A tropical cyclone is a storm system characterized by a large low-pressure center, a closed low-level circulation and a spiral arrangement of numerous thunderstorms that produce strong winds and heavy rainfall. Tropical cyclones feed on the heat released when moist air rises, resulting in condensation of water vapor contained in the moist air. They are fueled by a different heat mechanism than other cyclonic windstorms such as Nor'easters, European windstorms and polar lows, leading to their classification as "warm core" storm systems. Most tropical cyclones originate in the doldrums, approximately ten degrees from the Equator.
The term "tropical" refers to both the geographic origin of these systems, which form almost exclusively in tropical regions of the globe, as well as to their formation in maritime tropical air masses. The term "cyclone" refers to such storms' cyclonic nature, with anticlockwise rotation in the Northern Hemisphere and clockwise rotation in the Southern Hemisphere. Depending on its location and intensity, a tropical cyclone may be referred to by names such as "hurricane", "typhoon", "tropical storm", "cyclonic storm", "tropical depression" or simply "cyclone".
Types of cyclone: 1. A "Typhoon" is a tropical cyclone located in the North-west Pacific Ocean which has the most cyclonic activity and storms occur year-round. 2. A "Hurricane" is also a tropical cyclone located at the North Atlantic Ocean or North-east Pacific Ocean which have an average storm activity and storms typically form between May 15 and November 30. 3. A "Cyclone" is a tropical cyclone that occurs in the South Pacific and Indian Oceans.
Hurricane Cora was a tropical cyclone which affected the Lesser Antilles during August 1978. The first hurricane of the 1978 Atlantic hurricane season, Cora originated as a disturbance that exited the African coast on August 7, the storm moved at an unusually high forward speed for a cyclone in the Atlantic Ocean in August. The storm later reached hurricane strength and formed a well-defined eye that lasted only 12 hours before the eye rapidly lost organization for unknown reasons, though the post-season report on the storm mentions the possibility that its high speed caused the eye to dissipate. The storm moved west-southwestward, weakening before making landfall on the island of Grenada. The storm lost its circulation and became a tropical wave on August 12. The remnant crossed over Central America into the Pacific Ocean, where it reintensified, becoming Hurricane Kristy.
Cora was an unusual cyclone, maintaining an unusually low latitude for the Atlantic in August at high speeds, similar to the tracks of Tropical Storm Alma in 1974 and Tropical Storm Fran in 1990. The hurricane was also upgraded into a hurricane based solely on satellite photography, the second time this occurred. Although it passed through the Windward Islands and the Lesser Antilles, only minor effects were reported. Cora was also responsible for altering weather conditions allowing for a takeoff of the historical flight of the Double Eagle II hot air balloon. (Full article...)Tropical cyclones and subtropical cyclones are named by various warning centers to simplify communication between forecasters and the general public regarding forecasts, watches and warnings. The names are intended to reduce confusion in the event of concurrent storms in the same basin. Once storms develop sustained wind speeds of more than 33 knots (61 km/h; 38 mph), names are generally assigned to them from predetermined lists, depending on the basin in which they originate. Some tropical depressions are named in the Western Pacific, while tropical cyclones must contain a significant amount of gale-force winds before they are named in the Southern Hemisphere.
Before it became standard practice to give personal (first) names to tropical cyclones, they were named after places, objects, or the saints' feast days on which they occurred. Credit for the first usage of personal names for weather systems is generally given to Queensland Government meteorologist Clement Wragge, who named systems between 1887 and 1907. When Wragge retired, the practice fell into disuse for several years until it was revived in the latter part of World War II for the Western Pacific. Formal naming schemes and lists have subsequently been used for major storms in the Eastern, Central, Western and Southern Pacific basins, and the Australian region, Atlantic Ocean and Indian Ocean. (Full article...)
The 1933 Atlantic hurricane season is the most active Atlantic hurricane season on record in terms of accumulated Cyclone Energy (ACE), with a total of 259. It also set a record for nameable tropical storms in a single season, 20, which stood until 2005, when there were 28 storms. The season ran for six months of 1933, with tropical cyclone development occurring as early as May and as late as November. A system was active for all but 13 days from June 28 to October 7.
Because technologies such as Earth observation satellites were not available until the 1960s, historical data on tropical cyclones from the early 20th century is often incomplete. Tropical cyclones that did not approach populated areas or shipping lanes, especially if they were relatively weak and of short duration, may have remained undetected. Compensating for the lack of comprehensive observation and the limited technological ability to monitor all tropical cyclone activity in the Atlantic Basin during this era, research meteorologist Christopher Landsea estimates that the 1933 season may have produced an additional 2–3 missed tropical cyclones. A 2013 reanalysis of the 1933 Atlantic Hurricane Database did indeed identify two new tropical storms; however, it was also determined that two existing cyclones did not reach tropical storm intensity and so were removed from the database. Additionally, researchers found two existing storms to be one continuous system. As a result, the season storm total dropped from 21 to 20. (Full article...)Italicized basins are unofficial.
Last updated: 21:17, 11 August 2024 (UTC)
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