411 REFERENCE · Wikipedia
2007 Pacific hurricane season
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Hurricane Flossie (2007) 2007 Pacific hurricane season Hurricane Flossie (2007) October 2026
EPac
2007
2007 Pacific hurricane season summary.png
May 27, 2007
October 23, 2007
Flossie
949
120
1
15
11
4
1
42 total
81.08
52.6
2005, 2006, 2007, 2008, 2009
2007 Atlantic hurricane season
2007 Pacific typhoon season
2007 North Indian Ocean cyclone season
The 2007 Pacific hurricane season was a well below-average Pacific hurricane season, featuring only one major hurricane. The season officially started on May 15 in the eastern Pacific and on June 1 in the central Pacific, and ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in the region. The first tropical cyclone of the season, Alvin, developed on May 27, while the final system of the year, Kiko, dissipated on October 23. Due to unusually strong wind shear, activity fell short of the long-term average, with a total of 11 named storms, 4 hurricanes, and 1 major hurricane. At the time, 2007 featured the second-lowest value of the Accumulated cyclone energy (ACE) index since reliable records began in 1971. Two tropical cyclones – Cosme and Flossie – crossed into the central Pacific basin during the year, activity below the average of 4 to 5 systems.
Impact during the season was relatively minimal. In early June, Tropical Storm Barbara moved ashore just northwest of the Mexico–Guatemala border, causing $55 million (2007 USD)All damage totals are in 2007 USD unless otherwise stated. "nb" in damage and 4 deaths. In late July, Cosme passed south of the island of Hawaii as a weakening tropical depression; light rain and increased surf resulted. A few days later, Dalila passed offshore the coastline of southwestern Mexico, killing 11 and causing minimal damage. Hurricane Flossie followed a similar track to Cosme in mid-August, producing gusty winds and light precipitation in Hawaii. Hurricane Henriette in early September produced torrential rainfall in southwestern Mexico, killing 6 and causing $25 million in damage. Baja California received moderate rains from Hurricane Ivo in mid-September, though no damage nor fatalities were reported. In mid-October, Tropical Storm Kiko passed just offshore the coastline of southwestern Mexico. Though no deaths were reported on the Mexico mainland, the storm capsized a ship with 30 people on board, 15 of whom were recovered dead, and 9 of whom were reported missing. Overall, the season ended with $80 million in damage and 49 deaths.
Seasonal forecasts
+Predictions of tropical activity in the 2007 seasonSourceDateNamedstormsHurricanesMajorhurricanesRefAverage (1971–2006)15.38.84.2Record high activity2716 (tie)11Record low activity8 (tie)30† (tie)CPCMay 23, 200711-166-92-4Carmeyia Gillis NOAA Predicts Below Normal 2007 East Pacific Hurricane Season http://www.publicaffairs.noaa.gov/releases2007/may07/noaa07-r213.html National Oceanic and Atmospheric Administration Climate Prediction Center May 22, 2007 November 2, 2013 https://web.archive.org/web/20131106035756/http://www.publicaffairs.noaa.gov/releases2007/may07/noaa07-r213.html 2013-11-06 deadActual activity 1141
On May 21, 2007, the National Oceanic and Atmospheric Administration's Central Pacific Hurricane Center released its outlook for the 2007 Central Pacific hurricane season, predicting a total of 2–3 tropical cyclones to form or cross into the basin; in a typical season, 4–5 systems cross or form in the Central Pacific.Delores Clark NOAA Announces Central Pacific Hurricane Season Outlook http://www.publicaffairs.noaa.gov/releases2007/may07/noaa07-r212.html National Oceanic and Atmospheric Administration Central Pacific Hurricane Center May 21, 2007 November 2, 2013 https://web.archive.org/web/20131106035802/http://www.publicaffairs.noaa.gov/releases2007/may07/noaa07-r212.html 2013-11-06 dead A day later, the National Oceanic and Atmospheric Administration's Climate Prediction Center released its seasonal prediction for the 2007 East Pacific hurricane season, predicting a total of 11–16 named storms, 6–9 hurricanes, and 2–4 major hurricanes. Below-average activity was expected as a result of either ENSO-Neutral or La Niña conditions, as well as the continuation of the reduction in activity beginning in 1995.
Seasonal summary
The Accumulated Cyclone Energy (ACE) index for the 2007 Pacific hurricane season (Eastern Pacific and Central Pacific combined) as calculated by Colorado State University using data from the National Hurricane Center was 51.6 units,The total represents the sum of the squares of the maximum sustained wind speed (knots) for every (sub)tropical storm's intensity of over 33 kn mph km/h, divided by 10,000 while they are above that threshold; therefore, tropical depressions are not included. "nb"Basin Archives: Northeast Pacific Ocean Historical Tropical Cyclone Statistics http://tropical.atmos.colostate.edu/Realtime/index.php?arch&loc=northeastpacific Colorado State University Fort Collins, Colorado July 8, 2022 which was a well below the 1981–2010 average of 113.3 units, and at the time the second-lowest value observed since reliable records began in 1971.Hurricane Specialist Unit Monthly Tropical Weather Summary: November http://www.nhc.noaa.gov/archive/2007/tws/MIATWSEP_nov.shtml National Oceanic and Atmospheric Administration National Hurricane Center November 30, 2007 November 2, 2013 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 39 mph km/h on.
