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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Bud at peak intensity while off the coast of Mexico on June 11

Hurricane Bud was a Category 4 hurricane that brought winds and severe flooding to Mexico throughout its existence as a tropical cyclone in June 2018. It was the second named storm, hurricane, and major hurricane of the 2018 Pacific hurricane season.^[1] Bud originated from a tropical wave that departed from Western Africa on May 29. It traveled across the Atlantic Ocean before entering the Northeast Pacific Ocean late on June 6. The system moved towards the northwest and steadily organized, becoming a tropical depression on June 9 and Tropical Storm Bud early the next day. Favorable upper-level winds, ample moisture aloft, and warm sea surface temperatures allowed the storm to rapidly intensify to a hurricane late on June 10, and further to a major hurricane on the following day. Bud ultimately peaked the next morning with maximum sustained winds of 140 mph (230 km/h) and a minimum central pressure of 943 mbar (943 hPa; 27.8 inHg). Its track curved more northward while the storm rapidly succumbed to the effects of upwelling. Bud made landfall on Baja California Sur as a minimal tropical storm early on June 15. On the next day, land interaction and increasing wind shear caused Bud to degenerate into a post-tropical cyclone. It opened up into a trough of low-pressure on June 16. The remnants of Bud moved towards the Southwestern United States, bringing tropical moisture and gusty winds to the region.

Bud prompted the issuance of multiple watches and warnings for Baja California Sur and western and central Mexico. Bud caused two deaths in Mexico; one in Mexico City and another in Baja California Sur. Despite remaining offshore for most of its track, the hurricane caused torrential rainfall and severe flooding in several regions. A peak rainfall total of 6.50 in (165 mm) was recorded in San Lorenzo, Sinaloa. In Guadalajara, Jalisco, hundreds of vehicles were inundated and swept away. A canal overflowed in Guadalajara, causing damage to multiple stores in a mall. At least 100 additional structures were damaged in the city. In Guerrero, hundreds of businesses and homes were flooded. Over 100 businesses in Pie de la Cuesta were damaged by strong waves. More than 60 homes in Maruata, Michoacan, experienced flood or wind damage. Severe flooding along a street in Mexico City inundated dozens of vehicles, necessitating the rescue of their passengers. Rains from Bud's remnants brought relief to drought-stricken areas and slowed the growth of wildfires in Wyoming and Colorado. The influx of moisture prompted the issuance of flash flood watches for Colorado and New Mexico, and caused flooding near Cave Creek, Arizona. (Full article...)

List of selected named cyclones

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The hurricane on October 16, 1970

The 1970 Canada hurricane was an unnamed tropical cyclone that brought impact to Bermuda and Newfoundland. The fourth hurricane and ninth tropical storm of the annual hurricane season, this system developed northeast of the Bahamas as a subtropical depression on October 12. While tracking northeastward, the system intensified, becoming a subtropical storm on the following day. The subtropical storm transitioned into a tropical cyclone on October 16, and strengthened into a hurricane about twelve hours later. The hurricane later bypassed Bermuda, before further intensifying into a Category 2 hurricane on the Saffir–Simpson hurricane wind scale. Thereafter, the hurricane accelerated rapidly northeastward, and made landfall on the Avalon Peninsula of Newfoundland as a Category 1 hurricane. It transitioned into an extratropical cyclone early on October 17.

The system produced tropical storm force winds on Bermuda, which caused the suspension of schools, transportation, and interrupted businesses, although minimal structural damage occurred. Light rainfall was also reported on the island. Hurricane-force winds were observed throughout Newfoundland, which caused damage to structures, though mostly limited to broken windows. Rough seas damaged fishing dories and a fishing ramp on the Atlantic coast of the island. The cost of damage on the Burin Peninsula was estimated to be in the thousands of dollars, although the specific figure in unknown. Heavy rainfall was also reported in the region, with precipitation in Quebec reaching nearly 5 inches (130 mm). On the French Territory of Saint Pierre and Miquelon, several buildings and houses lost their roof due to strong winds. (Full article...)

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Cyclone Inigo near peak intensity, as a Category 5 severe tropical cyclone on the Australian region scale, with 10-minute sustained winds of 150 miles per hour (240 km/h) and 1-minute sustained winds of 160 miles per hour (260 km/h). This image was taken from by one of NASA's EOSDIS satellites on April 4, 2003, while the cyclone was to the south of Indonesia.

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The 1996 Pacific hurricane season had below normal tropical cyclone activity, producing 9 tropical storms, of which 5 became hurricanes, with 2 of those intensifying into major hurricanes. With an Accumulated cyclone energy (ACE) index of 53.9, the season ranks among the least intense Pacific hurricane seasons on record. It officially began May 15, 1996, in the eastern north Pacific and on June 1, 1996, in the central north Pacific. It ended on November 30, 1996. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. The season slightly exceeded these bounds when tropical storm One-E formed on May 13.

