2013 Pacific hurricane season#Tropical Storm Unala

On May 21, the Central Pacific Hurricane Center (CPHC) released its forecast for tropical activity across the Central Pacific during 2013. In its report, the organization predicted a 70 percent chance of a below-average season, a 25 percent chance of a near-average season, and a 5 percent chance of an above-average season, equating to 1–3 tropical cyclones across the basin. An average season yields 4–5 tropical cyclones. This forecast was based primarily on the expectation of Neutral El Niño–Southern Oscillation conditions and a continuation of the positive Atlantic multidecadal oscillation.{{cite web|title=NOAA expects below-normal Central Pacific hurricane season|url=http://www.noaanews.noaa.gov/stories2013/20130521_hurricaneoutlook_centralpacific.html|publisher=National Oceanic and Atmospheric Administration|work=Central Pacific Hurricane Center|date=May 21, 2013|access-date=January 19, 2015}}

Two days later, the Climate Prediction Center (CPC) issued its forecast for tropical activity across the East Pacific during 2013. With near or below average sea surface temperatures in the eastern equatorial Pacific and a continuation of the climate pattern responsible for the ongoing era of low Pacific hurricane activity that began in 1995, the organization called for a 55 percent chance of a below-average season, a 35 percent chance of a near-average season, and a 10 percent chance of an above-average season. In total, the CPC predicted 11–16 named storms, 5–8 hurricanes, and 1–4 major hurricanes; an average season yields 15.4 named storms, 8.4 hurricanes, and 3.9 major hurricanes. Both the CPHC and CPC stressed the importance of being prepared prior to the start of the season, noting that significant tropical cyclones can occur even in below-average seasons.{{cite web|title=NOAA predicts below-normal Eastern Pacific hurricane season|url=http://www.noaanews.noaa.gov/stories2013/20130523_hurricaneoutlook_easternpacific.html|publisher=National Oceanic and Atmospheric Administration|work=Climate Prediction Center|date=May 23, 2013|access-date=January 19, 2015}}

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{{List of costliest Pacific hurricane seasons|align=right}}

{{Least ACE Pacific hurricane seasons}}

The Accumulated Cyclone Energy (ACE) index for the 2013 Pacific hurricane season (Eastern Pacific and Central Pacific combined) as calculated by Colorado State University using data from the National Hurricane Center was 74.8 units.{{#tag:ref|The total represents the sum of the squares of the maximum sustained wind speed (knots) for every (sub)tropical storm's intensity of over {{convert|33|kn|mph km/h}}, divided by 10,000 while they are above that threshold; therefore, tropical depressions are not included.|group="nb"}}{{cite web| title=Basin Archives: Northeast Pacific Ocean Historical Tropical Cyclone Statistics|url=http://tropical.atmos.colostate.edu/Realtime/index.php?arch&loc=northeastpacific|publisher=Colorado State University|location=Fort Collins, Colorado|access-date=July 8, 2022}} 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}}.

The season's first tropical storm formed on May 15,{{cite report|url=http://www.nhc.noaa.gov/archive/2013/ep01/ep012013.discus.002.shtml|title=Tropical Storm Alvin Discussion Number 2|author=Robbie J. Berg|date=May 15, 2013|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|access-date=May 15, 2013}} coinciding with the official start of the Pacific hurricane season.{{cite web|title=Tropical Cyclone Climatology|url=http://www.nhc.noaa.gov/climo/|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|access-date=May 23, 2013|author=National Hurricane Center|date=May 2, 2013}} On average, a tropical cyclone develops in May in the eastern Pacific every other year.{{cite report|url=http://www.nhc.noaa.gov/archive/2011/tws/MIATWSEP_may.shtml?t|title=Monthly Tropical Weather Summary|author=Hurricane Specialist Unit|date=June 1, 2011|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|access-date=May 23, 2013}} The formation of Barbara in late May marked only the fifth time since 1949 that two tropical storms formed during the month, with the other seasons being 1956, 1984, 2007, 2012, and 2021.{{cite web|author=Hurricane Specialist Unit|title=Monthly Tropical Weather Summary|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=June 1, 2013|access-date=June 30, 2013|url=http://www.nhc.noaa.gov/archive/text/TWSEP/2013/TWSEP.201306011144.txt|format=TXT}}{{cite report|author=Hurricane Specialist Unit|title=Monthly Tropical Weather Summary|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=June 1, 2012|access-date=June 30, 2013|url=http://www.nhc.noaa.gov/archive/text/TWSEP/2012/TWSEP.201206011445.txt|format=TXT}}{{cite report|author=Hurricane Specialist Unit|title=Monthly Tropical Weather Summary|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=June 1, 2007|access-date=June 30, 2013|url=http://www.nhc.noaa.gov/archive/2007/tws/MIATWSEP_may.shtml?|format=TXT}}

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{{Infobox hurricane small

| Basin = EPac

| Image = Tropical Storm Alvin 2013-05-15 2052Z.jpg

| Track = Alvin 2013 track.png

| Formed = May 15

| Dissipated = May 17

| 1-min winds = 50

| Pressure = 1000

}}

A tropical wave was first observed over the southeastern Caribbean Sea on May 4. The wave entered the East Pacific a few days later, where atmospheric conditions allowed for gradual development. Curved bands of convection developed around a defined center early on May 15, leading to the formation of a tropical depression around 06:00 UTC that day; at 7.8°N, the depression tied 1976's Hurricane Annette as the second-lowest-latitude tropical cyclone to form in the East Pacific. Twelve hours later, the depression intensified into Tropical Storm Alvin. Influenced by a subtropical ridge over central Mexico, Alvin steadily strengthened and reached peak winds of {{convert|60|mph|km/h|abbr=on|round=5}} early on May 16. Thereafter, increasing wind shear and the introduction of mid-level dry air caused the cyclone to begin a quick weakening trend. The low-level circulation became increasingly elongated and opened up into a trough at 00:00 UTC on May 17. Six hours later, Alvin dissipated while located about {{convert|775|mi|km|abbr=on}} southwest of Manzanillo, Mexico.{{cite report|author=Stacy R. Stewart|title=Tropical Cyclone Report: Tropical Storm Alvin|url={{NHC TCR url|id=EP012013_Alvin}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=May 31, 2013|access-date=January 10, 2015|location=Miami, Florida|format=PDF}}

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{{Infobox hurricane small

| Basin = EPac

| Image = Barbara May 29 2013 1930Z.jpg

| Track = Barbara 2013 track.png

| Formed = May 28

| Dissipated = May 30

| 1-min winds = 70

| Pressure = 983

}}

{{main|Hurricane Barbara (2013)}}

A tropical wave emerged off the western coast of Africa on May 16, entering the East Pacific on May 24. Following the passage of an atmospheric kelvin wave, a broad area of low pressure formed and gradually organized as convection simultaneously increased. At 12:00 UTC on May 28, the wave was declared a tropical depression; six hours later, the depression intensified into Tropical Storm Barbara. Steered northeastward amid favorable atmospheric conditions, a period of rapid deepening ensued, and the system was upgraded to a Category 1 hurricane at 18:00 UTC on May 29. At 19:50 UTC that day, Barbara attained peak winds of {{convert|80|mph|km/h|abbr=on|round=5}} as it moved ashore west-southwest of Tonalá, Chiapas. The cyclone quickly weakened thereafter as it passed over the Sierra Madre mountain range. At 00:00 UTC on May 30, Barbara weakened to a tropical storm, and by six hours later, it further weakened to a tropical depression. After losing its deep convection, the depression degenerated into a remnant low at 12:00 UTC, while located over the Bay of Campeche. The remnant low opened into a trough at 00:00 UTC on May 31.{{cite report|author=Daniel P. Brown|title=Tropical Cyclone Report: Hurricane Barbara|url={{NHC TCR url|id=EP022013_Barbara}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=August 19, 2013|access-date=January 10, 2015|location=Miami, Florida|format=PDF}}

