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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Typhoon Thelma at peak intensity on July 11

Typhoon Thelma, known in the Philippines as Typhoon Katring, was the first super typhoon to form in the 1987 Pacific typhoon season. Forming from the monsoon trough in the Philippine Sea, Thelma was first designated as a tropical cyclone on July 7. After moving north, Thelma turned west, while remaining poorly organized. It finally attained typhoon status on July 9, soon after developing an eye, and began to intensify at a brisker clip. During the evening of July 10, Thelma attained maximum intensity while well to the east of the northern Philippines. It also turned sharply northward in response to a trough, slowly weakening. On July 15, Typhoon Thelma, now greatly reduced in intensity, struck the south coast of South Korea. The next day, Thelma rapidly dissipated, shortly after emerging into the Sea of Japan.

Although Thelma remained well offshore the Philippines, around 500 homes were swept away due to flooding, which left more than 3,500 people homeless. A total of 130 people were rescued after a vessel sunk. Nationwide, 12 people perished. In Japan, the typhoon brought heavy rains that was responsible for property damage in 19 prefectures. Throughout the country, three people died while around 1,000 dwellings were flooded. (Full article...)

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The ITOS 1 weather satellite image of the cyclone shortly after peak intensity making landfall in East Pakistan on November 12

The 1970 Bhola cyclone (also known as the Great Cyclone of 1970) was a devastating tropical cyclone that struck East Pakistan (present-day Bangladesh) and India's West Bengal on November 12, 1970. It remains the deadliest tropical cyclone ever recorded and one of the world's deadliest humanitarian disasters. At least 300,000 people died in the storm, possibly as many as 500,000, primarily as a result of the storm surge that flooded much of the low-lying islands of the Ganges Delta. Bhola was the sixth and strongest cyclonic storm of the 1970 North Indian Ocean cyclone season.

The cyclone formed over the central Bay of Bengal on November 8 and traveled northward, intensifying as it did so. It reached its peak with winds of 185 km/h (115 mph) on November 10, and made landfall on the coast of East Pakistan on the following afternoon. The storm surge devastated many of the offshore islands, wiping out villages and destroying crops throughout the region. In the most severely affected upazila, Tazumuddin, over 45% of the population of 167,000 were killed by the storm. (Full article...)

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The emblem of the 53rd Weather Reconnaissance Squadron, also known by its nickname, Hurricane Hunters. The squadron is a flying unit of the United States Air Force, and "the only Department of Defense organization still flying into tropical storms and hurricanes." It flies into tropical cyclones in the Atlantic Ocean, the Caribbean Sea, the Gulf of Mexico and the Central Pacific Ocean for the specific purpose of directly measuring weather data in and around those storms.

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The 1983 Atlantic hurricane season was the least active Atlantic hurricane season since 1930. The season officially began on June 1, 1983, and lasted until November 30, 1983. These dates conventionally delimit the period of each year when most storms form in the Atlantic basin. The season had very little activity, with only seven tropical depressions, four of which reached tropical storm strength or higher. This led to the lowest accumulated cyclone energy count since 1977.

The season began later than normal; the first tropical depression formed on July 23 and the second on July 27. Neither tropical depressions strengthened and they dissipated soon thereafter. Hurricane Alicia formed as Tropical Depression Three on August 15, quickly intensified into a hurricane on August 16 and made landfall in Texas on August 18. Alicia caused $3 billion in damage in Texas. Hurricane Barry formed on August 25, crossed Florida and strengthened into a hurricane. Barry made landfall near the Mexico–United States border, and dissipated over land on August 30. (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): No active systems

Australian region (2023–24): No active systems

South Pacific (2023–24): No active systems

South Atlantic (2023–24): No active systems

Last updated: 21:54, 8 May 2024 (UTC)

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Tropical cyclone anniversaries

May 19

1997 - A powerful cyclone (pictured) struck Bangladesh, killing 1,146 people.
2004 - A cyclone made landfall in Burma, causing floods and resulting in 236 fatalities.
2018 - Cyclone Sagar moved ashore Somaliland, with its associated floods killing 79 people across the region.