Tropical cyclone activity totaled to eleven named storms, four hurricanes, and only major hurricane within the season; all three of these values fall below the 1971–2006 long-term average of 15 named storms, 9 hurricanes, and 4 major hurricanes. The main contributing factor to below-average activity was much above-average wind shear across the Pacific basin.Lixion A. Avila Jamie R. Rhome Eastern North Pacific Hurricane Season of 2007 137 10.1175/2009MWR2915.1 National Hurricane Center 8 2436 American Meteorological Society February 10, 2009 2009MWRv..137.2436A 121578587 https://zenodo.org/record/1234539 free In May 2007, two tropical storms – Alvin and Barbara – developed, marking at the time the third such instance of more than one tropical storm developing within the month since official records began in 1949.Hurricane Specialist Unit Monthly Tropical Weather Summary: May http://www.nhc.noaa.gov/archive/2007/tws/MIATWSEP_may.shtml National Oceanic and Atmospheric Administration National Hurricane Center June 1, 2007 November 2, 2013 In June 2007, only one tropical depression developed in the East Pacific basin, making 2007 one of only four years in which a tropical storm did not form in the month.Hurricane Specialist Unit Monthly Tropical Weather Summary: June http://www.nhc.noaa.gov/archive/2007/tws/MIATWSEP_jun.shtml National Oceanic and Atmospheric Administration National Hurricane Center July 1, 2007 November 2, 2013 By the following month, in terms of ACE, 2007 was considered the third quietest year-to-date since the satellite era began in 1966;Hurricane Specialist Unit Monthly Tropical Weather Summary: June http://www.nhc.noaa.gov/archive/2007/tws/MIATWSEP_jul.shtml National Oceanic and Atmospheric Administration National Hurricane Center August 1, 2007 November 2, 2013 in September, the season fell to the second quietest year-to-date.Hurricane Specialist Unit Monthly Tropical Weather Summary: June http://www.nhc.noaa.gov/archive/2007/tws/MIATWSEP_sep.shtml National Oceanic and Atmospheric Administration National Hurricane Center October 1, 2007 November 2, 2013 Below-average activity continued for the remainder of the year.
Systems
Tropical Storm Alvin
EPac
Alvin 2007-05-29 1802Z.jpg
Alvin 2007 path.png
May 27
May 31
35
1003
The genesis of Alvin can be attributed to a tropical wave that crossed Dakar, Africa on May 9. The wave remained poorly organized as it moved across the Atlantic Ocean and Caribbean Sea through mid-May. On May 20, the disturbance crossed Central America and emerged into the eastern Pacific Ocean, where convection—shower and thunderstorm activity—gradually began to increase over the well-defined center; this led to the formation of a tropical depression by 0000 UTC on May 27, approximately 345 mi km on south of the southern tip of Baja California. Following designation, the depression was slow to organize as a result of moderate easterly shear; by 0000 UTC on May 29, however, the system had gained enough organization to be considered a tropical storm. After attaining its peak intensity with winds of 40 mph km/h on and a minimum barometric pressure of 1003 mbar hPa inHg on off, increasingly stable air and higher wind shear caused Alvin to begin a weakening trend. At 0600 UTC on May 30, it weakened to a tropical depression, and by 0000 UTC on June 1, Alvin degenerated into a non-convective remnant low. The remnant low continued generally westward until dissipation six days later.Lixion A. Avila Tropical Cyclone Report: Tropical Storm Alvin EP012007_Alvin National Oceanic and Atmospheric Administration National Hurricane Center October 2, 2007 October 28, 2013 PDF
Tropical Storm Barbara
Tropical Storm Barbara (2007)
EPac
Barbara 2007-06-01 1655Z.jpg
Barbara 2007 path.png
May 29
June 2
45
1000
A tropical wave emerged off the western coast of Africa on May 14. After emerging into the eastern Pacific on May 25, the system acquired enough organization to be considered a tropical depression at 1800 UTC on May 29, about 115 mi km on south-southeast of Puerto Escondido, Oaxaca.Richard D. Knabb Tropical Cyclone Report: Tropical Storm Barbara EP022007_Barbara National Oceanic and Atmospheric Administration National Hurricane Center August 21, 2007 October 28, 2013 PDF Within an environment of weak steering currents, the storm became better organized as evidenced by an improving satellite appearance, with the formation of a curved band in the southeast quadrant.James L. Franklin Tropical Storm Barbara Discussion Number 4 http://www.nhc.noaa.gov/archive/2007/ep02/ep022007.discus.004.shtml National Oceanic and Atmospheric Administration National Hurricane Center May 30, 2007 October 28, 2013 At 1200 UTC on May 30, the depression was upgraded to a tropical storm; by 0000 UTC on June 1, however, increased northerly wind shear caused Barbara to weaken back to a tropical depression. After re-intensifying into a tropical storm for a second time six hours later, Barbara attained its peak intensity with winds of 50 mph km/h on and a minimum barometric pressure of 1000 mbar hPa inHg on off at 1800 UTC. Drifting northeast, the storm maintained this intensity until landfall just northwest of the Mexico-Guatemala border at 1300 UTC on June 2. Rapid weakening ensued thereafter, with the system weakening to a tropical depression at 1800 UTC. The low-level circulation dissipated six hours later, marking the dissipation of Barbara.
Heavy rainfall exceeding 4 in mm on caused many rivers to swell.Alberto Unzón Cirilo Lujano 2007 Reseña de la Tormenta Tropical "Barbara" del Océano Pacífico http://smn.cna.gob.mx/ciclones/tempo2007/pacifico/barbara/barbara.pdf Servicio Meteorológico Nacional October 30, 2013 dead https://web.archive.org/web/20070625121641/http://smn.cna.gob.mx/ciclones/tempo2007/pacifico/barbara/barbara.pdf June 25, 2007 An unspecified island was separated from the Mexico mainland after the bridge connecting the two was washed away, stranding dozens of families.Mica Rosenberg Tropical storm lashes Guatemala, Mexico coasts http://uk.reuters.com/article/homepageCrisis/idUKN02390123._CH_.242020070602 https://web.archive.org/web/20070606155023/http://uk.reuters.com/article/homepageCrisis/idUKN02390123._CH_.242020070602 dead June 6, 2007 Reuters June 2, 2007 October 30, 2013 In El Salvador, significant flooding killed four people.Heavy rain leaves 12 dead in Caribbean, Central America http://www.sauress.com/en/spaen/455075 Saudi Press Agency June 1, 2007 October 30, 2013 Gusts peaked at 58 mph km/h on at an automated weather station in Puerto Madero, Chiapas.Daniel P. Brown Lixion A. Avila Tropical Storm Barbara Discussion Number 16 http://www.nhc.noaa.gov/archive/2007/ep02/ep022007.discus.016.shtml National Oceanic and Atmospheric Administration National Hurricane Center June 2, 2007 October 30, 2013 Across the affected regions, these winds caused damage limited to house roofs and trees. Barbara caused severe crop damage totaling to 200 million pesos (2007 MXN; $55 million).Destruye tormenta tropical más de 9 mil hectáreas de plátano http://www.teorema.com.mx/articulos.php?id_sec=47&id_art=4064&id_ejemplar=0 2007-09-30 https://web.archive.org/web/20070930065751/http://www.teorema.com.mx/articulos.php?id_sec=47&id_art=4064&id_ejemplar=0 Teorema Ambiental June 26, 2007 October 30, 2013 es About a hundred residents were forced to evacuate after the storm destroyed a dozen palm huts in Guatemala.