The precursor disturbance brought rainfall to El Salvador,{{cite news|title=Lluvias persisten en el país por sistema de baja presión |url=http://www.elsalvador.com/mwedh/nota/nota_completa.asp?idCat=47673&idArt=7920578 |access-date=May 29, 2013 |newspaper=El Salvador.com |date=May 27, 2013 |author=Liseth Alues |language=es |url-status=dead |archive-url=https://web.archive.org/web/20150610201824/http://www.elsalvador.com/mwedh/nota/nota_completa.asp?idCat=47673&idArt=7920578 |archive-date=June 10, 2015 }} where one person was killed.{{cite news|title=Dejan lluvias en el Salvador un muerto y varias viviendas afectadas |url=http://www.prensalibre.com/noticias/comunitario/Conred-declara-amarilla-depresion-tropical_0_927507485.html |access-date=May 29, 2013 |newspaper=Rotavio |date=May 27, 2013 |language=es |url-status=dead |archive-url=https://web.archive.org/web/20141215213109/http://www.prensalibre.com/noticias/comunitario/Conred-declara-amarilla-depresion-tropical_0_927507485.html |archive-date=December 15, 2014 }} In Mexico, rainfall peaked at {{convert|470|mm|in|abbr=on}}.{{cite web|author=Georgina Saldierna|publisher=La Jordana|date=June 22, 2013|access-date=June 24, 2013|title=Pérdidas por $250 mil millones por sequías e inundaciones en la última década: Peña Nieto|url=http://www.jornada.unam.mx/ultimas/2013/06/22/103952761-perdidas-por-250-mil-millones-por-sequias-e-inundaciones-en-la-ultima-decada-pena-nieto|language=es|archive-url=https://web.archive.org/web/20130624024845/http://www.jornada.unam.mx/ultimas/2013/06/22/103952761-perdidas-por-250-mil-millones-por-sequias-e-inundaciones-en-la-ultima-decada-pena-nieto|archive-date=2013-06-24|url-status=dead}} Even though Hurricane Barbara struck a largely undeveloped stretch of coastal lagoons, containing small fishing villages,{{cite news|title=Hurricane Barbara landfall in Mexico 2nd earliest|url=https://news.yahoo.com/hurricane-barbara-landfall-mexico-2nd-earliest-222921946.html|access-date=May 30, 2013|newspaper=Yahoo! News|date=May 29, 2013|agency=Associated Press}} two elderly people were killed in Oaxaca.{{cn|date=May 2023}} Furthermore, 14 fishermen were left missing off the coast of Tapanatepec;{{cite news|title=Hurricane Barbara slams into Mexico's Pacific Coast; two dead|url=http://www.latimes.com/news/world/worldnow/la-fg-wn-hurricane-barbara-mexico-pacific-coast-20130529,0,5226239.story|access-date=May 30, 2013|newspaper=Los Angeles Times|date=May 29, 2013}}{{cite news|title=Hurricane Barbara floods Mexico's southern Pacific coast, kills two|url=http://worldnews.nbcnews.com/_news/2013/05/30/18600922-hurricane-barbara-floods-mexicos-southern-pacific-coast-kills-two?lite|access-date=May 30, 2013|date=May 29, 2013|author=Jose Cortes|agency=Ruters}} eight of which were found alive.{{cite news|title=Declaran emergencia al sur de México por daños de huracán Bárbara|url=http://www.eluniverso.com/noticias/2013/05/31/nota/973481/declaran-emergencia-sur-mexico-danos-huracan-barbara|access-date=June 2, 2013|newspaper=El Universo|date=May 31, 2013}} The towns of Tonala and Arriaga were the worst affected by the hurricane.{{cite news|title=Tonalá y Arriaga, los más afectados por Bárbara|url=http://www.eluniversal.com.mx/notas/926371.html|access-date=May 30, 2013|newspaper=El Universal|date=May 30, 2013|language=es}} Although damage was minor,{{cite news|title=Daños menores en Chiapas tras paso de 'Bárbara'|url=http://www.eluniversal.com.mx/notas/926481.html|access-date=May 30, 2013|newspaper=El Universal|date=May 30, 2013|language=es}} 50 people were evacuated and 2,000 homes were damaged.{{cite news|title=Hallan a salvo a pescadores dados por perdidos en Oaxaca|url=http://www.eluniversal.com.mx/notas/926483.html|access-date=May 30, 2013|newspaper=El Universal|date=May 30, 2013|author=Lopez Morals|language=es}} Throughout the region, 57,000 people were homeless and 10,000 hectares of crops were destroyed.{{cite news|title=Bárbara dejó más de 57 mil damnificados|url=http://www.eluniversal.com.mx/notas/927804.html|access-date=June 6, 2013|newspaper=El Universal|date=June 5, 2013|language=es}} Total losses were estimated at 1.89 billion pesos (US$148 million).{{cite report |url=https://www1.cenapred.unam.mx/es/Publicaciones/archivos/324-NO.15-IMPACTOSOCIOECONMICODELOSPRINCIPALESDESASTRESOCURRIDOSENMXICOENELAO2013.PDF |title=Impacto Socioeconómico de los Principales Desastres Ocurridos en México en 2013 |trans-title=Socioeconomic Impact of Major Disasters in Mexico in 2013 |year=2021 |publisher=CENAPRED |language=es |access-date=June 16, 2022 |archive-url=https://web.archive.org/web/20220616091844/https://www1.cenapred.unam.mx/es/Publicaciones/archivos/324-NO.15-IMPACTOSOCIOECONMICODELOSPRINCIPALESDESASTRESOCURRIDOSENMXICOENELAO2013.PDF |archive-date=June 16, 2022 |url-status=live}}

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{{Main|Hurricane Cosme (2013)}}

{{Infobox hurricane small

| Basin = EPac

| Image = Cosme Jun 25 2013 2050Z.jpg

| Track = Cosme 2013 track.png

| Formed = June 23

| Dissipated = June 27

| 1-min winds = 75

| Pressure = 980

}}

A tropical wave, the same responsible for Tropical Storm Barry in the Atlantic, moved across the eastern Pacific in late June, yielding a broad area of low pressure by June 21. Northwesterly shear initially hindered development of the system, but a subsequent decrease in upper-level winds, as well as the passage of an eastward-moving kelvin wave, led to the formation of a tropical depression by 12:00 UTC on June 23; twelve hours later, the depression intensified into Tropical Storm Cosme. Steered northwest and eventually west-northwest, the cyclone intensified amid favorable atmospheric dynamics, becoming a minimal hurricane by 12:00 UTC on June 25 and attaining peak winds of {{convert|85|mph|km/h|abbr=on|round=5}} twelve hours later. A track over cooler waters and into an increasingly stable environment caused Cosme to weaken to a tropical storm by 18:00 UTC on June 26 and further degenerate into a remnant low by 12:00 UTC the next day while located about {{convert|690|mi|km|abbr=on}} west-southwest of Cabo San Lucas, Mexico. The remnant low tracked westward prior to dissipating well east-southeast of the Hawaiian Islands on July 1.{{cite report|author=Eric S. Blake|title=Tropical Cyclone Report: Hurricane Cosme|url={{NHC TCR url|id=EP032013_Cosme}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=September 10, 2013|access-date=January 21, 2015|location=Miami, Florida|format=PDF}}

Due to the storm's large size,{{cite news|title=Prevén lluvias en 5 estados por tormenta Cosme|url=http://www.eluniversal.com.mx/notas/931678.html|access-date=June 24, 2013|newspaper=El Universal|date=June 24, 2013|language=es|archive-date=October 21, 2013|archive-url=https://web.archive.org/web/20131021104234/http://www.eluniversal.com.mx/notas/931678.html|url-status=dead}} a "green" alert (low risk) was issued for the states of Colima, Jalisco and Michoacán while a "blue" alert (minimum risk) was placed into effect for the states of Nayarit, Guerrero,{{cite news|title=Cosme se fortalece y se aleja de costas mexicanas|url=http://www.eluniversal.com.mx/notas/931902.html|access-date=July 25, 2013|newspaper=El Universal|date=July 25, 2013|language=es|archive-date=October 21, 2013|archive-url=https://web.archive.org/web/20131021104232/http://www.eluniversal.com.mx/notas/931902.html|url-status=dead}} and Baja California Sur.{{cite news|url=http://www.eluniversal.com.mx/notas/932157.html|title=BCS decreta alerta azul por huracán Cosme|access-date=June 26, 2013|newspaper=El Universal|date=June 25, 2013|language=es}} As the system passed through the Revillagigedo Islands, winds reached {{convert|42|mph|km/h|abbr=on}} on Socorro Island.{{cite news|title=Ya como huracán, "Cosme" se aleja de México|url=http://www.oem.com.mx/laprensa/notas/n3030872.htm|access-date=June 26, 2013|newspaper=La Prensa|date=June 25, 2013|agency=Organización Editorial Mexicana|language=es|archive-url=https://web.archive.org/web/20131021105456/http://www.oem.com.mx/laprensa/notas/n3030872.htm|archive-date=October 21, 2013|url-status=dead}} The outer rainbands brought moderate rains to Guerrero, causing minor flooding in Acapulco. Across the state, the storm generated 24 landslides,{{cite news|title=Deja dos muertos huracán "Cosme" en Guerrero |url=http://www.xeu.com.mx/nota.cfm?id=529018 |access-date=June 26, 2013 |newspaper=Xeu |date=June 25, 2013 |language=es |url-status=dead |archive-url=https://web.archive.org/web/20131105040322/http://www.xeu.com.mx/nota.cfm?id=529018 |archive-date=November 5, 2013 }} which blocked highways.{{cite news|title=Guerrero alerta por lluvias generadas por Cosme|url=http://www.eluniversal.com.mx/notas/931743.html|access-date=June 24, 2013|newspaper=El Universal|date=June 24, 2013|language=es|archive-date=June 28, 2013|archive-url=https://web.archive.org/web/20130628035447/http://www.eluniversal.com.mx/notas/931743.html|url-status=dead}} Two people were killed in the Guerrero, one a tourist that drowned in Zihuatanejo{{cite news|title=Huracán Cosme deja dos muertos en Guerrero|url=http://www.eluniversal.com.mx/notas/932042.html|access-date=June 25, 2013|newspaper=El Universal|date=June 25, 2013|language=es|archive-date=October 21, 2013|archive-url=https://web.archive.org/web/20131021104239/http://www.eluniversal.com.mx/notas/932042.html|url-status=dead}} and the other a police officer in an airplane crash that injured 19 others.{{cite news|title=Huracán Cosme provoca muerte de policía en Guerrero|url=http://rednoticiero.com/huracan-cosme-provoca-muerte-de-policia-en-guerrero/|access-date=June 26, 2013|newspaper=Red Noticier|date=June 26, 2013|language=es|archive-date=October 21, 2013|archive-url=https://web.archive.org/web/20131021133526/http://rednoticiero.com/huracan-cosme-provoca-muerte-de-policia-en-guerrero/|url-status=dead}} High seas flooded numerous buildings across coastal towns in Colima,{{cite news|title=Volcán de Colima registra 'deslaves' por lluvia|url=http://www.eluniversal.com.mx/notas/931947.html|access-date=June 25, 2013|newspaper=El Universal|date=June 25, 2013|language=es|archive-date=October 21, 2013|archive-url=https://web.archive.org/web/20131021103848/http://www.eluniversal.com.mx/notas/931947.html|url-status=dead}}{{cite news|title=Huracán 'Cosme' causa lluvias en Colima: SMN|access-date=June 25, 2013|newspaper=La Jarnada|date=June 25, 2013|url=http://www.jornada.unam.mx/ultimas/2013/06/25/21855559-huracan-cosme-causa-lluvias-en-colima|language=es|archive-url=https://web.archive.org/web/20130627201945/http://www.jornada.unam.mx/ultimas/2013/06/25/21855559-huracan-cosme-causa-lluvias-en-colima|archive-date=2013-06-27|url-status=dead}} damaging 34 tourist facilities and killing one person.{{cite news|title=Aumentan daños en playas de Colima por Cosme|url=http://www.eluniversal.com.mx/notas/932492.html|date=June 29, 2013|access-date=June 29, 2013|archive-date=November 5, 2013|archive-url=https://web.archive.org/web/20131105040040/http://www.eluniversal.com.mx/notas/932492.html|url-status=dead}} Additionally, many restaurants built of wood and coconut were damaged. In Manzanillo, the port was closed to small craft,{{cite news|title=Cosme daña restaurantes de playa en Colima|url=http://www.eluniversal.com.mx/notas/932192.html|access-date=June 26, 2013|newspaper=El Universal|date=June 26, 2013|archive-date=October 21, 2013|archive-url=https://web.archive.org/web/20131021104327/http://www.eluniversal.com.mx/notas/932192.html|url-status=dead}} as was the port of Mazatlán.{{cite news|title=Mazatlán port close by Cosme effects|url=http://www.eluniversal.com.mx/notas/932289.html|access-date=June 29, 2013|newspaper=El Universal|date=June 26, 2013|language=es|archive-date=November 5, 2013|archive-url=https://web.archive.org/web/20131105035930/http://www.eluniversal.com.mx/notas/932289.html|url-status=dead}} Overall, 50 homes were damaged by the storm.{{cite news|title=CICLÓN COSME SE ALEJA DE MÉXICO |url=http://www.fahrenheitmagazine.com/conciencia/planeta/ciclon-cosme-se-aleja-de-mexico/ |access-date=August 3, 2013 |newspaper=Fahrenheit magazine |date=June 28, 2013 |agency=AFP |language=es |url-status=dead |archive-url=https://web.archive.org/web/20151118083014/http://www.fahrenheitmagazine.com/conciencia/planeta/ciclon-cosme-se-aleja-de-mexico/ |archive-date=November 18, 2015 }}

