Portal:Tropical cyclones

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The Tropical Cyclones Portal

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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.

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Tropical Storm Manuel near hurricane strength on September 18

Hurricane Manuel (/ˌmæn(j)uˈɛl, ˌmɑːn-/) brought widespread flooding across much of Mexico in September 2013, in conjunction with Hurricane Ingrid. The fifteenth named storm and seventh hurricane of the annual hurricane season, Manuel originated from a strong area of low pressure south of Acapulco on September 13. Within favorable conditions aloft, the storm intensified into a tropical storm as it tracked northward. The following day, Manuel curved westward and strengthened to a point just shy of hurricane intensity before making its first landfall at that intensity on September 15. Due to interaction with land, the tropical storm quickly weakened, and its center dissipated over western Mexico on September 16. However, the storm's remnants continued to track northwestward into the Gulf of California, where they reorganized into a tropical cyclone the next day. Manuel regained tropical storm status on September 18 as it began to curve northeastward. Shortly thereafter, Manuel attained Category 1 hurricane intensity, before making its final landfall just west of Culiacán at peak intensity. Over land, Manuel quickly weakened due to interaction with Mexico's high terrain, and the storm dissipated early on September 20.

Due to the impending threat of Manuel, several Mexican municipalities were put under disaster alerts. Upon making its first landfall, Manuel caused extreme flooding in southern Mexico. Property and agricultural damage as a result of the system was widespread, and roughly one million people were estimated to have been directly affected. In Guerrero, 97 people perished, including 18 in Acapulco. Seventy-one others died due to a mudslide in La Pintada. In Guerrero alone, around 30,000 homes were damaged and 46 rivers overflowed their banks. There, 20,000 persons were evacuated to shelters. Statewide, repairs to damage from the storm totaled MXN$3 billion ($230 million USD). Other impacts from Manuel spread as far east as the Isthmus of Tehuantepec, where 300 families were displaced. In the region, at least 11,591 homes were destroyed by the floods. Meanwhile, the nation sustained additional impacts from Atlantic Hurricane Ingrid. (Full article...)

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The Atlantic hurricane reanalysis project of the National Oceanic and Atmospheric Administration seeks to correct and add new information about past North Atlantic hurricanes. It was started around 2000 to update HURDAT, the official hurricane database for the Atlantic Basin, which has become outdated since its creation due to various systematic errors introduced into the database over time. This effort has involved reanalyses of ship observations from the International Comprehensive Ocean-Atmosphere Data Set (ICOADS) as well as reanalyses done by other researchers over the years. It has been ongoing as of 2024. (Full article...)

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Unusual path of Typhoon Wayne, among the longest lasting Pacific typhoons on record. It formed to the west of the Philippines on August 16, and after looping to the northwest it attained typhoon status. Wayne turned to the northeast, striking Taiwan before turning to the southwest and weakening to tropical depression status. It then turned eastward and to the northeast, then re-attained typhoon status before changing its motion to the west. On September 5 it crossed northern Hainan Island, and the next day it dissipated after striking northern Vietnam. Typhoon Wayne caused over 71 fatalities along its path.

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The 1969 Atlantic hurricane season was the most active Atlantic hurricane season since the 1933 season, and was the final year of the most recent positive ("high-quality") Atlantic multidecadal oscillation (AMO) era. The hurricane season officially began on June 1, and lasted until November 30. Altogether, 12 tropical cyclones reached hurricane strength, the highest number on record at the time; a mark not surpassed until 2005. The season was above-average despite an El Niño, which typically suppresses activity in the Atlantic Ocean, while increasing tropical cyclone activity in the Pacific Ocean. Activity began with a tropical depression that caused extensive flooding in Cuba and Jamaica in early June. On July 25, Tropical Storm Anna developed, the first named storm of the season. Later in the season, Tropical Depression Twenty-Nine caused severe local flooding in the Florida Panhandle and southwestern Georgia in September.