Tropical Depression Three-E
EPac
03E 2007-06-12 1815Z.jpg
03E 2007 path.png
June 11
June 12
30
1004
On May 24, a tropical wave emerged off the western coast of Africa. The wave entered the eastern Pacific around June 6 and shower and thunderstorm activity began to increase shortly thereafter. A broad area of low pressure formed a few hundred miles south of Acapulco, Mexico two days later.James L. Franklin Tropical Cyclone Report: Tropical Depression Three-E EP032007_Three-E National Oceanic and Atmospheric Administration National Hurricane Center July 12, 2007 October 28, 2013 Following satellite evidence of a well-defined circulation and organized convective activity,Michelle Mainelli Tropical Depression Three-E Discussion Number 1 http://www.nhc.noaa.gov/archive/2007/ep03/ep032007.discus.001.shtml National Oceanic and Atmospheric Administration National Hurricane Center June 11, 2007 October 28, 2013 the National Hurricane Center upgraded the disturbance to a tropical depression at 1200 UTC on June 11. After attaining winds of 35 mph km/h on and a minimum barometric pressure of 1004 mbar hPa inHg on off, the depression began to traverse cooler waters and much more stable air. This caused all associated convection to fade away, and the depression degenerated to a non-convective remnant low at 0000 UTC on June 13. The remnant low continued northwest until dissipation by 0600 UTC on June 15.
Tropical Depression Four-E
EPac
04E 2007-07-09 2105Z.jpg
04E 2007 path.png
July 9
July 11
30
1006
A tropical wave emerged off the western coast of Africa on June 23. It reached the eastern Pacific on July 3, where associated convection began to increase three days later. Continued slow development occurred thereafter, and following satellite trends, the disturbance was upgraded to Tropical Depression Four-E at 1800 UTC on July 9. Tracking westward, the depression began to move across waters too cool to support a tropical cyclone and into an environment of moderate shear.Jack L. Beven II Tropical Cyclone Report: Tropical Depression Four-E EP042007_Four-E National Oceanic and Atmospheric Administration National Hurricane Center August 28, 2007 October 29, 2013 PDF The low-level circulation became ill-defined and exposed,Michelle Mainelli Tropical Depression Four-E Discussion Number 5 http://www.nhc.noaa.gov/archive/2007/ep04/ep042007.discus.005.shtml National Oceanic and Atmospheric Administration National Hurricane Center July 10, 2007 October 29, 2013 leading to degeneration to a remnant low at 0600 UTC on July 11 about 910 mi km on west-southwest of Cabo San Lucas, Mexico. The low continued northwest until dissipation at 0000 UTC the following day.
Tropical Depression Five-E
EPac
05E 2007-07-14 1815Z.jpg
05E 2007 path.png
July 14
July 15
30
1006
On June 21, a tropical wave emerged off the western coast of Africa. It entered the eastern Pacific on July 10, and shower and thunderstorm activity began to increase a day later as a result. Tracking westward, the wave gradually became better organized; by 1200 UTC on July 14, the disturbance acquired enough organization to be upgraded to a tropical depression.Jamie R. Rhome Tropical Cyclone Report: Tropical Depression Five-E EP052007_Five-E National Oceanic and Atmospheric Administration National Hurricane Center July 17, 2007 October 29, 2013 PDF Within an environment of moderate wind shear, the low-level center quickly became poorly defined as convection dissipated.David P. Roberts Jack L. Beven II Tropical Depression Five-E Discussion Number 7 http://www.nhc.noaa.gov/archive/2007/ep05/ep052007.discus.007.shtml National Oceanic and Atmospheric Administration National Hurricane Center July 15, 2007 October 29, 2013 Turning west-northwest on July 15, the depression entered cooler waters and an increasingly stable airmass, causing the system to degenerate into a remnant low by 0000 UTC the following day. The remnant low dissipated a few hours later.
Hurricane Cosme
EPac
Cosme 2007-07-16 1935Z.jpg
Cosme 2007 path.png
July 14
July 22
65
987
A tropical wave emerged off the western coast of Africa on June 27 and tracked westward to reach the eastern Pacific on July 8. Initially embedded within the ITCZ, development was slow until the system's convection increased on July 13. A day later, the NHC classified it as Tropical Depression Six-E about midway between Mexico and Hawaii. Although wind shear was light, ocean temperatures were marginal for intensification, and the depression intensified into Tropical Storm Cosme on July 15, while moving generally northwestward.Michelle Mainelli Tropical Cyclone Report: Hurricane Cosme EP062007_Cosme National Oceanic and Atmospheric Administration National Hurricane Center December 17, 2007 October 30, 2013 PDFLixion Avila Tropical Depression Six-E Discussion Number 1 2007 National Hurricane Center 2008-04-15 http://www.nhc.noaa.gov/archive/2007/ep06/ep062007.discus.001.shtml? Following the development of a curved convection band and appearance of an eye on satellite,Michelle Mainelli Hurricane Cosme Discussion Number 10 http://www.nhc.noaa.gov/archive/2007/ep06/ep062007.discus.010.shtml National Oceanic and Atmospheric Administration National Hurricane Center July 16, 2007 October 30, 2013 Cosme was upgraded to a Category 1 hurricane at 1800 UTC the next day, about 1600 mi km on east of Hilo, Hawaii; it is at this time that the hurricane attained its peak with winds of 75 mph km/h on and a minimum barometric pressure of 987 mbar hPa inHg on. Cosme tracked westward over cooler waters, causing the system to weaken quickly back to tropical storm strength. At 1800 UTC on July 18, Cosme weakened to a tropical depression after crossing into the central Pacific. Gradually weakening, Tropical Depression Cosme passed south of the Hawaiian Islands on July 20 with a minimum central pressure of 1010 mbar.Ballard Tropical Depression Cosme Advisory Number 27 2007 Central Pacific Hurricane Center 2008-04-15 http://www.prh.noaa.gov/cphc/tcpages/archive/2007/TCPCP1.EP062007.27.0707210244 By late on July 22, Cosme degenerated into a remnant low near Johnston Island. The circulation dissipated three days later.Houston Tropical Depression Cosme Discussion Number 33 2007 Central Pacific Hurricane Center 2008-04-15 http://www.prh.noaa.gov/cphc/tcpages/archive/2007/TCPCP1.EP062007.33.0707221445