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{{Infobox hurricane small

| Basin = EPac

| Image = Hurricane Dalila 2013-07-02 1745Z.jpg

| Track = Dalila 2013 track.png

| Formed = June 29

| Dissipated = July 7

| 1-min winds = 70

| Pressure = 984

}}

A tropical wave was first observed over the central Atlantic on June 17. It entered the East Pacific on June 24 and steadily organized, acquiring enough organization to be declared a tropical depression by 18:00 UTC on June 29. Twelve hours later, it was upgraded to Tropical Storm Dalila. Steered northwest parallel to the coastline of Mexico, the cyclone only slowly organized despite favorable conditions, becoming a Category 1 hurricane by 12:00 UTC on July 2. After attaining peak winds of {{convert|80|mph|km/h|abbr=on|round=5}} six hours later, the influence of drier air and increasing shear caused the storm to begin a weakening trend. At 18:00 UTC on July 3, Dalila was downgraded to a tropical storm, and by 00:00 UTC on July 5, the system further weakened to a tropical depression. After becoming devoid of convection, Dalila degenerated into a remnant low at 06:00 UTC on July 7 while located roughly {{convert|460|mi|km|abbr=on|round=5}} south-southwest of Cabo San Lucas, Mexico. The low turned east-northeastward into the circulation of Tropical Storm Erick thereafter, dissipating late on July 8.{{cite report|author=Richard J. Pasch|title=Tropical Cyclone Report: Hurricane Dalila|url={{NHC TCR url|id=EP042013_Dalila}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=December 10, 2013|access-date=January 10, 2015|location=Miami, Florida|format=PDF}}

When Dalila threatened Western Mexico, the states of Colima, Michoacán, and Jalisco went under a yellow alert; Nayarit was placed on a green alert. Blue alerts were issued for Baja California Sur, Sinaloa, Guerrero, and Oaxaca.{{cite news|title=Se intensifica tormenta Dalila; enciende alerta|url=http://www.eluniversal.com.mx/notas/933089.html|access-date=July 4, 2013|newspaper=El Universal|date=July 1, 2013|archive-date=July 4, 2013|archive-url=https://web.archive.org/web/20130704191002/http://www.eluniversal.com.mx/notas/933089.html|url-status=dead}} The port of Manzanillo was closed as a precaution, where the storm brought rain and storm surge.{{cite news|title=Cierran puerto en Manzanillo por tormenta Dalila|url=http://www.eluniversal.com.mx/notas/933153.html|access-date=July 4, 2013|newspaper=El Universal|date=July 1, 2013|archive-date=October 12, 2013|archive-url=https://web.archive.org/web/20131012063750/http://www.eluniversal.com.mx/notas/933153.html|url-status=dead}} The outer rainbands of the storm also brought moderate to heavy rainfall along coastal areas of Colima and Jalisco.{{cite news|title=Tormenta 'Dalila' causará lluvias en Jalisco y Colima|url=http://www.eluniversal.com.mx/notas/933262.html|access-date=July 4, 2013|newspaper=El Universal|date=July 2, 2013|archive-date=July 7, 2013|archive-url=https://web.archive.org/web/20130707023514/http://www.eluniversal.com.mx/notas/933262.html|url-status=dead}} A total of 49 structures were damaged due to the storm.{{cite news|title=Suspenden navegación en Michoacán por Erick |url=http://www.eluniversal.com.mx/estados/2013/michoacan-tormenta-erick--934138.html |access-date=July 6, 2013 |newspaper=El Universal |date=July 5, 2013 |language=es |url-status=dead |archive-url=https://web.archive.org/web/20130709085950/http://www.eluniversal.com.mx/estados/2013/michoacan-tormenta-erick--934138.html |archive-date=July 9, 2013 }}{{cite news|last=Adriana Covarrubias |title=Acapulco y Zihuatanejo cierran bahías por Erick |url=http://www.eluniversal.com.mx/estados/2013/erick-tormenta-guerrero-acapulco-zihuatanejo-934135.html |access-date=July 6, 2013 |newspaper=El Universal |date=July 5, 2013 |language=es |url-status=dead |archive-url=https://web.archive.org/web/20130709035338/http://www.eluniversal.com.mx/estados/2013/erick-tormenta-guerrero-acapulco-zihuatanejo-934135.html |archive-date=July 9, 2013 }}

{{clear}}

{{main|Hurricane Erick (2013)}}

{{Infobox hurricane small

| Basin = EPac

| Image = Erick Jul 6 2013 2030Z (cropped).jpg

| Track = Erick 2013 track.png

| Formed = July 4

| Dissipated = July 9

| 1-min winds = 70

| Pressure = 983

}}

A tropical wave moved off the western coast of Africa on June 18 and continued westward across Central America and into the eastern Pacific by June 29. It subsequently interacted with a large cyclonic gyre, leading to an increase in convective activity and the formation of an area of low pressure. Following satellite and microwave data,{{cite report|author=Eric S. Blake|title=Tropical Depression Five-E Discussion Number 1|url=http://www.nhc.noaa.gov/archive/2013/ep05/ep052013.discus.001.shtml|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=July 4, 2013|access-date=November 2, 2013}} the disturbance was upgraded to a tropical depression at 1200 UTC on July 4. Initially, moderate easterly shear prevented much organization as the system tracked west-northwest; however, a reprieve in upper-level winds by 0000 UTC on July 5 allowed the depression to intensify into Tropical Storm Erick as convective bands gained more curvature. A period of steady intensification over the next day allowed the system to attain Category 1 hurricane intensity at 0600 UTC and reach its peak with winds of {{convert|80|mph|km/h|abbr=on|round=5}} and a minimum barometric pressure of {{convert|983|mbar|hPa inHg|abbr=on}} six hours later. Decreasing ocean temperatures caused the convective appearance to deteriorate at a steady pace; by 1800 UTC on July 7, Erick weakened to a tropical storm, and by 0600 UTC on July 9, the system no longer sustained enough organization to be considered a tropical cyclone.{{cite report|author=Lixion A. Avila|title=Tropical Cyclone Report: Hurricane Erick|url={{NHC TCR url|id=EP052013_Erick}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=August 28, 2013|access-date=November 2, 2013|format=.PDF}}