May 20

1989 - Typhoon Brenda makes landfall over Southern China as a Category 1 typhoon, killing about 84 people.
1999 - A powerful cyclone (pictured) struck southeastern Pakistan, killing at least 400 people, and perhaps as many as 6,000.
2005 - Tropical Depression Adrian became the first Pacific tropical cyclone to strike the Pacific coast of Honduras.

May 21

1976 - Typhoon Pamela passed over Guam with winds of 220 km/h (140 mph) and caused over $500 million of damage to the island.
2010 - Cyclone Laila (pictured) dissipates after causing destruction over the Andhra Pradesh region of India.

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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
Atlantic hurricane
(from Cyclone)
Image 2Tropical 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 3Comparison between extratropical and tropical cyclones on surface analysis (from Cyclone)
Image 4
South Pacific cyclone
(from Cyclone)
Image 5All 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 6Chart with concurrent information for Hurricane Arlene and Tropical Storm Bret logged and plotted (from Tropical cyclone preparedness)
Image 7The 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 8An example of a chart for Matthew showing its five-day forecast track (from Tropical cyclone preparedness)
Image 9
Australian region cyclone
(from Cyclone)
Image 10
North Indian Ocean cyclone
(from Cyclone)
Image 11
South-West Indian Ocean cyclone
(from Cyclone)
Image 12Broken 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 13
Pacific typhoon
(from Cyclone)
Image 14Aerial image of destroyed houses in Tacloban, following Typhoon Haiyan (from Effects of tropical cyclones)
Image 15Hurricane Isabel (2003)'s effect on the North Carolina Outer Banks (from Effects of tropical cyclones)
Image 162017 Atlantic hurricane season summary map (from Cyclone)
Image 17An extratropical cyclone near Iceland (from Cyclone)
Image 18Flooding 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 19Surface weather map of the 1935 Labor Day hurricane moving up the west coast of Florida (from Tropical cyclone observation)
Image 20Cyclone on Mars, imaged by the Hubble Space Telescope (from Cyclone)
Image 21Radar image of Hurricane Erika making landfall over Northeastern Mexico (from Tropical cyclone observation)
Image 22The 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 23A 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 24Subtropical Storm Alex in the north Atlantic Ocean in January 2016 (from Cyclone)
Image 25The aftermath of Hurricane Katrina in Gulfport, Mississippi. Katrina was the costliest tropical cyclone in United States history. (from Effects of tropical cyclones)
Image 26Hurricane Catarina, a rare South Atlantic tropical cyclone viewed from the International Space Station on March 26, 2004 (from Cyclone)
Image 27
Pacific hurricane
(from Cyclone)
Image 28The aftermath of Hurricane Katrina in Gulfport, Mississippi. (from Tropical cyclone preparedness)
Image 29A polar low over the Sea of Japan in December 2009 (from Cyclone)
Image 30The 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 31Percentages of hurricane deaths in the United States from 1970 to 1999. (from Effects of tropical cyclones)
Image 32Personnel and equipment from the National Guard of the United States en route to Hurricane Florence response efforts in 2018
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 Florida hurricanes from 1900 to 1949 encompasses 108 Atlantic tropical cyclones that affected the U.S. state of Florida. Collectively, tropical cyclones in Florida during the time period resulted in about $4 billion (2008 USD) in damage. Additionally, tropical cyclones in Florida were directly responsible for about 3,550 fatalities during the time period, most of which from the 1928 Okeechobee Hurricane. The 1947 season was the year with the most tropical cyclones affecting the state, with a total of 6 systems. The 1905, 1908, 1913, 1927, 1931, 1942, and 1943 seasons were the only years during the time period in which a storm did not affect the Floridan coasts.

The strongest hurricane to hit the state during the time period was the 1935 Labor Day hurricane, which also bears the distinction of being the strongest recorded hurricane to strike the United States. Several other major hurricanes struck the state during the time period, including the 1926 Miami hurricane, the 1928 Okeechobee hurricane, and a cyclone each in 1945, 1947, 1948, and 1949. All of these storms made landfall as Category 4 hurricanes. (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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