Cosme was initially forecast to pass over Hawaii at tropical storm strength.James L. Franklin Tropical Storm Cosme Discussion Number 12 http://www.nhc.noaa.gov/archive/2007/ep06/ep062007.discus.012.shtml National Oceanic and Atmospheric Administration National Hurricane Center July 17, 2007 October 30, 2013Michelle Mainelli Tropical Storm Cosme Discussion Number 13 http://www.nhc.noaa.gov/archive/2007/ep06/ep062007.discus.013.shtml National Oceanic and Atmospheric Administration National Hurricane Center July 17, 2007 October 30, 2013 In anticipation of the storm, the National Weather Service issued a flash flood watch for the island of Hawaii on July 20, and a small craft advisory and high surf advisory for Maui and Hawaii.CBS News CBS News Hawaii Braces For A Tropical Depression 2008-04-15 https://www.cbsnews.com/news/hawaii-braces-for-a-tropical-depression/ 2007-07-20 The Hawaii County Civil Defense opened evacuation centers,Laurie Au Storm set to weaken but could pose threat 2007 Honolulu Star-Bulletin 2008-04-15 http://starbulletin.com/2007/07/17/news/story01.html 2008-07-24 https://web.archive.org/web/20080724234447/http://starbulletin.com/2007/07/17/news/story01.html dead while county crews cleaned out drains and culverts to prevent flooding.Jan TenBruggencate Tropical depression dumps heavy rain on Hawaii USA Today 2008-04-15 https://www.usatoday.com/weather/hurricane/2007-07-20-cosme-hawaii_N.htm 2007-07-22 Because the depression stayed far from land, the effects were mostly minor. Rain bands produced 6.94 in mm on on of rainfall in Hakalau,Kevin R. Kodama July 2007 Precipitation Summary 2007 National Weather Service 2008-04-15 http://www.prh.noaa.gov/hnl/hydro/pages/jul07sum.php https://web.archive.org/web/20070613043117/http://www.prh.noaa.gov/hnl/hydro/pages/jul07sum.php 2007-06-13 causing small stream and drainage ditch flooding, as well as ponding on roadways in portions of Hilo, Puna, and Kau.National Climatic Data Center Event report for Tropical Depression Cosme (2) 2007 2008-04-15 http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~675476August 2026 InternetArchiveBot The rainfall helped to relieve a persistent drought which had existed for several months. Wind gusts reached 40 mph km/h on in southern portions of Hawaii.Associated Press Tropical depression hits Hawaii's Big Island NBC News February 5, 2024 https://www.nbcnews.com/id/wbna19888664 July 21, 2007 A strong trade wind swell north of Cosme generated waves up to 9 ft m on high.National Climatic Data Center National Climatic Data Center Event report for Tropical Depression Cosme 2007 2008-04-15 http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~673779August 2026 InternetArchiveBot
Tropical Storm Dalila
Tropical Storm Dalila (2007)
EPac
Dalila 2007-07-25 2100Z.jpg
Dalila 2007 path.png
July 22
July 27
50
995
A tropical wave emerged into the eastern Pacific on July 17. Tracking west-northwest, the system acquired enough organization to be upgraded to a tropical depression at 0000 UTC on July 22, while positioned 460 mi km on south of Manzanillo, Mexico. Following formation, moderate northeasterly shear inhibited significant development, causing the system to remain a tropical depression for 48 hours. A mid-level ridge over Mexico caused the system to turn northwest as shear began to decrease; at 0000 UTC on July 24, the depression was upgraded to Tropical Storm Dalila. After attaining its peak intensity with winds of 60 mph km/h on and a minimum barometric pressure of 995 mbar hPa inHg on a day later, the storm tracked over progressively cool waters, causing it to weaken. At 0600 UTC on July 27, Dalila weakened to a tropical storm, and by 1800 UTC, the system no longer retained enough organization to be considered a tropical cyclone. The remnant low tracked west, southwest, and eventually south prior to dissipation at 1200 UTC on July 30.Daniel P. Brown Tropical Cyclone Report: Tropical Storm Dalila EP072007_Dalila National Oceanic and Atmospheric Administration National Hurricane Center August 29, 2007 October 29, 2013 PDF
Though the center of the storm remained offshore, outer rainbands led to heavy rainfall that triggered substantial flooding. In Michoacán, Dalila flooded ten municipalities with at least 15 in mm on of precipitation, destroying dozens of wooden structures.'Dalila' deja 200 damnificados e inundaciones en Michoacán http://www.esmas.com/noticierostelevisa/mexico/647532.html Noticieros Televisa July 24, 2007 October 29, 2013 es dead https://web.archive.org/web/20120925004143/http://www.esmas.com/noticierostelevisa/mexico/647532.html September 25, 2012 Heavy rains in Jalisco killed eleven, many of whom occurred in automobile crashes.Ulises Gutierrez Gerardo Flores Se descarrila por lluvias tren en Sonora; 4 muertos http://www.jornada.unam.mx/2007/07/25/index.php?section=estados&article=040n1est La Jornada July 25, 2007 October 29, 2013 esTormenta Tropical Dalila http://www.semarnat.gob.mx/saladeprensa/sistesisdeprensanacional/Pages/Sintesis24dejulio2007.aspx Semarnat July 24, 2007 October 29, 2013 es https://archive.today/20071231222658/http://www.semarnat.gob.mx/saladeprensa/sistesisdeprensanacional/Pages/Sintesis24dejulio2007.aspx 2007-12-31 dead Flood waters covered numerous roads, causing many accidents, while approximately 50 homes were damaged.Juan Partida Rene Ramon Rene Lopez Provocan aguaceros seis muertes en Guadalajara http://www.jornada.unam.mx/2007/07/24/index.php?section=estados&article=029n1est La Jornada July 24, 2007 October 29, 2013 es Rough seas and heavy rain affected Baja California Sur, though no damage or fatalities were reported.Weakened Tropical Storm Dalila dumps rain, kicks up surf along Mexico's coast http://www1.whdh.com/news/articles/world/BO58458 WHDH TV Associated Press July 26, 2007 October 29, 2013 https://archive.today/20131104103143/http://www1.whdh.com/news/articles/world/BO58458 2013-11-04 dead