The outer rainbands of the storm brought gusty winds just offshore the Mexican coast.{{cite news|title=La tormenta tropical Erick pone en alerta al pacifico mexicano|url=http://mexico.cnn.com/nacional/2013/07/05/la-tormenta-tropical-erick-pone-en-alerta-al-pacifico-mexicano|access-date=July 5, 2013|newspaper=CNN Mexico|date=July 5, 2013|language=es}}{{cite news|title=Autoridades de Acapulco, en alerta por tormenta Erick |url=http://www.eluniversal.com.mx/estados/2013/autoridades-de-acapulco-en-alerta-por-tormenta-erick-934008.html |access-date=July 5, 2013 |newspaper=El Universal |date=July 5, 2013 |language=es |url-status=dead |archive-url=https://web.archive.org/web/20130709035327/http://www.eluniversal.com.mx/estados/2013/autoridades-de-acapulco-en-alerta-por-tormenta-erick-934008.html |archive-date=July 9, 2013 }} In Acapulco and Puerto Marques, the storm was responsible for minor flooding. Elsewhere across the state, most of the damage was due to landslides.{{cite news|title="Erick"deja inundaciones en Guerrero|url=http://www.el-mexicano.com.mx/informacion/noticias/1/2/nacional/2013/07/05/681804/erickdeja-inundaciones-en-guerrero|access-date=July 6, 2013|newspaper=El Mexicano|date=July 6, 2013|language=es}} Along the coast of Colima, {{convert|9|ft|m|adj=on}} waves were recorded.{{cite news|title=Amenaza Erick costa de Colima; registran marejadas |url=http://www.eluniversal.com.mx/estados/2013/amenaza-erick-costa-de-colima-registran-marejadas-934275.html |access-date=July 6, 2013 |newspaper=El Universal |date=July 6, 2013 |language=es |url-status=dead |archive-url=https://web.archive.org/web/20130710215701/http://www.eluniversal.com.mx/estados/2013/amenaza-erick-costa-de-colima-registran-marejadas-934275.html |archive-date=July 10, 2013 }} Although some flooding was reported across the state, damage was minor.{{cite news|last=Jiménez Padilla |first=Jesús |title=Huracán Erick provoca inundaciones en Nayarit; en Colima cierran puerto |url=http://www.elfinanciero.com.mx/component/content/article/47/21850.html |access-date=July 7, 2013 |newspaper=El Financiero |date=July 7, 2013 |url-status=dead |archive-url=https://web.archive.org/web/20130712155635/http://www.elfinanciero.com.mx/component/content/article/47/21850.html |archive-date=July 12, 2013 }} Further north, in Nayarit, however, damage was extensive. One woman died. One river overflowed its banks, which directly affected numerous cities. The Mexican military and officials in Nayarit attempted to rescue hundreds of people affected by Hurricane Erick.{{cite news|last=Guistav|title=Huracán Erick causa muerte e inundación en Nayarit|url=http://noticabos.org/2013/07/07/huracan-erick-causa-muerte-e-inundacion-en-nayarit/|access-date=July 7, 2013|newspaper=Noti Cabos|date=July 6, 2013|language=es}}

{{clear}}

{{main|Tropical Storm Flossie (2013)}}

{{Infobox hurricane small

| Basin = EPac

| Image = Flossie Jul 28 2013 2310Z (cropped).jpg

| Track = Flossie 2013 track.png

| Formed = July 25

| Dissipated = July 30

| 1-min winds = 60

| Pressure = 994

}}

A tropical wave moved off the western coast of Africa on July 9 and crossed Central America on July 18. The disturbance initially lacked a well-defined center until early on July 25 as convection steadily increased, leading the formation of a tropical depression at 00:00 UTC that day; six hours later, the depression strengthened into Tropical Storm Flossie. Steered westward amid a favorable environment, the cyclone steadily intensified, attaining peak winds of {{convert|70|mph|km/h|abbr=on|round=5}} at 12:00 UTC on July 27 as an eye became evident on satellite imagery. Flossie crossed into the Central Pacific shortly thereafter, where increasing wind shear prompted a gradual weakening trend. At 00:00 UTC on July 30, the system weakened to a tropical depression; twelve hours later, it degenerated into a remnant low while located near the northern coast of Kauai.{{cite report|author=John P. Cangialosi|author2=Derek Wroe|title=Tropical Cyclone Report: Tropical Storm Flossie|url={{NHC TCR url|id=EP062013_Flossie}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center and Central Pacific Hurricane Center|date=November 4, 2013|access-date=January 11, 2015|location=Miami, Florida and Honolulu, Hawaii|format=PDF}}

Following Flossie's crossing into the Central Pacific Hurricane Center's warning zone, a tropical storm watch was issued for Hawaii and Maui counties on July 27.{{cite web|author=Robert T. Burke|work=Central Pacific Hurricane Center|publisher=National Oceanic and Atmospheric Administration|date=July 27, 2013|access-date=July 29, 2013|title=Tropical Storm Flossie Advisory Number 13|type=Report|url=http://www.prh.noaa.gov/cphc/tcpages/archive/2013/WEB_TCPCP1.EP062013.013.1307280232.php}} All Maui County parks were closed due to the storm as county authorities activated emergency operations.{{cite news|title=Maui Activates Emergency Operations Center, All County Facilities to Close Monday|url=http://mauinow.com/2013/07/28/maui-activates-emergency-operations-center-all-county-facilities-to-close-monday/|access-date=July 29, 2013|date=July 28, 2013}} Upon becoming the first storm to directly hit the state in 20 years,{{cite news|title=Hawaii braces for tropical storm Flossie, first direct hit in 20 years|url=http://www.alaskadispatch.com/article/20130729/hawaii-braces-tropical-storm-flossie-first-direct-hit-20-years|archive-url=https://archive.today/20130730050614/http://www.alaskadispatch.com/article/20130729/hawaii-braces-tropical-storm-flossie-first-direct-hit-20-years|url-status=dead|archive-date=July 30, 2013|access-date=July 29, 2013|newspaper=Alaska Disptach|date=July 29, 2013|author=Amanda Paulson}} gusty winds downed trees and power lines. More than 9,000 residences were without electricity across the state, with most outages concentrated in Kihei, Maui, and Puna.{{cite news|title=Tropical Storm Flossie dumps rain, knocks out power as it rakes Hawaii|url=http://usnews.nbcnews.com/_news/2013/07/29/19749826-tropical-storm-flossie-dumps-rain-knocks-out-power-as-it-rakes-hawaii?lite|access-date=July 30, 2013|newspaper=NBC News|author=Henry Austin and Daniel Arkin}}{{cite news|title=Hawaiian Electric companies responding to power outages following Flossie|url=http://www.khon2.com/2013/07/29/hawaiian-electric-companies-responding-to-power-outages-following-flossie/|access-date=July 29, 2013|date=July 29, 2013|author=Web Staff|agency=Khon2}}{{cite news|title=Thousands on Maui, Big Island without electricity|url=http://www.staradvertiser.com/news/hawaiinews/20130730__Thousands_on_Maui_Big_Island_without_electricity_.html?id=217562501|access-date=July 30, 2013|newspaper=Hawaii Star-Advertiser|date=July 29, 2013|author=Alan Yonan Jr.}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Gil Jul 31 2013 2045Z.png

| Track = Gil 2013 track.png

| Formed = July 30

| Dissipated = August 6

| 1-min winds = 75

| Pressure = 985

}}

The formation of Gil is attributed to a tropical wave that departed the west coast of Africa on July 16 and entered the East Pacific on July 24. Initially disheveled, the wave slowly organized as convection increased and its associated center became better defined, leading to the formation of a tropical depression at 12:00 UTC on July 30; six hours later, the depression strengthened into Tropical Storm Gil. With a small circulation, the cyclone entered a period of rapid deepening, intensifying into a Category 1 hurricane at 18:00 UTC on July 31 and attaining peak winds of {{convert|85|mph|km/h|abbr=on|round=5}} a day later. Thereafter, increasing shear and drier air caused the storm to begin weakening; at 18:00 UTC on August 2, Gil weakened to a tropical storm, and two days later, it weakened further to a tropical depression. A brief burst of convection allowed the cyclone to regain tropical storm intensity at 06:00 UTC on August 6 as it crossed into the Central Pacific, but Gil quickly weakened to a tropical depression twelve hours later. At 00:00 UTC on August 7, the system degenerated into an open trough well east-southeast of the Hawaiian Islands.{{cite report|author=John L. Beven II|author2=Sam Houston|title=Tropical Cyclone Report: Hurricane Gil|url={{NHC TCR url|id=EP072013_Gil}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center and Central Pacific Hurricane Center|date=February 6, 2014|access-date=January 11, 2015|location=Miami, Florida and Honolulu, Hawaii|format=PDF}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Henriette Aug 8 2013 1945Z.jpg

| Track = Henriette 2013 track.png

| Formed = August 3

| Dissipated = August 11

| 1-min winds = 90

| Pressure = 976

}}

A tropical wave emerged off the western coast of Africa on July 19 and reached the East Pacific on July 26. Embedded within the Intertropical Convergence Zone, convection slowly coalesced about an area of low pressure, leading to the formation of a tropical depression by 12:00 UTC on August 3; twelve hours later, the depression intensified into Tropical Storm Henriette while located about {{convert|1,800|mi|km|abbr=on}} southwest of the southern tip of Baja California. The system initially moved west-southwest following formation, but turned toward the west-northwest as it reached the western periphery of a mid-level ridge to its north. Amid a favorable environment, Henriette steadily intensified, becoming a Category 1 hurricane by 06:00 UTC on August 6 and unexpectedly attaining peak winds of {{convert|105|mph|km/h|abbr=on|round=5}} by 18:00 UTC on August 8. The hurricane quickly weakened over increasingly cool waters as it resumed its southwesterly track into the Central Pacific, weakening to a tropical storm early on August 9 and further to a tropical depression two days later. By 18:00 UTC on August 11, the effects of increasing wind shear caused Henriette to degenerate into a remnant low while positioned roughly {{convert|430|mi|km|abbr=on|round=5}} south of Kailua-Kona, Hawaii. The remnant low drifted west-southwest until dissipating the next day.{{cite report|author=Robbie J. Berg|author2=Jeff Powell|title=Tropical Cyclone Report: Hurricane Henriette|url={{NHC TCR url|id=EP082013_Henriette}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center and Central Pacific Hurricane Center|date=January 23, 2014|access-date=January 14, 2015|location=Miami, Florida and Honolulu, Hawaii|format=PDF}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Pewa Aug 17 2013 2255Z.jpg

| Track = Pewa 2013 track.png

| Formed = August 16

| Dissipated = August 18 (Exited basin)

