Cyclone Amanda
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Cyclone Amanda
The name Amanda has been used for two tropical cyclone 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. Depend ...s in the Eastern Pacific Ocean and two in the Southern Hemisphere. Eastern Pacific Ocean: * Hurricane Amanda (2014), a Category 4 hurricane that became the strongest Eastern Pacific hurricane in the month of May. * Tropical Storm Amanda (2020), a short-lived tropical storm that made landfall in southeastern Guatemala. Its remnants spawned Tropical Storm Cristobal in the Gulf of Mexico. South-West Indian Ocean: * Cyclone Amanda (1963), stayed well out to sea to the east of Madagascar. Australian region: * Cyclone Amanda (1965), formed in the Arafura Sea and drifted across the Northern Territory and Western Australia. See also * Hurricane Amanda, an 1863 Atlantic storm which ...
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Tropical Cyclone
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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Hurricane Amanda (2014)
Hurricane Amanda was the strongest Eastern Pacific tropical cyclone ever recorded in the month of May. The first named storm, hurricane and major hurricane of the 2014 Pacific hurricane season, Amanda originated from a tropical wave that had entered the Eastern Pacific on May 16. Slow development occurred as it tracked westward, and development into a tropical depression occurred on May 22. The depression later strengthened into a tropical storm on May 23. Amid very favorable conditions, Amanda then rapidly intensified late on May 23, eventually reaching its peak intensity on May 25 as a high-end Category 4 hurricane. Afterwards, steady weakening occurred due to upwelling beneath the storm, and Amanda fell below major hurricane intensity on May 26. Rapid weakening occurred and the cyclone eventually dissipated on May 29. The tropical cyclone did not directly impact landmasses, however it had indirect impacts along the coast of Mexico. Heavy rains caused flooding in the towns of ...
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Tropical Storms Amanda And Cristobal
Tropical Storm Amanda and Tropical Storm Cristobal were two related, consecutive tropical storms that affected Central America, southern Mexico, the central United States, and Canada in late May and early June 2020. The first tropical cyclone formed in the East Pacific and was named ''Amanda.'' After crossing Central America, it regenerated into a second one in the Gulf of Mexico and was named ''Cristobal''. Amanda was the second tropical depression and the first named storm of the 2020 Pacific hurricane season, and Cristobal was the third named storm of the extremely active 2020 Atlantic hurricane season, and the earliest third named storm in the North Atlantic Ocean on record. Cristobal's regeneration date in the North Atlantic eclipsed the date set by Tropical Storm Colin in 2016, which formed on June 5. It was also the first Atlantic tropical storm formed in the month of June since Cindy in 2017, and the first June tropical cyclone to make landfall in Mexico since ...
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1963–64 South-West Indian Ocean Cyclone Season
The 1963–64 South-West Indian Ocean cyclone season was an average cyclone season. Systems Tropical Cyclone Amanda Amanda existed from December 1 to December 14. Moderate Tropical Storm Betty Better existed from December 23 to December 28. Severe Tropical Storm Christine Christine existed from January 9 to January 16. Tropical Cyclone Danielle Danielle existed from January 15 to January 23. On January 20, Danielle crossed between Réunion and Mauritius, producing wind gusts of in the latter island. Over three days, the storm dropped heavy rainfall, reaching . Moderate Tropical Storm Eileen Eileen existed from January 29 to February 10. Tropical Disturbance Frances Frances existed from February 19 to February 23. Intense Tropical Cyclone Giselle Giselle existed from February 22 to March 4. On February 28, Giselle passed just northwest of Réunion, producing wind gusts of . Four days' of rainfall, reaching at Belouve, caused heavy flooding damage. ...
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1960–1970 Australian Region Cyclone Seasons
The following is a list of all reported tropical cyclones within the Australian region between 90°E and 160°E in the 1960s. During the decade, tropical cyclones were named by the New Caledonia Meteorological Service, while the Australian Bureau of Meteorology started to name them during the 1963–64 season. Systems 1960–61 *July 15–21, 1960 – A tropical cyclone existed over the Indian Ocean. *November 29–30, 1960 – A tropical cyclone existed over the Indian Ocean. *December 15–24, 1960 – A tropical cyclone existed over the Arafura Sea and moved towards north-western Australia. *December 29, 1960 – January 3, 1961 – A tropical cyclone existed over the Indian Ocean. *January 2–6, 1961 – A tropical cyclone existed over the Coral Sea and impacted the Cape York Peninsular. *January 7–14, 1961 – Tropical Cyclone Barberine. *January 8–11, 1961 – A tropical cyclone existed near the Cocos Islands. *January 15–2 ...
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1863 Atlantic Hurricane Season
The 1863 Atlantic hurricane season featured five landfalling tropical cyclones. In the absence of modern satellite and other remote-sensing technologies, only storms that affected populated land areas or encountered ships at sea were recorded, so the actual total could be higher. An undercount bias of zero to six tropical cyclones per year between 1851 and 1885 has been estimated. There were seven recorded hurricanes and no major hurricanes, which are Category 3 or higher on the modern day Saffir–Simpson scale. Of the known 1863 cyclones, seven were first documented in 1995 by José Fernández-Partagás and Henry Diaz, while the ninth tropical storm was first documented in 2003. These changes were largely adopted by the National Oceanic and Atmospheric Administration's Atlantic hurricane reanalysis in their updates to the Atlantic hurricane database (HURDAT), with some adjustments. Although it is not officially listed in HURDAT, Hurricane "Amanda", named after a ship ru ...
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Pacific Hurricane Set Index Articles
The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the continents of Asia and Oceania in the west and the Americas in the east. At in area (as defined with a southern Antarctic border), this largest division of the World Ocean—and, in turn, the hydrosphere—covers about 46% of Earth's water surface and about 32% of its total surface area, larger than Earth's entire land area combined .Pacific Ocean
. '' Britannica Concise.'' 2008: Encyclopædia Britannica, Inc.
The centers of both the

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South-West Indian Ocean Cyclone Set Index Articles
The points of the compass are a set of horizontal, radially arrayed compass directions (or azimuths) used in navigation and cartography. A compass rose is primarily composed of four cardinal directions—north, east, south, and west—each separated by 90 degrees, and secondarily divided by four ordinal (intercardinal) directions—northeast, southeast, southwest, and northwest—each located halfway between two cardinal directions. Some disciplines such as meteorology and navigation further divide the compass with additional azimuths. Within European tradition, a fully defined compass has 32 'points' (and any finer subdivisions are described in fractions of points). Compass points are valuable in that they allow a user to refer to a specific azimuth in a colloquial fashion, without having to compute or remember degrees. Designations The names of the compass point directions follow these rules: 8-wind compass rose * The four cardinal directions are north (N), east (E), s ...
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