Tropical Storm Erick
EPac
Erick 2007-07-31 2200Z.jpg
Erick 2007 path.png
July 31
August 2
35
1004
A tropical wave emerged off the western coast of Africa on July 16. Tracking westward, intermittent bursts of deep convection occurred as it crossed the Leeward Islands on July 22, but associated activity remained disorganized. The wave crossed Central America three days later, emerging into the eastern Pacific Ocean shortly thereafter. On July 28, a broad area of low pressure formed along the wave axis; easterly shear, however, prevented thunderstorms from developing over the center. Convective activity increased by July 31, leading to the formation of a tropical depression at 1200 UTC that day.Eric S. Blake Tropical Cyclone Report: Tropical Storm Erick EP082007_Erick National Oceanic and Atmospheric Administration National Hurricane Center August 23, 2007 October 29, 2013 PDF Despite the unfavorable environment, satellite intensity estimates increased to tropical storm intensity, prompting the National Hurricane Center to upgrade the depression to such.Lixion A. Avila Tropical Storm Erick Discussion Number 2 http://www.nhc.noaa.gov/archive/2007/ep08/ep082007.discus.002.shtml National Oceanic and Atmospheric Administration National Hurricane Center July 31, 2007 October 29, 2013 After attained a peak intensity with winds of 40 mph km/h on and a minimum barometric pressure of 1004 mbar hPa inHg on off at 0600 UTC on August 1, continued wind shear caused Erick to weaken to a tropical depression. The low-level center became lost organization as it became elongated northeast to southwest on August 2, leading to degeneration into a tropical wave by 06:00 UTC. The remnants of the system dissipated six hours later.
Hurricane Flossie
Hurricane Flossie (2007)
EPac
Flossie 11 aug 2007 2015Z.jpg
Flossie 2007 path.png
August 8
August 16
120
949
An ill-defined tropical wave entered the eastern Pacific on August 1 and steadily organized to attain tropical depression intensity eight days later. Within an environment of light shear, the depression intensified into Tropical Storm Flossie at 0000 UTC on August 9 and continued to organize to attain Category 1 hurricane intensity by 1200 UTC the following day as an eye became apparent on satellite. Continuing westward and crossing into the central Pacific basin, the system began a period of rapid intensification that brought it to its peak intensity with winds of 140 mph km/h on and a minimum barometric pressure of 949 mbar hPa inHg on at 0000 UTC on September 12, while positioned roughly 980 mi km on east-southeast of the Big Island. Increased wind shear the next day caused Flossie to begin a slow weakening trend thereafter; at 1200 UTC on September 14, the system weakened to a Category 2 hurricane, and by 0600 UTC on September 15, the cyclone was barely a Category 1 hurricane. Six hours later, it weakened to a tropical storm as the low-level center became exposed on satellite. Flossie weakened to a tropical depression early on September 16 and dissipated by 1800 UTC.Richard J. Pasch David P. Roberts Tropical Cyclone Report: Hurricane Flossie EP092007_Flossie National Oceanic and Atmospheric Administration National Hurricane Center January 10, 2008 October 30, 2013 PDF
In preparation for the cyclone, the Central Pacific Hurricane Center issued a hurricane watch for the Big Island.Sam Houston Hurricane Flossie Discussion Number 20 http://www.prh.noaa.gov/cphc/tcpages/archive/2007/TCDCP2.EP092007.20.0708131530 National Oceanic and Atmospheric Administration Central Pacific Hurricane Center August 13, 2007 November 11, 2013 A tropical storm warning was subsequently issued for the same location,Jeff Powell Hurricane Flossie Discussion Number 21 http://www.prh.noaa.gov/cphc/tcpages/archive/2007/TCDCP2.EP092007.21.0708132045 National Oceanic and Atmospheric Administration Central Pacific Hurricane Center August 13, 2007 November 11, 2013 The Federal Emergency Management Agency (FEMA) sent 20 transportation, public works, and health experts to the region.Flossie downgraded again after swiping Hawaii https://www.nbcnews.com/id/wbna20228092 NBC News Associated Press August 15, 2007 November 11, 2013 Many schools were closed, including the University of Hawaii at Hilo and Hawaii Community College; as a result, an estimated 26,000 college students were sent home.Storm shelter, closure information http://www.kitv.com/weather/hurricanes/whats-closed-ahead-of-flossie/-/9327530/21216070/-/8m79wb/-/index.html KITV News July 29, 2007 November 11, 2013 dead https://web.archive.org/web/20131112035732/http://www.kitv.com/weather/hurricanes/whats-closed-ahead-of-flossie/-/9327530/21216070/-/8m79wb/-/index.html November 12, 2013 As a weakening cyclone, Flossie produced light precipitation on the island of Hawaii. Large waves impacted south-facing beaches while the maximum sustained wind observed reached 39 mph km/h on at South Point.Tim Craig Sam Houston Wes Browning 2007 Tropical Cyclones Central North Pacific National Oceanic and Atmospheric Administration Central Pacific Hurricane Center June 9, 2019 https://www.nhc.noaa.gov/data/tcr/CP2007_Seasonal_TCR.pdf No fatalities were reported.