| 1-min winds = 55

| Pressure = 1000

}}

A broad trough was first identified west of Central America in early August. This trough drifted westward to the south of the Hawaiian Islands by August 14, where it yielded three defined areas of disturbed weather. Largely devoid of convection initially, the westernmost disturbance steadily organized over the coming days, leading to the formation of a tropical depression by 06:00 UTC on August 16; six hours later, the depression intensified into Tropical Storm Pewa. The cyclone tracked west-northwest following formation, steered by a mid-level ridge to its north. Pewa crossed the International Date Line into the West Pacific on August 18, where it would later become a typhoon before succumbing to unfavorable wind shear.{{cite report|author=Thomas Birchard|title=Tropical Cyclone Report: Tropical Storm/Typhoon Pewa|url=https://www.nhc.noaa.gov/data/tcr/CP012013_Pewa.pdf|publisher=National Oceanic and Atmospheric Administration|work=Central Pacific Hurricane Center|date=January 10, 2015|access-date=June 9, 2019|location=Honolulu, Hawaii}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Unala Aug 19 2013 0105Z.jpg

| Track = Unala 2013 track.png

| Formed = August 19

| Dissipated = August 19 (Exited basin)

| 1-min winds = 35

| Pressure = 1005

}}

On August 10, the CPHC began monitoring a trough located roughly {{convert|1,300|mi|km|abbr=on}} east-southeast of the Big Island of Hawaii for potential development.{{cite web|work=Central Pacific Hurricane Center |publisher=National Oceanic and Atmospheric Administration |date=August 10, 2013 |access-date=August 19, 2013 |title=Tropical Weather Outlook |url=http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308102346.txt |format=Report |url-status=dead |archive-url=https://web.archive.org/web/20170209120742/http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308102346.txt |archive-date=February 9, 2017 }} Disorganized convective activity developed in association with the trough as it moved generally westward.{{cite web|work=Central Pacific Hurricane Center |publisher=National Oceanic and Atmospheric Administration |date=August 11, 2013 |access-date=August 19, 2013 |title=Tropical Weather Outlook |url=http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308111746.txt |format=Report |url-status=dead |archive-url=https://web.archive.org/web/20160304210106/http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308111746.txt |archive-date=March 4, 2016 }} By August 13, multiple areas of vorticity formed within the disturbance, hindering its development into a coherent cyclone.{{cite web|work=Central Pacific Hurricane Center |publisher=National Oceanic and Atmospheric Administration |date=August 13, 2013 |access-date=August 19, 2013 |title=Tropical Weather Outlook |url=http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308130552.txt |format=Report |url-status=dead |archive-url=https://web.archive.org/web/20160304040511/http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308130552.txt |archive-date=March 4, 2016 }} Marginally favorable environmental conditions allowed for some organization on August 15.{{cite web|work=Central Pacific Hurricane Center |publisher=National Oceanic and Atmospheric Administration |date=August 15, 2013 |access-date=August 19, 2013 |title=Tropical Weather Outlook |url=http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308151155.txt |format=Report |url-status=dead |archive-url=https://web.archive.org/web/20160304205344/http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308151155.txt |archive-date=March 4, 2016 }} Following an increase strong thunderstorms around the center, the CPHC stated that it was becoming a tropical depression.{{cite web|work=Central Pacific Hurricane Center |publisher=National Oceanic and Atmospheric Administration |date=August 15, 2013 |access-date=August 19, 2013 |title=Special Tropical Weather Outlook |url=http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308151410.txt |format=Report |url-status=dead |archive-url=https://web.archive.org/web/20181027101308/https://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308151410.txt |archive-date=October 27, 2018 }} However, outflow from a nearby disturbance, which would soon become Tropical Storm Pewa, disrupted the system and caused it to become more disorganized.{{cite web|work=Central Pacific Hurricane Center |publisher=National Oceanic and Atmospheric Administration |date=August 16, 2013 |access-date=August 19, 2013 |title=Tropical Weather Outlook |url=http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308160514.txt |format=Report |url-status=dead |archive-url=https://web.archive.org/web/20170225031107/http://www.nhc.noaa.gov/archive/text/TWOCP/2013/TWOCP.201308160514.txt |archive-date=February 25, 2017 }} Late on August 19 the depression strengthened into a tropical storm. However, outflow from the nearby Typhoon Pewa caused an increase in wind shear over the system, causing Unala to become disorganized and weaken. By this time the system has crossed into the Western Pacific basin. During the afternoon hours of August 19, the depression had dissipated completely, as it was being absorbed by Pewa.{{cite report|author=Derek Wroe|title=Tropical Cyclone Report: Tropical Storm Unala|url=https://www.nhc.noaa.gov/data/tcr/CP022013_Unala.pdf|publisher=National Oceanic and Atmospheric Administration|work=Central Pacific Hurricane Center|date=June 19, 2014|access-date=June 9, 2019|location=Honolulu, Hawaii}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = 03C Aug 19 2013 2245Z.jpg

| Track = 03-C 2013 track.png

| Formed = August 19

| Dissipated = August 20 (Exited basin)

| 1-min winds = 30

| Pressure = 1008

}}

The third in a trio of Central Pacific tropical cyclones was first monitored by the NHC on August 9. The disturbance formed a weak surface low three days later but ultimately opened into a trough as it entered the CPHC's area of responsibility on August 14. There, steady organization led to the formation of a tropical depression around 18:00 UTC on August 19. Upper-level outflow from nearby Tropical Storm Pewa imparted shear on the newly formed system, and it failed to attain tropical storm strength, instead crossing the International Date Line as a tropical depression on August 20 and dissipating the next day.{{cite report|author=Sam Houston|title=Tropical Cyclone Report: Tropical Depression Three-C|url=https://www.nhc.noaa.gov/data/tcr/CP032013_Three-C.pdf|publisher=Central Pacific Hurricane Center|date=February 2, 2015|access-date=June 9, 2019|location=Honolulu, Hawaii}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Tropical Storm Ivo 2013-08-23 2030Z.jpg

| Track = Ivo 2013 track.png

| Formed = August 22

| Dissipated = August 25

| 1-min winds = 40

| Pressure = 997

}}

The southern portion of a tropical wave entered the East Pacific on August 15. Although moderate shear initially hindered the organization of convection, a broad low- to mid-level circulation formed and steadily coalesced. Upper-level winds lessened on August 22 as the disturbance turned northwestward, leading to the formation of a tropical depression by 12:00 UTC. Following designation, the depression began to interact with a tropical wave to its east, ultimately leading to an abrupt center formation to the northeast. By 00:00 UTC on August 23, the cyclone intensified into Tropical Storm Ivo. Resuming its northwest track around a mid-level ridge across the central United States and Mexico, Ivo attained peak winds of {{convert|45|mph|km/h|abbr=on|round=5}} before crossing a sharp sea surface temperature gradient. The system weakened to a tropical depression by 00:00 UTC on August 25 and further degenerated into a remnant low by 18:00 UTC on August 25 while located less than {{convert|115|mi|km|abbr=on|round=5}} west of the west-central coast of the Baja California peninsula. The remnant low drifted slowly south-southwestward before dissipating early on August 28.{{cite report|author=Todd B. Kimberlain|title=Tropical Cyclone Report: Tropical Storm Ivo|url={{NHC TCR url|id=EP092013_Ivo}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=November 25, 2013|access-date=January 14, 2015|location=Miami, Florida|format=PDF}}

