8

|1-min winds=70

|Pressure=980

}}

On June 29, a tropical depression with a minimum pressure of {{Cvt|1006|hPa|inHg}} formed well southwest of the Mariana Islands.{{cite web|title=1967 Typhoon BILLIE (1967181N09148)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967181N09148|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=26 October 2024|location=Asheville, North Carolina}} Slowly deepening during the next three days as it tracked northwestward, on July 2, it intensified into a tropical storm, being named Billie by the Joint Typhoon Warning Center. The next day, it crossed into the Philippine Area of Responsibility, being named Herming by PAGASA. Around that time, the 54th Weather Reconnaissance Squadron investigated Billie, revealing that the system was loosely organized, with most convective activity persisting in its southwest quadrant.{{cite journal |last1=Fett |first1=Robert W. |title=SOME UNUSUAL ASPECTS CONCERNING THE DEVELOPMENT AND STRUCTURE OF TYPHOON BILLIE—JULY 1967 |journal=Monthly Weather Review |date=September 1968 |volume=96 |issue=9 |pages=637–648 |doi=10.1175/1520-0493(1968)096<0637:SUACTD>2.0.CO;2 |url=https://journals.ametsoc.org/view/journals/mwre/96/9/1520-0493_1968_096_0637_suactd_2_0_co_2.xml |access-date=24 October 2024}} Embedded in a major trough axis, Billie recurved westward the next day. Rapid intensification ensued, with Billie intensifying {{cvt|30|kn|mph km/h|order=out|round=5}} during that time, becoming a typhoon and peaking with sustained winds of {{cvt|70|kn|mph km/h|order=out|round=5}} and a minimum pressure of {{cvt|980|hPa|inHg}}. Despite exhibiting a mesoscale warm core, Billie never was able to develop an eyewall which encircled its eye, preventing the typhoon from intensifying further. This caused Billie to undergo several cycles of weakening and restrengthening from July 5–6 as it recurved northwestwards. However, soon after, Billie weakened into a tropical storm, exiting the Philippine Area of Responsibility on July 7 prior to weakening into a tropical depression on 18:00 UTC the next day. This depression helped enhance a front prior to becoming an extratropical low the next day.{{cite web |title=昭和４２年７月豪雨　昭和42年（1967年）　７月８日～７月９日 |url=https://www.data.jma.go.jp/obd/stats/data/bosai/report/1967/19670708/19670708.html |publisher=Japan Meteorological Agency |access-date=26 October 2024 |language=ja}} This low passed through Japan, exiting on July 9, and tracked westward prior to dissipating near the International Date Line on July 12.

The front that Billie and another tropical depression enhanced caused devastating flooding throughout Southern Japan. These rains, which were concentrated in Kyushu and southwestern Honshu, produced nearly two thousand landslides.{{sfn|Mariners Weather Log|1967|p=188}} More than a thousand homes were destroyed or damaged, almost seven hundred of which were washed away.{{sfn|Mariners Weather Log|1967|p=188}} 277 bridges were swept away by landslides and floods.{{sfn|Mariners Weather Log|1967|p=188}} In total, this flooding, dubbed by the [{Japan Meteorological Center]] as the "Heavy Rains of July 1967", killed 351 people, made another eighteen go missing, and injured a further 618 people.

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{{main|Typhoon Clara (1967)}}

{{Infobox tropical cyclone small

|Basin=WPac

|Image=Clara Jul 10 1967.png

|Track=Clara 1967 path.png

|Formed=July 2

|Dissipated=July 12

|1-min winds=100

|Pressure=960

}}

On July 2, a tropical depression with a minimum pressure of {{Cvt|1008|hPa|inHg}} formed well east of the Mariana Islands.{{cite web|title=1967 Typhoon CLARA (1967183N20155)|url=https://ncics.org/ibtracs/index.php?name=v04r01-1967183N20155|website=IBTrACS|publisher=University of North Carolina at Asheville|access-date=27 October 2024|location=Asheville, North Carolina}} As it recurved northwestwards on July 4, the system exhibited characteristics of a cold-core low according to the Joint Typhoon Warning Center.{{sfn|Annual Typhoon Report|1967|p=106}} However, as it recurved southwestwards on July 6, the low soon developed divergence and attained tropical characteristics, causing it to be named Clara by the Joint Typhoon Warning Center.{{sfn|Annual Typhoon Report|1967|p=106}} As a result, Clara underwent rapid intensification, intensifying from having maximum winds of {{cvt|30|kn|mph km/h|order=out}} to a typhoon with sustained winds of {{cvt|65|kn|mph km/h|order=out}}, becoming the first tropical cyclone in the season to form north of 15°N.{{sfn|Mariners Weather Log|1967|p=188}} Tracking into the Philippine Area of Responsibility the next day, the system was named Ising by PAGASA. Soon after, Clara recurved northwestwards, finishing that recurvature on July 9.

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{{See also|Tropical cyclone naming|History of tropical cyclone naming}}

The following list of names was used in 1967 by the Joint Typhoon Warning Center to name tropical cyclones which formed in the Northwestern Pacific Ocean and produced sustained winds of at least {{cvt|35|kn|mph km/h|order=out|round=5}}.{{sfn|Mariners Weather Log|1967|p=90}}

{{notelist}}

• {{cite book |title=Climatological Data: Pacific |date=1967 |volume=12 |publisher=U.S. Department of Commerce, Weather Bureau |url=https://books.google.com/books?id=PZyEQsZIYvsC |ref={{harvid|Climatological Data|1967}}|language=en}}
• {{cite book |title=Mariners Weather Log |date=1967 |publisher=Environmental Data and Information Service |url=https://books.google.com/books?id=NyYKXUs0YvgC |access-date=20 October 2024 |ref={{harvid|Mariners Weather Log|1967}} |language=en}}
• {{Cite report |url=https://www.metoc.navy.mil/jtwc/products/atcr/1967atcr.pdf |title=Annual Typhoon Report 1967 |date=3 January 1968 |publisher=Joint Typhoon Warning Center |location=Guam, Mariana Islands |page=44-48 |access-date=October 26, 2024 |last1=Negele |first1=J. H. |last2=Roper |first2=William D. |last3=Geraldson |first3=E. Lee |last4=Haraguchi |first4=Paul Y. |last5=Langemo |first5=James C. |last6=Newman |first6=William R. |last7=Depew |first7=John H. |last8=Halsteter |first8=Joseph |last9=Martin |first9=Donald G. |last10=Andreasen |first10=Glen R. |last11=McGuire |first11=Kenneth J. |last12=Summer |first12=David B. |last13=Buquing |first13=Alvina L. |ref={{harvid|Annual Typhoon Report|1967}} |language=en}}

{{reflist}}