Tropical Storm Gil
EPac
Gil 2007-08-30 2040Z.jpg
Gil 2007 path.png
August 29
September 2
40
1001
A vigorous tropical wave emerged off the western coast of Africa on August 16. Characterized with abundant deep convection, the wave remained organization until it interacted with an upper-level trough across the eastern Caribbean Sea a few days later. On August 26, the wave split in two, with the northern portion leading the formation of a weak low in the Bay of Campeche and the southern portion continuing westward into the eastern Pacific. After the formation of deep convection over the center and associated convective bands, the disturbance was upgraded to a tropical depression at 1200 UTC on August 29.Lixion A. Avila Tropical Cyclone Report: Tropical Storm Gil EP102007_Gil National Oceanic and Atmospheric Administration National Hurricane Center October 10, 2007 October 29, 2013 Though the circulation remained positioned on the northeast side of most thunderstorm activity, satellite intensity estimates supported tropical storm strength and it was upgraded to such accordingly.Eric S. Blake Tropical Storm Gil Discussion Number 2 http://www.nhc.noaa.gov/archive/2007/ep10/ep102007.discus.002.shtml National Oceanic and Atmospheric Administration National Hurricane Center August 29, 2007 October 29, 2013 At 1200 UTC on August 30, Gil attained its peak intensity with winds of 45 mph km/h on and a minimum barometric pressure of 1001 mbar hPa inHg on off. Shortly thereafter, increasing wind shear and decreasing sea surface temperatures caused the system to steadily weaken; at 0000 UTC on September 1, the system deteriorated into a tropical depression, and by 1800 UTC the following afternoon, the system no longer displayed enough organization to be considered a cyclone. The remnant low continued westward and dissipated twelve hours later.
Although the storm never made landfall, heavy rainfall was reported in the Mexican states of Baja California Sur and Sinaloa. A total of 26 neighborhoods were flooded with up to 4.9 ft m on of water in the town of Culiacán, while a 14-year-old boy was swept away by a swollen river.Javier Martínez http://www.eluniversal.com.mx/notas/446021.html Deja tormenta tropical Gil primera víctima en Culiacán June 6, 2011 https://web.archive.org/web/20110606003626/http://www.eluniversal.com.mx/notas/446021.html August 30, 2007 El Universal November 11, 2013 es live At least 100 vehicles were stranded in sectors such as Las Quintas, the city center and Chapultepec, causing severe road congestion. The shuttle service had to be suspended for two hours. Dozens of families were evicted by Civil Protection personnel and municipal police.August 31, 2007 Aguaceros en Culiacán dejan un desaparecido - La Jornada https://www.jornada.com.mx/2007/08/31/index.php?section=estados&article=032n2est 2021-03-17 www.jornada.com.mx es
Hurricane Henriette
Hurricane Henriette (2007)
EPac
Henriette 04 sept 2007 1745Z.jpg
Henriette 2007 path.png
August 30
September 6
75
972
A poorly organized tropical wave moved into the eastern Pacific on August 29 and quickly developed into a tropical depression by 0600 UTC the following day. Within an environment of low wind shear, the depression intensified into a tropical storm, acquiring the name Henriette, at 1200 UTC on August 31. Moving west-northwest around a ridge positioned over inland Mexico, the center passed narrowly offshore after producing squally weather along the coastline. The system moved westward while continuing to intensify, becoming a Category 1 hurricane at 0600 UTC on September 4 and subsequently attaining its peak intensity with winds of 85 mph km/h on and a minimum barometric pressure of 972 mbar hPa inHg on six hours later. An approaching upper-level trough caused Henriette to turn northwest later that day, moving it ashore near San José del Cabo, Mexico at 2100 UTC as a minimal hurricane. After crossing Baja California Sur, Henriette weakened to a tropical storm and made a second landfall near Guaymas, Mexico. The system moved inland and quickly weakened, dissipating by 1200 UTC on September 6.Richard D. Knabb Tropical Cyclone Report: Hurricane Henriette EP112007_Henriette National Oceanic and Atmospheric Administration National Hurricane Center November 23, 2007 October 30, 2013 PDF
The hardest hit city by Henriette was Acapulco, where heavy rains led to rockslides and mudslides that killed six.Landslide kills six as storm passes Mexico http://www.abc.net.au/news/2007-09-02/landslide-kills-six-as-storm-passes-mexico/657172 ABC News Australia Agence France-Presse September 2, 2007 October 30, 2013 In Sonora, the hurricane damaged thousands of structures and killed four, two of whom off the coast.Carmen Duarte Sonora cleanup begins http://azstarnet.com/news/local/border/sonora-cleanup-begins/article_b542276b-6a17-56b6-b2b3-1a096ccf9793.html Arizona Daily Star September 7, 2007 October 30, 2013Frank Daniel Hurricane Henriette Pounds Mexico, 2 Reported Dead http://www.enn.com/top_stories/article/22764 Reuters Environmental News Network September 6, 2007 October 30, 2013 Farther northwest, a woman died while attempting to surf waves off the coast of Baja California Sur.Henriette threatens Mexican mainland https://www.nbcnews.com/id/wbna20602791 NBC News Associated Press September 5, 2007 October 30, 2013 Heavy rains stranded many cars while causing rivers to overflow, flooding communities.Azota "Henriette" al territorio nacional http://sipse.com/archivo/novedades-de-quintana-roo/azota-henriette-al-territorio-nacional-60813.html Sipse Notimex September 3, 2007 October 30, 2013 es https://archive.today/20131104103139/http://sipse.com/archivo/novedades-de-quintana-roo/azota-henriette-al-territorio-nacional-60813.html 2013-11-04 dead Damage totaled to $275 million (2007 MXN; $25 million).