When the system first posed a threat to the Baja California Peninsula, a "green alert" was declared for Socorro Island and Baja California Sur.{{cite news|title=Alerta verde en BCS por tormenta tropical Ivo: Sinaproc|url=http://www.elimparcial.com/EdicionEnLinea/Notas/Nacional/23082013/744735-Alerta-verde-en-BCS-por-tormenta-tropical-Ivo-Sinaproc.html|access-date=August 23, 2013|newspaper=El Imparical|date=August 23, 2013}} At 21:00 UTC on August 23, a tropical storm warning was issued from Punta Abreojos to Loreto, including Cabo San Lucas. A tropical storm watch was placed for the Baja California Peninsula from Punta Abreojos to Punta Eugenia.{{cite news|title=Tropical Storm Ivo heads north in eastern Pacific|url=http://www.sandiegouniontribune.com/news/2013/aug/23/tropical-storm-ivo-heads-north-in-eastern-pacific/|access-date=November 19, 2015|newspaper=San Diego Union Tribune|date=August 23, 2013|agency=Associated Press}} Seven ports in Baja California Sur were closed.{{cite news|title=Cierran siete puertos en BCS por tormenta Ivo|url=http://www.eluniversal.com.mx/estados/2013/cierran-siete-puertos-en-bcs-por-ivo-944957.html|access-date=August 27, 2013|newspaper=El Universal|date=August 24, 2013|language=es}} Along the peninsula, 6,000 people were affected and many highways were damaged. Water supply was cut off to Loreto.{{cite news|title=BCS reporta mil 600 afectados por tormenta Ivo|url=http://www.eluniversal.com.mx/estados/2013/bcs-afectaciones-tormenta-ivo-945403.html|access-date=August 27, 2013|newspaper=El Universal|date=August 26, 2013|language=es}} In all, 400 people were evacuated and 200 homes were flooded. Six people were injured, including two serious.{{cite news|title=Alerta en Veracruz por Fernand|url=http://www.eluniversal.com.mx/estados/2013/impreso/alerta-en-veracruz-por-8220fernand-8221-92147.html|access-date=August 27, 2013|newspaper=El Universal|date=August 26, 2013}} Damages in Baja California totaled to MXN$1.126 billion (USD$88.3 million).{{Cite web |last=Arróliga García |first=Norlang Marcel |last2=Marin Cambranis |first2=Rafael Humberto |last3=Méndez Estrada |first3=Karla Margarita |last4=Reyez Rodríguez |first4=Rosa |date=2013 |title=Impacto Socioeconómico de los Principales Desastres Ocurridos en la República Mexicana en 2013 |url=https://www.cenapred.unam.mx/es/Publicaciones/archivos/324-NO.15-IMPACTOSOCIOECONMICODELOSPRINCIPALESDESASTRESOCURRIDOSENMXICOENELAO2013.PDF |access-date=September 18, 2024 |website=cenapred.unam.mx}} In the United States, flash flood watches were issued for Pima County,{{cite news|title=Ivo keeps monsoon active today|url=http://www.kvoa.com/news/ivo-keeps-monsoon-active-today/|access-date=August 25, 2013|newspaper=KOVA News|date=August 25, 2013|archive-url=https://web.archive.org/web/20130827101238/http://www.kvoa.com/news/ivo-keeps-monsoon-active-today/|archive-date=2013-08-27|url-status=dead}} extending westward across western Arizona and into Southern Nevada.{{cite news|title=Las Vegas copes with sporadic flooding|url=http://www.mohavedailynews.com/articles/2013/08/27/news/state/doc521c529d8dc84281956751.txt|access-date=August 27, 2013|newspaper=Mohave Daily News|date=August 27, 2013}} Several roads were closed in Yuma County.{{cite news|title=Tropical Depression Ivo brings showers to Yuma County|url=http://www.abc15.com/weather/weather-news/tropical-depression-ivo-brings-showers-to-yuma-county|access-date=October 7, 2015|newspaper=ABC 15 News|date=August 25, 2013}} In East County, many roads were flooded.{{cite news|title=Heavy rains flood roads in East County|url=http://fox5sandiego.com/2013/08/25/heavy-rains-flood-roads-in-east-county/|access-date=October 8, 2015|newspaper=FOX 5 News San Diego|date=August 25, 2013}} Elsewhere, Borrego Springs saw {{convert|3|in|mm}} of rain in less than an hour, resulting in flash flooding, which stranded motorists.{{cite news|title=Flash floods strand cars in Southern CA desert|url=http://www.sacbee.com/2013/08/25/5680246/flash-floods-strand-cars-in-southern.html|access-date=August 25, 2013|newspaper=The Sacramento Bee|date=August 25, 2013|agency=Associated Press|archive-url=https://web.archive.org/web/20130829025900/http://www.sacbee.com/2013/08/25/5680246/flash-floods-strand-cars-in-southern.html|archive-date=2013-08-29|url-status=dead}} Several mudslides were also reported in San Bernardino County. One person drowned in Needles after flood waters overwhelmed her vehicle;{{cite news|title=Thunderstorms pound S. Cal for second day|url=http://www.utsandiego.com/news/2013/aug/26/thunderstorms-pound-s-cal-for-second-day/|access-date=August 27, 2013|newspaper=UT San Diego|date=August 26, 2013}} 18 swift water rescues were made in the same area. Heavy rains in Nevada, amounting to nearly {{convert|4|in|mm|abbr=on}} at Mount Charleston, caused significant flooding; damage in the Las Vegas Valley reached $300,000.{{cite web|publisher=The Weather Channel|date=August 26, 2013|access-date=August 27, 2013|title=Las Vegas Area Flooding: Death Blamed on Remnants of Tropical Storm Ivo|url=http://www.weather.com/news/las-vegas-flooding-crews-carry-out-18-water-rescues-20130826}} Widespread flooding occurred around Zion National Park.{{cite news|title=Heavy rains wash through Southern Utah|url=http://www.thespectrum.com/article/20130826/NEWS01/308260015/|access-date=August 27, 2013|newspaper=The Spectrum|date=August 26, 2013|archive-url=https://archive.today/20130827235338/http://www.thespectrum.com/article/20130826/NEWS01/308260015/|archive-date=2013-08-27|url-status=dead}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Juliette Aug 28 2013 1740Z.jpg

| Track = Juliette 2013 track.png

| Formed = August 28

| Dissipated = August 29

| 1-min winds = 55

| Pressure = 997

}}

An area of convection occurred on August 25. It was classified as a disturbance the next day. Late on August 27, the disturbance entered warm waters as it became Tropical Depression Ten-E. Due to warm waters and windshear, Ten-E intensified into Tropical Storm Juliette late on August 28.{{cite report|author=Daniel P. Brown|title=Tropical Storm Juliette Public Advisory Number 1|url=http://www.nhc.noaa.gov/archive/2013/ep10/ep102013.discus.001.shtml|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=August 28, 2013|access-date=August 28, 2013}} As Juliette races towards northwest, it reached peak intensity and then rapidly weakened to a depression on August 29. The NHC issued its final advisories later that day while Juliette's remnants continued to move west, with its circulation dissipating very early on August 31.{{NHC TCR url|id=EP102013_Juliette}}

Upon formation, a "green alert" was issued for Sonora, the northern portion of the Baja California Peninsula, Jalisco, Nayarit, and Socorro Island, while a "blue alert" was issued for Baja California Sur and Colima.{{cite news|title=Tormenta Juliette prende alertas en siete estados|url=http://www.eluniversal.com.mx/estados/2013/tormenta-juliette-prede-alertas-en-siete-estados-946105.html|access-date=August 28, 2013|newspaper=El Universal|date=August 28, 2013|language=es}} Six shelters opened for in San José del Cabo and Cabo San Lucas{{cite news|title=Evacuan Los Cabos por tormenta Juliette|url=http://www.eluniversal.com.mx/estados/2013/evacuan-los-cabos-por-tormenta-juliette-946137.html|access-date=August 29, 2013|newspaper=El Universal|date=August 28, 2013|language=es}} and were used by 164 residents,{{cite news|title=Tormenta Juliette toca tierra en Baja California Sur|access-date=August 29, 2013|newspaper=El Universal|url=http://www.eluniversal.com.mx/estados/2013/tormenta-juliette-toca-tierra-en-baja-california-sur-946144.html|date=August 29, 2013|language=es}} though many refused to go. Much of Baja California Sur briefly lost power, including the communities of Todos Santos and Pescadero, and portions of Cabo San Lucas and San José del Cabo. Furthermore, one man was electrocuted and later died. One home was destroyed.{{cite news|title=Tropical Storm Juliette hits Mexico resorts|access-date=November 19, 2015|url=http://www.mercurynews.com/ci_23971341/tropical-storm-juliette-moving-along-mexican-coast|newspaper=San Jose Mercury News|date=August 29, 2013|agency=Associated Press}} A total of 1,600 persons spent the night in a shelter.{{cite news|title=Tropical Storm Juliette kills one near Mexican tourist hub|url=https://www.reuters.com/article/us-storm-juliette-idUSBRE97S03620130829|access-date=September 6, 2013|date=August 29, 2013|author=Lizbeth Diaz|work=Reuters}} However, there were no reports of significant damages from the storm.

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Kiko Aug 31 2013 2120Z.jpg

| Track = Kiko 2013 track.png

| Formed = August 30

| Dissipated = September 2

| 1-min winds = 65

| Pressure = 989

}}

On August 28, a trough within the ITCZ was first identified well south-southwest of the southern tip of Baja California. That day, an area of low pressure formed along the trough and tracked northwest. A tropical wave, one responsible for the development of tropical storms Erin and Fernand in the Atlantic, and Tropical Storm Juliette in the East Pacific, bypassed the low on August 30, leading to an increase in convection and the formation of a tropical depression by 12:00 UTC that day. The depression initially strengthened slowly under the influence of moderate northerly wind shear, becoming a tropical storm by 12:00 UTC on August 31. Thereafter, upper-level winds became more conducive as the system turned north-northeast, and Kiko began a period of rapid deepening yielding peak winds of {{convert|75|mph|km/h|abbr=on|round=5}} by 06:00 UTC on September 1. Following peak, an increase in wind shear and track over cooler waters led to a weakening trend. Kiko deteriorated into a tropical storm by 18:00 UTC and further degenerated into a remnant low by 12:00 UTC on September 2. The remnant low executed a cyclonic loop and tracked southeast before dissipating on September 4.{{cite report|author=Daniel P. Brown|title=Tropical Cyclone Report: Hurricane Kiko|url={{NHC TCR url|id=EP112013_Kiko}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=November 4, 2013|access-date=January 21, 2015|location=Miami, Florida|format=PDF}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Image = Lorena 2013-09-06 2045Z.jpg

| Track = Lorena 2013 track.png

| Formed = September 5

| Dissipated = September 7

| 1-min winds = 45

| Pressure = 1002

}}

The formation of Lorena is attributed to a tropical wave first identified over Central America on August 31. The wave moved slowly across the East Pacific for several days while remaining disorganized. However, by 06:00 UTC on September 5, the disturbance acquired sufficient organization to be declared a tropical depression; six hours later, the depression intensified into Tropical Storm Lorena. Steered northwest around a mid-level ridge over Mexico, an elongation of the low-level center, separation of the low and mid-level centers, and light to moderate southwesterly shear prompted only gradual strengthening, and Lorena attained peak winds of {{convert|50|mph|km/h|abbr=on|round=5}} on September 6. Thereafter, the introduction of dry and stable air caused the cyclone to become disheveled as associated convection dissipated. Lorena weakened to a tropical depression at 12:00 UTC on September 7 and degenerated into a remnant low six hours later while located {{convert|60|mi|km|abbr=on|round=5}} west-southwest of Santa Fe, Mexico. The low turned west and south before opening up into a trough early on September 9.{{cite report|author=Eric S. Blake|title=Tropical Cyclone Report: Tropical Storm Lorena|url={{NHC TCR url|id=EP122013_Lorena}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=January 8, 2014|access-date=January 14, 2015|location=Miami, Florida|format=PDF}}