The most significant storm of the season was Hurricane Camille, which peaked as a Category 5 hurricane on August 17 and devastated the Gulf Coast of the United States upon striking Mississippi the next day. Strong winds and storm surge heights especially impacted Mississippi and Louisiana. Later in its duration, the storm caused severe flooding Virginia and West Virginia. Camille alone was responsible for 259 deaths and $1.43 billion. It was the costliest United States hurricane at the time, until Hurricane Agnes in 1972. In early September, Hurricane Francelia caused deadly floods in Central America, with 271 people killed in Central America. Hurricane Inga had the third longest duration of an Atlantic tropical cyclone. The last storm, Hurricane Martha, was the only known tropical cyclone to make landfall in Panama. Martha caused minor flooding in the former and Costa Rica. Overall, the systems of the season collectively caused 535 deaths and over $1.5 billion in losses. (Full article...)

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Currently active tropical cyclones

Italicized basins are unofficial.

North Atlantic (2024): No active systems

East and Central Pacific (2024): No active systems

West Pacific (2024): No active systems

North Indian Ocean (2024): No active systems

Mediterranean (2023–24): No active systems

South-West Indian Ocean (2023–24): Moderate Tropical Storm Hidaya

Australian region (2023–24): No active systems

South Pacific (2023–24): No active systems

South Atlantic (2023–24): No active systems

Last updated: 02:33, 2 May 2024 (UTC)

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Tropical cyclone anniversaries

May 4

1982 - A tropical cyclone struck southern Burma, where it killed five people.
2009 - Typhoon Kujira (pictured) reaches peak strength as a Category 4 typhoon, after killing 28 people and causing P1.25 million (US$27 million) in damage in the Philippines.

May 5, 1974 - Typhoon Carla (pictured) reached its peak intensity with 150 km/h (90 mph) winds to the east of Iwo Jima. Carla had previously caused heavy damage to crops in the Northern Mariana Islands.

May 6, 1957 - Typhoon Trix (track pictured) reached its peak intensity with a central pressure of 950 hPa (mbar) to the east of the Philippines.

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Did you know…

…that the Joint Typhoon Warning Center considers that Typhoon Vera (pictured) of 1986 is actually two distinct systems, formed from two separated low-level circulations?
…that Hurricane Agatha (pictured) was the strongest Pacific hurricane to make landfall in Mexico in May since records began in 1949?
…that Cyclone Raquel (track pictured) travelled between the Australian and South Pacific basins between the 2014–15 and 2015–16 seasons, spanning both seasons in both basins?
…that Cyclone Amphan (pictured) in 2020 was the first storm to be classified as a Super Cyclonic Storm in the Bay of Bengal since 1999?

Did you know archive

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The following are images from various tropical cyclone-related articles on Wikipedia.