Hurricane Ivo
EPac
Ivo 2007-09-20 2055Z.jpg
Ivo 2007 path.png
September 18
September 23
70
984
A tropical wave moved off the western coast of Africa on September 1 and continued westward until reaching the eastern Pacific fifteen days later. A broad area of low pressure formed along the wave axis on September 16 as convective activity organized, and by 0600 UTC on September 18, the system acquired enough organization to be declared a tropical depression.James L. Franklin Tropical Cyclone Report: Hurricane Ivo EP122007_Ivo National Oceanic and Atmospheric Administration National Hurricane Center December 3, 2007 October 30, 2013 PDF Convective bands began to form near the center a few hours later,Jack L. Beven II Tropical Depression Twelve-E Discussion Number 2 http://www.nhc.noaa.gov/archive/2007/ep12/ep122007.discus.002.shtml National Oceanic and Atmospheric Administration National Hurricane Center September 18, 2007 November 11, 2013 leading to an improved satellite presentation overall. Tracking west-northwestward as a result of the mid-level ridge,Lixion A. Avila Tropical Storm Ivo Discussion Number 1 http://www.nhc.noaa.gov/archive/2007/ep12/ep122007.discus.003.shtml National Oceanic and Atmospheric Administration National Hurricane Center September 18, 2007 November 11, 2013 the system intensified into Tropical Storm Ivo at 0000 UTC on September 19. Turning northwest, a well-defined eye became visible on satellite, prompting the NHC to upgrade the system to a Category 1 hurricane 24 hours later. With an area of deep convection near the center,Lixion A. Avila Hurricane Ivo Discussion Number 7 http://www.nhc.noaa.gov/archive/2007/ep12/ep122007.discus.007.shtml National Oceanic and Atmospheric Administration National Hurricane Center September 19, 2007 November 11, 2013 the hurricane attained its peak intensity with winds of 80 mph km/h on and a minimum barometric pressure of 984 mbar hPa inHg on at 0000 UTC on September 21. Westerly flow associated with a large upper-level low began to undercut the outflow of Ivo, and it weakened to a tropical storm by the afternoon hours. The convective pattern rapidly deteriorated due to southeasterly wind shear,Robbie J. Berg Eric S. Blake Tropical Storm Ivo Discussion Number 15 http://www.nhc.noaa.gov/archive/2007/ep12/ep122007.discus.015.shtml National Oceanic and Atmospheric Administration National Hurricane Center September 21, 2007 November 11, 2013 and despite a brief burst of convection,Jack L. Beven II Tropical Storm Ivo Discussion Number 16 http://www.nhc.noaa.gov/archive/2007/ep12/ep122007.discus.016.shtml National Oceanic and Atmospheric Administration National Hurricane Center September 22, 2007 November 11, 2013 the storm was downgraded to a tropical depression to the west-southwest of the southern tip of Baja California at 0000 UTC on September 23. Associated deep convection dissipated later that day as Ivo turned eastward, and the system degenerated into a remnant low accordingly. The remnant low dissipated two days later as it continued in the same direction.
Initially, some forecasts predicted the storm would strike the Baja California Peninsula as a tropical storm;Michelle Mainelli Hurricane Ivo Discussion Number 13 http://www.nhc.noaa.gov/archive/2007/ep12/ep122007.discus.013.shtml National Oceanic and Atmospheric Administration National Hurricane Center September 21, 2007 November 11, 2013 a tropical storm watch was briefly issued from Santa Fe to Cabo San Lucas accordingly. Over 100 shelters were opened in the municipalities of Los Cabos, La Paz and Comondú, respectively.Gladys Rodríguez Caen en BCS las primeras lluviaspor 'Ivo' http://www.eluniversal.com.mx/estados/66002.html El Universal September 23, 2007 November 11, 2013 es October 18, 2007 https://web.archive.org/web/20071018014330/http://eluniversal.com.mx/estados/66002.html dead In all, Ivo contributed to heavy rainfall across Baja California Sur; however, no damage was reported.
Tropical Depression Thirteen-E
EPac
13E 2007-09-19 2155Z.jpg
13E 2007 path.png
September 19
September 20
30
1007
A tropical wave emerged off the western coast of Africa on August 27 and reached the eastern Pacific on September 7. Tracking westward, little development occurred until September 18, when associated shower and thunderstorm activity began to increase. Following visible satellite trends, the National Hurricane Center deemed the disturbance organized enough to be declared a tropical depression at 0600 UTC on September 19, while located about 1,200 mi km on west-southwest of the southern tip of Baja California. In an environment of cool ocean temperatures and stable air, the depression failed to organize as it turned west-northwest.Jack L. Beven II Christopher W. Landsea Tropical Cyclone Report: Tropical Depression Thirteen-E EP132007_Thirteen-E National Oceanic and Atmospheric Administration National Hurricane Center October 17, 2007 October 29, 2013 PDF Associated deep convection dissipated,Christopher W. Landsea James L. Franklin Tropical Depression Thirteen-E Discussion Number 6 http://www.nhc.noaa.gov/archive/2007/ep13/ep132007.discus.006.shtml National Oceanic and Atmospheric Administration National Hurricane Center September 20, 2007 October 29, 2013 leading to degeneration into a remnant low by 0000 UTC on September 20. Performing a slow counter-clockwise loop, the remnant low dissipated five days later.
Tropical Storm Juliette
EPac
Juliette_2007-09-30_1825Z.jpg
Juliette 2007 path.png
September 29
October 2
50
997
The formation of Tropical Storm Juliette can be traced back to a tropical wave that emerged off the western coast of Africa on September 12. After interacting with a secondary wave over the central Atlantic a few days later, it entered the eastern Caribbean, becoming steadily better defined. Convective activity was enhanced as the wave passed into the West Caribbean on September 22 and it moved inland over Central American shortly thereafter. A broad area of low pressure formed along the wave axis on September 27 and convection steadily increased; around 0000 UTC on September 29, the system acquired enough organization to be declared a tropical depression. Twelve hours later, the system intensified into Tropical Storm Juliette. Turning northwest as a result of an upper-level trough, the system attained its peak with winds of 60 mph km/h on and a minimum barometric pressure of 997 mbar hPa inHg on at 1200 UTC on September 30. Strong wind shear began to affect the storm thereafter, causing it to steadily weaken to tropical depression strength by 0000 UTC on October 2. Twelve hours later, the system degenerated into a remnant low. The low meandered several hundred miles off the coast of Baja California before degenerating into a trough on October 5.Robbie J. Berg Jamie R. Rhome Tropical Cyclone Report: Tropical Storm Juliette EP142007_Juliette National Oceanic and Atmospheric Administration National Hurricane Center November 8, 2007 October 29, 2013 PDF