Upon becoming a tropical cyclone, a "yellow alert" was issued for Colima and Nayarit. A "green alert" was issued for Socorro Island, Michoacán, and Jalisco while a "blue alert" was in effect for Baja California Sur and Sinaloa.{{cite news|title=Se forma tormenta tropical Lorena en el Océano Pacífico Se forma tormenta tropical Lorena en el Océano Pacífico|url=http://www.eluniversal.com.mx/estados/2013/tormenta-tropical-lorena-lluvias-948398.html|access-date=September 6, 2013|newspaper=El Universal|date=September 5, 2013|language=es}} Classes were suspended for Los Cabos.{{cite news|title=Suspenden clases en BCS por tormenta Lorena|url=http://www.eluniversal.com.mx/estados/2013/bcs-clases-tormenta-lorena-948462.html|access-date=September 6, 2013|newspaper=El Universal|date=September 6, 2013|language=es}} The ports of Mazatlán, La Paz, Cabo San Lucas, Los Barriles, and San José del Cabo were closed because of high waves.{{cite news|title=Cierran navegación en Mazatlán por Lorena|url=http://www.eluniversal.com.mx/estados/2013/mazatlan-puerto-tormenta-lorena-948465.html|access-date=September 6, 2013|newspaper=El Universal|date=September 6, 2013|language=es}}{{cite news|title=BCS cierra cuatro puertos por tormenta Lorena|url=http://www.eluniversal.com.mx/estados/2013/bcs-puertos-tormenta-lorena-948511.html|access-date=September 6, 2013|newspaper=El Universal|date=September 6, 2013}} Lorena brought moderate rain over the peninsula.{{cite news|title=Lorena afecta BCS; alistan sesión de Protección Civil|url=http://www.eluniversal.com.mx/estados/2013/tormenta-lorena-bcs-sesion-proteccion-civil-948479.html|access-date=September 6, 2013|newspaper=El Universal|date=September 6, 2013|language=es}} However, there were no reports of significant damages from the storm in Baja California. The remnants of Lorena caused flash flooding in Arizona, causing minor damage to homes and vehicles. Damage in Arizona is estimated at USD$25,000.{{Cite web |title=Storm Events Database - Event Details {{!}} National Centers for Environmental Information |url=https://www.ncdc.noaa.gov/stormevents/eventdetails.jsp?id=477041 |access-date=2024-09-21 |website=www.ncdc.noaa.gov}}

{{clear}}

{{Main|Hurricane Manuel}}

{{Infobox hurricane small

| Basin = EPac

| Image = Manuel Sept 18 2013 1800Z.jpg

| Track = Manuel 2013 track.png

| Formed = September 13

| Dissipated = September 19

| 1-min winds = 65

| Pressure = 983

}}

On September 13, a tropical depression formed off the southwest coast of Mexico from a tropical wave that entered the basin two days earlier. Six hours later, it intensified into Tropical Storm Manuel while moving northwestward. The storm turned to the north on September 14 as a mid-level ridge over central Mexico weakened. By 06:00 UTC on September 14, Manuel initially attained peak winds of {{convert|70|mph|km/h|abbr=on|round=5}}, which it maintained upon moving ashore near Pichilinguillo, Mexico six hours later. Once inland, Manuel weakened quickly over the high terrain of Mexico, degenerating into a weak trough by 06:00 UTC on September 16. The remnant mid-level center and trough continued to the northwest around the ridge, emerging into the Gulf of California during the afternoon of September 16. After the convection reorganized, Manuel reformed into a tropical depression about {{convert|175|mi|km|abbr=on|round=5}} east of Cabo San Lucas, Mexico. Within an environment exceptionally conducive for intensification, Manuel began a period of rapid deepening, becoming a tropical storm for a second time by 06:00 UTC on September 18 and a Category 1 hurricane by 00:00 UTC on September 19. Twelve hours later, the system made landfall near Culiacán, Mexico with peak winds of {{convert|75|mph|km/h|abbr=on|round=5}}. Manuel quickly weakened as it once again passed over the higher terrain of Mexico, becoming a tropical storm by 18:00 UTC and further degenerating into a broad area of low pressure over the Sierra Madre Occidental mountain range by 00:00 UTC on September 20.{{cite report|author=Richard J. Pasch|author2=David A. Zelinsky|title=Tropical Cyclone Report: Hurricane Manuel|url={{NHC TCR url|id=EP132013_Manuel}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=January 6, 2014|access-date=January 13, 2015|location=Miami, Florida|format=PDF}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Formed = October 6

| Dissipated = October 10

| Image = Narda Oct 7 2013 2135Z.jpg

| Track = Narda 2013 track.png

| 1-min winds = 55

| Pressure = 997

}}

A tropical wave emerged off the western coast of Africa on September 12 and entered the East Pacific almost two weeks later. On October 1, an area of low pressure detached from the wave and began to organize as it moved west-northwest. Organized convective bands were observed by 18:00 UTC on October 6, marking the formation of a tropical depression about {{convert|865|mi|km|abbr=on}} southwest of the southern tip of Baja California; six hours later, the depression strengthened into Tropical Storm Narda. Amid a favorable environment, the cyclone steadily intensified after designation, attaining peak winds of {{convert|65|mph|km/h|abbr=on|round=5}} by 18:00 UTC on October 7 as a partial eyewall became evident on satellite. However, associated convection began to weaken thereafter as Narda encountered drier air and stronger wind shear. At 00:00 UTC on October 9, Narda weakened to a tropical depression; after producing intermittent convection for a day, the system degenerated into a remnant low by 12:00 UTC on October 10. The low moved southwest and dissipated a few days later.{{cite report|author=Lixion A. Avila|title=Tropical Cyclone Report: Tropical Storm Narda|url={{NHC TCR url|id=EP142013_Narda}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=November 13, 2013|access-date=January 19, 2015|location=Miami, Florida|format=PDF}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Formed = October 12

| Dissipated = October 15

| Image = Octave Oct 13 2013 2100Z.jpg

| Track = Octave 2013 track.png

| 1-min winds = 55

| Pressure = 994

}}

A tropical wave moved across Central America and into the East Pacific on October 5. While passing south of the coastline of Mexico, the wave interacted with a large area of disturbed weather at the base of an upper-level trough, and the two features eventually merged by October 7. The incipient disturbance steadily organized over subsequent days, leading to the formation of a tropical depression by 18:00 UTC on October 12 while located about {{convert|545|mi|km|abbr=on|round=5}} south of the southern tip of Baja California; six hours later, the depression intensified into Tropical Storm Octave. Gradually recurving northeast around a subtropical ridge, the cyclone steadily strengthened amid a favorable atmospheric environment, reaching a peak intensity of {{convert|65|mph|km/h|abbr=on|round=5}} by 18:00 UTC on October 13. Thereafter, the cloud pattern became increasingly disorganized as wind shear increased the storm moved over cooler waters. The system moved ashore near Cabo San Lazaro, Mexico at 05:00 UTC on October 15 with maximum winds of {{convert|45|mph|km/h|abbr=on|round=5}} and quickly weakened over land. By 12:00 UTC, Octave weakened to a tropical depression, and six hours later, it further degenerated into a remnant low over the southern portion of Sonora. The low dissipated shortly thereafter.{{cite report|author=John P. Cangialosi|title=Tropical Cyclone Report: Tropical Storm Octave|url={{NHC TCR url|id=EP152013_Octave}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=December 2, 2013|access-date=January 19, 2015|location=Miami, Florida|format=PDF}}

6 inches of rain were reported in Baja California Sur and Northern Mexico. However, only minor flooding was reported. Moisture from Octave caused flash flooding in Texas and New Mexico. Damages from in both states totaled to US$34,000.{{Cite web |title=Storm Events Database - Search Results {{!}} National Centers for Environmental Information |url=https://www.ncdc.noaa.gov/stormevents/textsearch.jsp?q=Tropical+Storm+Octave |access-date=2024-09-21 |website=www.ncdc.noaa.gov}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Formed = October 14

| Dissipated = October 16

| Image = Priscilla Oct 14 2013 1840Z.jpg

| Track = Priscilla 2013 track.png

| 1-min winds = 40

| Pressure = 1001

}}

An area of convection, possibly in relation to a tropical wave that emerged off the western coast of Africa on September 16, developed along the ITCZ on October 7. Becoming embedded within a pre-existing, broad circulation, the disturbance only slowly congealed due to wind shear from nearby Tropical Storm Octave. Despite this, it acquired sufficient organization to be deemed a tropical depression by 00:00 UTC on October 14 while located about {{convert|810|mi|km|abbr=on}} south-southwest of the southern tip of Baja California. Steered northwest and north around a mid-level ridge over Mexico, the depression became a tropical storm by 06:00 UTC and attained peak winds of {{convert|45|mph|km/h|abbr=on|round=5}} six hours later. Thereafter, a combination of cooler waters and the continued influences of Octave caused Priscilla to weaken. At 18:00 UTC on October 15, it was downgraded to a tropical depression, and by 18:00 UTC the following day, the cyclone degenerated into a remnant low. The low turned westward before dissipating on October 18.{{cite report|author=John L. Beven II|title=Tropical Cyclone Report: Tropical Storm Priscilla|url={{NHC TCR url|id=EP162013_Priscilla}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=February 5, 2014|access-date=January 19, 2015|location=Miami, Florida|format=PDF}}

{{clear}}

{{Main|Hurricane Raymond (2013)}}

{{Infobox hurricane small

| Basin = EPac

| Formed = October 20

| Dissipated = October 30

| Image = Raymond Oct 21 2013 2010Z (cropped).jpg

| Track = Raymond 2013 track.png

| 1-min winds = 110

| Pressure = 951

}}

A disturbance within the ITCZ was first identified over the southwestern Caribbean Sea on October 13, crossing Central America and entering the East Pacific over the subsequent three days. Deep convection steadily increased and organized into curved spiral bands, leading to the formation of a tropical depression by 00:00 UTC on October 20; six hours later, it was upgraded to Tropical Storm Raymond. Steered northwest by a series of ridges to the cyclone's north, Raymond rapidly intensified amid warm ocean temperatures and low wind shear, becoming a hurricane by 00:00 UTC on October 21 and attaining Category 3 status with peak winds of {{convert|125|mph|km/h|abbr=on|round=5}} by 18:00 UTC that day. Executing a clockwise loop, significant cold water upwelling and increased upper-level winds caused the cyclone to weaken abruptly, deteriorating to tropical storm intensity by 06:00 UTC on October 23. Environmental conditions became more favorable for intensification the next day, allowing Raymond to gradually intensify to hurricane strength by 12:00 UTC on October 27 and further to Category 2 hurricane intensity twelve hours later. Recurving northeast under the influence of an approaching trough, the cyclone began to weaken once again as wind shear increased, with the system weakening below hurricane threshold again by 00:00 UTC on October 29 and further to tropical depression status by 06:00 UTC on October 30. After all associated convection dissipated, Raymond degenerated to a remnant low by 12:00 UTC. The remnant low turned west and dissipated on November 1.{{cite report|author=Robbie J. Berg|title=Tropical Cyclone Report: Hurricane Raymond|url={{NHC TCR url|id=EP172013_Raymond}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=January 6, 2014|access-date=January 20, 2015|location=Miami, Florida|format=PDF}}

