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List Of Off-season Pacific Hurricanes
There have been 26 recorded tropical and subtropical cyclones in the North-eastern Pacific basin outside the official Pacific hurricane season. The National Hurricane Center (NHC) monitors the area from North America westward to 140°W, while the Central Pacific Hurricane Center is from 140°W to the International Date Line, north of the equator. The National Oceanic and Atmospheric Administration (NOAA) currently defines the season as starting May 15 in the eastern Pacific and June 1 for the central Pacific and ending on November 30 for both regions in each calendar year. Occasionally, however, storms develop in late November and persist until December, such as Hurricane Nina of 1957. Few off-season tropical cyclones in the east Pacific have affected land, and none of them have made landfall. Only Hurricane Nina caused both property damage and fatalities. The strongest hurricane between December and May was Hurricane Ekeka in 1992, which reached winds of ...
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1992 Pacific Hurricane Season
The 1992 Pacific hurricane season is the most active Pacific hurricane season on record, featuring 27 named storms, and the second-costliest Pacific hurricane season in history, behind the 2013 season. The season also produced the second-highest ACE value on record in the basin, only surpassed by the 2018 season. The season officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. However, these bounds were easily exceeded when Hurricane Ekeka formed on January 28 and again a couple months later with Tropical Storm Hali. The most notable storm was Hurricane Iniki, which caused billions of dollars of damage to the Hawaiian Islands, primarily in Kauai, along with six casualties. Hurricanes Lester, Virgil, Winifred, and Orlene also made landfall and killed several people, but were significan ...
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1922 Pacific Hurricane Season
Nineteen or 19 may refer to: * 19 (number), the natural number following 18 and preceding 20 * one of the years 19 BC, AD 19, 1919, 2019 Films * ''19'' (film), a 2001 Japanese film * ''Nineteen'' (film), a 1987 science fiction film Music * 19 (band), a Japanese pop music duo Albums * ''19'' (Adele album), 2008 * ''19'', a 2003 album by Alsou * ''19'', a 2006 album by Evan Yo * ''19'', a 2018 album by MHD * ''19'', one half of the double album ''63/19'' by Kool A.D. * ''Number Nineteen'', a 1971 album by American jazz pianist Mal Waldron * ''XIX'' (EP), a 2019 EP by 1the9 Songs * "19" (song), a 1985 song by British musician Paul Hardcastle. * "Nineteen", a song by Bad4Good from the 1992 album ''Refugee'' * "Nineteen", a song by Karma to Burn from the 2001 album ''Almost Heathen''. * "Nineteen" (song), a 2007 song by American singer Billy Ray Cyrus. * "Nineteen", a song by Tegan and Sara from the 2007 album '' The Con''. * "XIX" (song), a 2014 song by Slipknot. ...
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1906 Pacific Hurricane Season
The 1900s Pacific hurricane seasons all began on May 15, 1900, in the northeast Pacific Ocean and on June 1, 1900, in the central Pacific. They ended on November 30, of each year. These dates conventionally delimit the time of year when most tropical cyclones form in northeast Pacific Ocean. Before the satellite age started in the 1960s, data on east Pacific hurricanes is extremely unreliable. For a few years, there are no reported cyclones, although many systems certainly formed. 1900 A "tropical hurricane" formed south of southwestern mainland Mexico on July 19, and moved generally westward out into the tropical Pacific, last noted well west-southwest of Baja California on July 29. 1901 A "tropical hurricane" formed south of southern Mexico on July 19, moving west-northwest through July 27, when it was last seen west of Baja California. 1902 I. Forming on July 14, a tropical cyclone made landfall on the southern portion of Baja California on July 22 as it moved northward and ...
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1904 Pacific Hurricane Season
The 1900s Pacific hurricane seasons all began on May 15, 1900, in the northeast Pacific Ocean and on June 1, 1900, in the central Pacific. They ended on November 30, of each year. These dates conventionally delimit the time of year when most tropical cyclones form in northeast Pacific Ocean. Before the satellite age started in the 1960s, data on east Pacific hurricanes is extremely unreliable. For a few years, there are no reported cyclones, although many systems certainly formed. 1900 A "tropical hurricane" formed south of southwestern mainland Mexico on July 19, and moved generally westward out into the tropical Pacific, last noted well west-southwest of Baja California on July 29. 1901 A "tropical hurricane" formed south of southern Mexico on July 19, moving west-northwest through July 27, when it was last seen west of Baja California. 1902 I. Forming on July 14, a tropical cyclone made landfall on the southern portion of Baja California on July 22 as it moved northward and ...