Tropical Storm Kiko
Tropical Storm Kiko (2007)
EPac
Kiko 2007-10-20 1800Z.jpg
Kiko 2007 path.png
October 15
October 23
60
991
A tropical wave exited the coast of Africa and moved westward across the Atlantic before entering the eastern Pacific on October 8. Despite strong easterly wind shear, the system acquired enough organization to be deemed a tropical depression at 0000 UTC on October 15. Within a broad cyclonic gyre, the system moved erratically, first drifting south then east-northeast and eventually northwest. Early on October 16, the system briefly intensified into a tropical storm as a convective band wrapped around the circulation, but continued strong shear caused associated convection to dissipate and the system weakened to a tropical depression by 1800 UTC. After intensifying back to a tropical storm the following day, a brief reprieve in harsh upper-level winds allowed Kiko to reach its peak intensity with winds of 70 mph km/h on and a minimum barometric pressure of 991 mbar hPa inHg on. An increase in southerly shear and entrance into a more stable airmass caused the system to weaken to a tropical depression at 0000 UTC on October 23; the system degenerated into a remnant low 24 hours later. The remnant low tracked west before turning north and eventually dissipated early on October 27.Michelle Mainelli Tropical Cyclone Report: Tropical Storm Kiko EP152007_Kiko National Oceanic and Atmospheric Administration National Hurricane Center November 18, 2007 October 30, 2013 PDF
Beginning early on October 18, Kiko was forecast to strike Mexico at tropical storm intensity and cyclone advisories were issued accordingly.Jack L. Beven II Tropical Storm Kiko Advisory Number 15 http://www.nhc.noaa.gov/archive/2007/ep15/ep152007.public.015.shtml National Oceanic and Atmospheric Administration National Hurricane Center October 18, 2007 October 30, 2013 However, a building mid-level ridge of high pressure over inland Mexico was then forecast to cause the center of circulation to pass just offshore.Eric S. Blake Lixion A. Avila Tropical Storm Kiko Discussion Number 17 http://www.nhc.noaa.gov/archive/2007/ep15/ep152007.discus.017.shtml National Oceanic and Atmospheric Administration National Hurricane Center October 18, 2007 October 30, 2013 Though no damage was reported in association with the cyclone, rough seas created by Kiko capsized a ship with thirty people on board; two were found still alive, fifteen bodies were recovered, and nine were reported missing.Fifteen people drown as boat capsizes near Mexico http://www.taipeitimes.com/News/world/archives/2007/10/22/2003384268 Taipei Times Agence France-Presse October 22, 2007 October 30, 2013 Kiko's remnants caused severe flash floods in California, damage totaling to $1.08 million.Storm Events Database - Search Results National Centers for Environmental Information https://www.ncdc.noaa.gov/stormevents/textsearch.jsp?q=Tropical+Storm+Kiko 2024-10-18 www.ncdc.noaa.gov
Storm names
The following list of names was used for named storms that formed in the eastern North Pacific, east of 140°W, in 2007.Regional Association IV (North America, Central America and the Caribbean) Hurricane Operational Plan Tropical Cyclone Programme 2007 92 https://www.preventionweb.net/files/5593_RAIVHurricaneOperationalPlan.pdf World Meteorological Organization Geneva, Switzerland January 30, 2024 This is the same list used in 2001 with the exception of Alvin, which replaced Adolph.https://www.aoml.noaa.gov/general/lib/lib1/nhclib/Publications/NatHurricaneOpsPlans/HOPs-P12-2002.pdf 38 NOAA Office of the Federal Coordinator for Meteorological Services and Supporting Research Washington, D.C. National Hurricane Operations Plan May 2002 January 30, 2024 The name Alvin was used for the first time this year. There were no names retired from this list following the season, thus it was used again for the 2013 season.National Hurricane Center Worldwide Tropical Cyclone Names 2008 National Oceanic and Atmospheric Administration August 4, 2008 http://www.nhc.noaa.gov/aboutnames.shtml https://web.archive.org/web/20080804225453/http://www.nhc.noaa.gov/aboutnames.shtml August 4, 2008 dead
Alvin
Barbara
Cosme*
Dalila
Erick
Flossie*
Gil
Henriette Ivo
Juliette
Kiko
Lorena
Manuel
Narda
Octave
Priscilla Raymond
Sonia
Tico
Velma
Wallis
Xina
York
Zelda
For named storms that form in the central North Pacific, between 140°W and 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. No named storms formed in the region in 2007. Named storms in the table above that crossed into the area during the season are noted (*).2007 Tropical Cyclones Central North Pacific Craig Tim Houston Sam Browning Wes https://www.nhc.noaa.gov/data/tcr/CP2007_Seasonal_TCR.pdf NOAA January 30, 2024
Season effects
The following table lists all of the storms that formed in the 2007 Pacific hurricane season. It includes their name, duration, 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 2007 USD.
center2007 Pacific hurricane
storm Alvin May 27–31 40 (65) 1003 None None None
storm Barbara May 29 – June 2 50 (85) 1000 Southwestern Mexico 55000000 $ 4
depression Three-E June 11–12 35 (55) 1004 None None None
depression Four-E July 9–11 35 (55) 1006 None None None
depression Five-E July 14–15 35 (55) 1006 None None None
cat1 Cosme July 14–22 75 (120) 987 Hawaii Minimal None
storm Dalila July 22–27 60 (95) 995 Baja California Peninsula, Western Mexico (Jalisco) Minimal 11
storm Erick July 31 – August 2 40 (65) 1004 None None None
cat4 Flossie August 8–16 140 (220) 949 Hawaii Minimal None
storm Gil August 29 – September 2 45 (75) 1001 Western Mexico Minimal 1
cat1 Henriette August 30 – September 6 85 (140) 972 Southwestern Mexico, Western Mexico, Baja California Peninsula, Northwestern Mexico (Sonora) 25000000 $ 11
cat1 Ivo September 18–23 80 (130) 984 Baja California Peninsula None None
depression Thirteen-E September 19–20 35 (55) 1007 None None None
storm Juliette September 29 – October 2 60 (95) 997 None None None
storm Kiko October 15–23 70 (110) 991 Western Mexico $1.08 million 15
15 May 27 – October 23 140 (220) 949 80000000 $ 42
See also
Tropical cyclones
Tropical cyclones in 2007
Pacific hurricane season
2007 Atlantic hurricane season
2007 Pacific typhoon season
2007 North Indian Ocean cyclone season
Australian region cyclone seasons: 2006–07, 2007–08
South Pacific cyclone seasons: 2006–07, 2007–08
South-West Indian Ocean cyclone seasons: 2006–07, 2007–08
Notes
nb
References
3
External links
NHC 2007 Pacific hurricane season archive
WPC 2007 Tropical Cyclone Rainfall pages
CPHC 2007 Pacific hurricane season archive
2000 Pacific hurricane
2007
Category:Pacific hurricane seasons
2007 EPac