Despite remaining offshore, Raymond's close proximity to the Mexican coast was enough to prompt tropical cyclone warnings and watches.{{cite news|title=En alerta roja por Raymond, Guerrero y Michoacán|url=http://www.eluniversal.com.mx/estados/2013/huracan-raymond-alerta-michoacan-guerrero-clases-959676.html|access-date=October 21, 2013|newspaper=El Universal|date=October 21, 2013|language=es|archive-date=October 25, 2013|archive-url=https://web.archive.org/web/20131025232502/http://www.eluniversal.com.mx/estados/2013/huracan-raymond-alerta-michoacan-guerrero-clases-959676.html|url-status=dead}} Due to the threat of rainfall, residents from 81 municipalities in Mexico were ordered to evacuate out of flood-prone regions.{{cite news|title=Por Raymond, pide Aguirre emergencia para 9 municipios|url=http://www.eluniversal.com.mx/estados/2013/por-raymond-pide-aguirre-emergencia-para-9-municipios-959605.html|access-date=October 20, 2013|newspaper=El Universal|date=October 20, 2013|language=es|archive-date=February 23, 2014|archive-url=https://web.archive.org/web/20140223000852/http://www.eluniversal.com.mx/estados/2013/por-raymond-pide-aguirre-emergencia-para-9-municipios-959605.html|url-status=dead}}{{cite web|title='Raymond' incrementa su fuerza y ya es huracán categoría 2|url=http://www.animalpolitico.com/2013/10/raymond-ya-es-huracan-categoria-1|publisher=Animal Politico|date=October 20, 2013|access-date=October 21, 2013|language=es|archive-date=September 6, 2020|archive-url=https://web.archive.org/web/20200906235021/https://www.animalpolitico.com/2013/10/raymond-ya-es-huracan-categoria-1/|url-status=dead}} Precipitation from Raymond peaked at {{convert|7.63|in|mm|abbr=on}} near Acapulco within a two-day period.{{cite news|title=Hurricane Raymond weakens near Mexico |url=http://www.lansingstatejournal.com/usatoday/article/3142927 |archive-url=https://archive.today/20131023141122/http://www.lansingstatejournal.com/usatoday/article/3142927 |url-status=dead |archive-date=October 23, 2013 |access-date=October 22, 2013 |newspaper=Langiston Journal |date=October 22, 2013 |author=Doyle Rice |author2=USA Today |agency=Associated Press }} Minor flooding resulted from the outer rainbands of the hurricane.{{cite news|title=Evacuan colonias de Acapulco por huracán Raymond|url=http://www.eluniversal.com.mx/estados/2013/acapulco-evacuacion-huracan-raymond-959710.html|access-date=October 21, 2013|newspaper=El Universal|date=October 21, 2013|language=es|archive-date=January 1, 2015|archive-url=https://web.archive.org/web/20150101160634/http://www.eluniversal.com.mx/estados/2013/acapulco-evacuacion-huracan-raymond-959710.html|url-status=dead}} Though no deaths were reported, 585 people were rendered homeless. Following the storm, the Mexican government declared a state of emergency for 10 municipalities in Guerrero.{{cite news|title=Fonden para 11 municipios tras Raymond; reanudan clases|url=http://www.eluniversal.com.mx/estados/2013/reanudan-labores-guerrero-960163.html|access-date=October 22, 2013|newspaper=El Universal|date=October 22, 2013|language=es|archive-date=November 11, 2013|archive-url=https://web.archive.org/web/20131111031144/http://www.eluniversal.com.mx/estados/2013/reanudan-labores-guerrero-960163.html|url-status=dead}}

{{clear}}

{{Infobox hurricane small

| Basin = EPac

| Formed = November 1

| Dissipated = November 4

| Image = Sonia Nov 3 2013 1810Z.jpg

| Track = Sonia 2013 track.png

| 1-min winds = 40

| Pressure = 1002

}}

{{Main|Tropical Storm Sonia (2013)}}

A strong upward pulse of the Madden–Julian oscillation pushed across the East Pacific during the last week of October, yielding the formation of a broad area of low pressure. A tropical wave passed through this gyre late on October 26, leading to the formation of disorganized convection. After several days of consolidation, the disturbance acquired sufficient organization to be declared a tropical depression by 06:00 UTC on November 1. Gradually recurving northeast in response to a series of troughs to the system's north, the cyclone only slowly organized under moderate wind shear, and the depression intensified into Tropical Storm Sonia by 00:00 UTC on November 3. After reaching peak winds of {{convert|45|mph|km/h|abbr=on|round=5}} later that afternoon, an additional increase in upper-level winds caused the cyclone to weaken to minimum tropical storm intensity as it made landfall near El Dorado, Mexico early on November 4. Sonia weakened rapidly once inland, becoming a tropical depression at 06:00 UTC and dissipating over the Sierra Madre Occidental mountain range six hours later.{{cite report|author=Todd B. Kimberlain|title=Tropical Cyclone Report: Tropical Storm Sonia|url={{NHC TCR url|id=EP182013_Sonia}}|publisher=National Oceanic and Atmospheric Administration|work=National Hurricane Center|date=January 8, 2013|access-date=January 11, 2015|location=Miami, Florida|format=PDF}}

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{{Tropical cyclone naming}}

The following list of names was used for named storms that formed in the North Pacific Ocean east of 140°W during 2013.{{cite web|archive-url=https://web.archive.org/web/20130430134031/http://www.nhc.noaa.gov/aboutnames.shtml |url=http://www.nhc.noaa.gov/aboutnames.shtml |title=Tropical Cyclone Names |location=Miami, Florida |publisher=National Hurricane Center |date=April 4, 2013 |archive-date=April 30, 2013 |access-date=May 8, 2013 |url-status=dead }} This is the same list used for the 2007 season.{{cite report|title=Regional Association IV (North America, Central America and the Caribbean) Hurricane Operational Plan|work=Tropical Cyclone Programme|year=2007|page=9{{hyphen}}2|url=https://www.preventionweb.net/files/5593_RAIVHurricaneOperationalPlan.pdf|publisher=World Meteorological Organization|location=Geneva, Switzerland|access-date=March 7, 2024}}

For storms that form in the North Pacific between 140°W to the International Date Line, the names come from a series of four rotating lists. Names are used one after the other without regard to year, and when the bottom of one list is reached, the next named storm receives the name at the top of the next list. Two named storms, listed below, formed within the area in 2013. Also, named storms in the table above that crossed into the area during the season are noted (*).{{cite report|last=Evans|first=Tom|title=Review of the 2013 Central Pacific Tropical Cyclone Season and Preliminary Verification|url=https://www.icams-portal.gov/meetings/TCORF/ihc14/presentations/Session1/s01-01Evans.pdf|publisher=Central Pacific Hurricane Center|location=Honolulu, Hawaii|access-date=January 28, 2024}}

{{see also|List of retired Pacific hurricane names}}

On April 10, 2014, at the 36th session of the RA IV hurricane committee, the World Meteorological Organization retired the name Manuel due to the damage and deaths it caused, and the name will not be used for another eastern North Pacific tropical storm or hurricane. Manuel was replaced with Mario for the 2019 season.{{#tag:ref|On April 10, 2014, the World Meteorological Organization also retired the name Ingrid from its rotating Atlantic name lists.|group="nb"}}{{cite news|url=https://www.noaa.gov/wmo-retires-ingrid-and-manuel-atlantic-and-eastern-north-pacific-basins|title=WMO retires Ingrid and Manuel for Atlantic and eastern North Pacific basins|date=April 10, 2014|publisher=National Oceanic and Atmospheric Administration|access-date=March 7, 2024|location=Silver Spring, Maryland}}

This is a table of all of the tropical cyclones that formed in the 2013 Pacific hurricane season. It includes their name, duration (within the basin), peak classification and intensities, areas affected, damage, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all of the damage figures are in 2013 USD.

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{{Portal|Tropical cyclones}}

• Tropical cyclones in 2013
• 2013 Atlantic hurricane season
• 2013 Pacific typhoon season
• 2013 North Indian Ocean cyclone season
• South-West Indian Ocean cyclone seasons: 2012–13, 2013–14
• Australian region cyclone seasons: 2012–13, 2013–14
• South Pacific cyclone seasons: 2012–13, 2013–14

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{{Commons category}}

• [http://www.nhc.noaa.gov National Hurricane Center Website]
• [https://web.archive.org/web/20120822015000/http://www.smn.cna.gob.mx/ Servicio Meteorológico Nacional Website] {{in lang|es}}
• [https://www.nhc.noaa.gov/data/tcr/index.php?season=2013&basin=epac NHC 2013 Pacific hurricane season archive]

{{Lowest ACE Pacific hurricane seasons}}

{{2013 Pacific hurricane season buttons}}

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

{{Tropical cyclone season|2013}}

Category:Pacific hurricane seasons

2013 Epac