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1902 Pacific Hurricane Season
The 1900s Pacific hurricane seasons all began on May 15, 1900, in the northeast Pacific Ocean and on June 1, 1900, in the central Pacific. They ended on November 30, of each year. These dates conventionally delimit the time of year when most tropical cyclones form in northeast Pacific Ocean. Before the satellite age started in the 1960s, data on east Pacific hurricanes is extremely unreliable. For a few years, there are no reported cyclones, although many systems certainly formed. 1900 A "tropical hurricane" formed south of southwestern mainland Mexico on July 19, and moved generally westward out into the tropical Pacific, last noted well west-southwest of Baja California on July 29. 1901 A "tropical hurricane" formed south of southern Mexico on July 19, moving west-northwest through July 27, when it was last seen west of Baja California. 1902 I. Forming on July 14, a tropical cyclone made landfall on the southern portion of Baja California on July 22 as it moved northward and ...
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1832 Pacific Hurricane Season
The following is a list of Pacific hurricanes before 1900. Data on most of the storms that formed is unavailable, however, some regions had a large enough coastal population or ship traffic to give data on the occurrence of hurricanes. Tropical cyclones in the region typically formed between May and November. Seasons 1537 A hurricane struck Tlapa in Guerrero, Mexico, producing strong winds, hail, excessive rains, and other natural phenomena. Juan Bautista Moya, an Augustinian missionary friar in Tlapa and Chilapa viewed this tempest as "a miraculous prodigy of the Lord to confirm his missionary preaching among the indigenous people. The wind unleashed over the town of Tlaba and lashed the countryside and cottages like a giant whip. The fury of the gale uprooted and demolished trees. Hail shattered the maize corn grains without pity. Successive earthquakes at quick intervals further terrorized the populace." In this and other cases, the "earthquakes" probably entered the ...
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Tropical Depression
A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Depending on its location and strength, a tropical cyclone is referred to by different names, including hurricane (), typhoon (), tropical storm, cyclonic storm, tropical depression, or simply cyclone. A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean, and a typhoon occurs in the northwestern Pacific Ocean. In the Indian Ocean, South Pacific, or (rarely) South Atlantic, comparable storms are referred to simply as "tropical cyclones", and such storms in the Indian Ocean can also be called "severe cyclonic storms". "Tropical" refers to the geographical origin of these systems, which form almost exclusively over tropical seas. "Cyclone" refers to their winds moving in a circle, whirling round ...
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Tropical Cyclone Scales
Tropical cyclones are ranked on one of five tropical cyclone intensity scales, according to their maximum sustained winds and which tropical cyclone basins they are located in. Only a few scales of classifications are used officially by the meteorological agencies monitoring the tropical cyclones, but other scales also exist, such as accumulated cyclone energy, the Power Dissipation Index, the Integrated Kinetic Energy Index, and the Hurricane Severity Index. Tropical cyclones that develop in the Northern Hemisphere are unofficially classified by the warning centres on one of three intensity scales. Tropical cyclones or subtropical cyclones that exist within the North Atlantic Ocean or the North-eastern Pacific Ocean are classified as either tropical depressions or tropical storms. Should a system intensify further and become a hurricane, then it will be classified on the Saffir–Simpson hurricane wind scale, and is based on the estimated maximum sustained winds over a 1-minut ...
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Maximum Sustained Wind
The maximum sustained wind associated with a tropical cyclone is a common indicator of the intensity of the storm. Within a mature tropical cyclone, it is found within the eyewall at a distance defined as the radius of maximum wind, or RMW. Unlike gusts, the value of these winds are determined via their sampling and averaging the sampled results over a period of time. Wind measuring has been standardized globally to reflect the winds at above the Earth's surface, and the maximum sustained wind represents the highest average wind over either a one-minute (US) or ten-minute time span (see the definition, below), anywhere within the tropical cyclone. Surface winds are highly variable due to friction between the atmosphere and the Earth's surface, as well as near hills and mountains over land. Over the ocean, satellite imagery determines the value of the maximum sustained winds within a tropical cyclone. Land, ship, aircraft reconnaissance observations, and radar imagery can ...
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Monthly Weather Review
The ''Monthly Weather Review'' is a peer-reviewed scientific journal published by the American Meteorological Society. It covers research related to analysis and prediction of observed and modeled circulations of the atmosphere, including technique development, data assimilation, model validation, and relevant case studies. This includes papers on numerical techniques and data assimilation techniques that apply to the atmosphere and/or ocean environment. The editor-in-chief is David M. Schultz (University of Manchester). History The journal was established in July 1872 by the United States Army Signal Corps. It was issued by the Office of the Chief Signal Officer from 1872 until 1891. In 1891, the Signal Office's meteorological responsibilities were transferred to the Weather Bureau under the United States Department of Agriculture. The Weather Bureau published the journal until 1970 when the Bureau became part of the newly formed National Oceanic and Atmospheric Administratio ...
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