Image 1
South-West Indian Ocean cyclone
(from Cyclone)
Image 2Radar image of Hurricane Erika making landfall over Northeastern Mexico (from Tropical cyclone observation)
Image 3Percentages of hurricane deaths in the United States from 1970 to 1999. (from Effects of tropical cyclones)
Image 4
Atlantic hurricane
(from Cyclone)
Image 5Hurricane Catarina, a rare South Atlantic tropical cyclone viewed from the International Space Station on March 26, 2004 (from Cyclone)
Image 6The initial extratropical low-pressure area forms at the location of the red dot on the image. It is usually perpendicular (at a right angle to) the leaf-like cloud formation seen on satellite during the early stage of cyclogenesis. The location of the axis of the upper level jet stream is in light blue. (from Cyclone)
Image 7Surface weather map of the 1935 Labor Day hurricane moving up the west coast of Florida (from Tropical cyclone observation)
Image 8Subtropical Storm Alex in the north Atlantic Ocean in January 2016 (from Cyclone)
Image 9The aftermath of Hurricane Katrina in Gulfport, Mississippi. (from Tropical cyclone preparedness)
Image 10Personnel and equipment from the National Guard of the United States en route to Hurricane Florence response efforts in 2018
Image 11Aerial image of destroyed houses in Tacloban, following Typhoon Haiyan (from Effects of tropical cyclones)
Image 122017 Atlantic hurricane season summary map (from Cyclone)
Image 13A fictitious synoptic chart of an extratropical cyclone affecting the UK and Ireland. The blue arrows between isobars indicate the direction of the wind, while the "L" symbol denotes the centre of the "low". Note the occluded, cold and warm frontal boundaries. (from Cyclone)
Image 14
Pacific hurricane
(from Cyclone)
Image 15An extratropical cyclone near Iceland (from Cyclone)
Image 16An example of a chart for Matthew showing its five-day forecast track (from Tropical cyclone preparedness)
Image 17The aftermath of Hurricane Katrina in Gulfport, Mississippi. Katrina was the costliest tropical cyclone in United States history. (from Effects of tropical cyclones)
Image 18Broken concrete utility pole in Puerto Rico after Hurricane Maria in 2017, which ranks fourth in costliest US tropical cyclones. (from Effects of tropical cyclones)
Image 19Comparison between extratropical and tropical cyclones on surface analysis (from Cyclone)
Image 20
North Indian Ocean cyclone
(from Cyclone)
Image 21Flooding in Port Arthur, Texas caused by Hurricane Harvey. Harvey was the wettest and second-costliest tropical cyclone in United States history. (from Effects of tropical cyclones)
Image 22
South Pacific cyclone
(from Cyclone)
Image 23A polar low over the Sea of Japan in December 2009 (from Cyclone)
Image 24The dangerous semicircle is the upper-right corner, with the arrow marking the direction of motion of a Northern Hemisphere storm. Note that typhoons, etc. are asymmetrical, and semicircle is a convenient misnomer. (from Effects of tropical cyclones)
Image 25
Pacific typhoon
(from Cyclone)
Image 26Chart with concurrent information for Hurricane Arlene and Tropical Storm Bret logged and plotted (from Tropical cyclone preparedness)
Image 27All but the most expensive bottles of water were sold out at this Publix supermarket before Hurricane Irma; in the week preceding the storm, water sold out soon after shipments arrived (from Tropical cyclone preparedness)
Image 28Cyclone on Mars, imaged by the Hubble Space Telescope (from Cyclone)
Image 29Tropical cyclones form when the energy released by the condensation of moisture in rising air causes a positive feedback loop over warm ocean waters. (from Cyclone)
Image 30Hurricane Isabel (2003)'s effect on the North Carolina Outer Banks (from Effects of tropical cyclones)
Image 31The number of $1 billion Atlantic hurricanes almost doubled from the 1980s to the 2010s, and inflation-adjusted costs have increased more than elevenfold. The increases have been attributed to climate change and to greater numbers of people moving to coastal areas. (from Effects of tropical cyclones)
Image 32
Australian region cyclone
(from Cyclone)
Image 33Hurricane response involves working in hazardous conditions, including contamination and electrocution hazards from floodwater.

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This is a featured list, which represents some of the best list articles on English Wikipedia.

The list of North Carolina hurricanes before 1900 encompasses 139 tropical cyclones that affected the U.S. state of North Carolina. Collectively, cyclones in North Carolina during the time period resulted in over 775 direct fatalities during the period. Seven cyclones affected the state in the 1893 season, which was the year with the most tropical cyclones impacting the state during the time period. From the beginning of the official North Atlantic hurricane record in 1851 to 1899, there were 12 years without a known tropical cyclone affecting the state. The strongest hurricane to hit the state during the official record was the San Ciriaco hurricane of 1899, which struck the state with winds of 120 mph (195 km/h), although the 1821 Norfolk and Long Island Hurricane may have been stronger.

Historical data prior to 1700 is sparse due to lack of significant European settlements along the coastline; the few storms listed are largely records from Roanoke Colony and later the Province of Carolina. Modern meteorologists believe early storms were tropical cyclones, though due to the time period confirmation is impossible. One theory explaining the disappearance of Roanoke Colony suggests a hurricane destroyed the village, though there is no evidence to prove the theory. It is considered unlikely due to lack of damage to a fence around the village, on which the villagers left an inscription. (Full article...)

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Related WikiProjects

WikiProject Tropical cyclones is the central point of coordination for Wikipedia's coverage of tropical cyclones. Feel free to help!

WikiProject Weather is the main center point of coordination for Wikipedia's coverage of meteorology in general, and the parent project of WikiProject Tropical cyclones. Three other branches of WikiProject Weather in particular share significant overlaps with WikiProject Tropical cyclones:

The Non-tropical storms task force coordinates most of Wikipedia's coverage on extratropical cyclones, which tropical cyclones often transition into near the end of their lifespan.
The Floods task force takes on the scope of flooding events all over the world, with rainfall from tropical cyclones a significant factor in many of them.
WikiProject Severe weather documents the effects of extreme weather such as tornadoes, which landfalling tropical cyclones can produce.

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