Much of the season's activity was clustered near the coast of Southwest Mexico, with four hurricanes and one tropical storm making landfall along it. The most impactful were: Hurricane Alma, which was responsible for 20 deaths, and Hurricane Fausto, which left behind damage amounting to around $800,000 (1996 USD). Hurricane Douglas was the strongest storm of the season, reaching Category 4 intensity on the Saffir-Simpson Hurricane Scale. Douglas developed in the Caribbean Sea, within the Atlantic basin, as Hurricane Cesar, before crossing into the Pacific as a tropical storm. (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: 21:50, 2 June 2024 (UTC)

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Tropical cyclone anniversaries

June 8

1960 - Typhoon Mary struck Hong Kong, killing 1,649 people across southeastern China.
1966 - Hurricane Alma made landfall in western Cuba causing severe flooding. The storm killed a total of 90 people and caused over $200 million of damage.

June 9

1934 - A hurricane struck what is now Belize after looping across Central America. The storm killed at least 516 people along its path.
1989 - Typhoon Dot (track pictured) reached peak strength as a Category 3 while nearing landfall over in Hainan, causing 8 deaths and CN¥170 million (US$45.1 million) of damages.
1998 - A cyclone struck the Indian state of Gujarat, killing at least 4,000 people.

June 10

1974 - Typhoon Dinah made landfall on the island of Luzon in the Philippines. Dinah killed 73 people in the Philippines, Hainan and Vietnam.
1991 - Cyclone Gritelle (pictured) became a named system, making it the strongest system within the south-west Indian Ocean to form in the month of June, as well as the latest in the cyclone year to be properly named.

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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

General images - load new batch

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

Image 1Tropical 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 2Cyclone on Mars, imaged by the Hubble Space Telescope (from Cyclone)
Image 3Surface weather map of the 1935 Labor Day hurricane moving up the west coast of Florida (from Tropical cyclone observation)
Image 4Radar image of Hurricane Erika making landfall over Northeastern Mexico (from Tropical cyclone observation)
Image 5Chart with concurrent information for Hurricane Arlene and Tropical Storm Bret logged and plotted (from Tropical cyclone preparedness)
Image 6
Atlantic hurricane
(from Cyclone)
Image 7Subtropical Storm Alex in the north Atlantic Ocean in January 2016 (from Cyclone)
Image 8Hurricane Catarina, a rare South Atlantic tropical cyclone viewed from the International Space Station on March 26, 2004 (from Cyclone)
Image 9A 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 10Personnel and equipment from the National Guard of the United States en route to Hurricane Florence response efforts in 2018
Image 11The aftermath of Hurricane Katrina in Gulfport, Mississippi. (from Tropical cyclone preparedness)
Image 12The 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 13All 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 14Hurricane response involves working in hazardous conditions, including contamination and electrocution hazards from floodwater.
Image 15The aftermath of Hurricane Katrina in Gulfport, Mississippi. Katrina was the costliest tropical cyclone in United States history. (from Effects of tropical cyclones)
Image 16An example of a chart for Matthew showing its five-day forecast track (from Tropical cyclone preparedness)
Image 17Broken 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 18
Pacific hurricane
(from Cyclone)
Image 19An extratropical cyclone near Iceland (from Cyclone)
Image 20A polar low over the Sea of Japan in December 2009 (from Cyclone)
Image 21The 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 22Percentages of hurricane deaths in the United States from 1970 to 1999. (from Effects of tropical cyclones)
Image 23Hurricane Isabel (2003)'s effect on the North Carolina Outer Banks (from Effects of tropical cyclones)
Image 24Aerial image of destroyed houses in Tacloban, following Typhoon Haiyan (from Effects of tropical cyclones)
Image 25The 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 26
South Pacific cyclone
(from Cyclone)
Image 272017 Atlantic hurricane season summary map (from Cyclone)
Image 28Flooding 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 29Comparison between extratropical and tropical cyclones on surface analysis (from Cyclone)
Image 30
North Indian Ocean cyclone
(from Cyclone)
Image 31
Australian region cyclone
(from Cyclone)
Image 32
Pacific typhoon
(from Cyclone)
Image 33
South-West Indian Ocean cyclone
(from Cyclone)

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

The Arabian Peninsula is a peninsula between the Red Sea, the Arabian Sea, and the Persian Gulf. There are 64 known tropical cyclones that affected the peninsula, primarily Yemen and Oman. For convenience, storms are included that affected the Yemeni island of Socotra. Most of the tropical cyclones originated in the Arabian Sea, the portion of the Indian Ocean north of the equator and west of India. The remainder formed in the Bay of Bengal off India's east coast. Collectively, the 64 storms have caused at least US$8.3 billion in damage and 1,693 deaths. The strongest and most damaging cyclone was Cyclone Gonu, which caused US$4 billion in damage and 50 fatalities when it struck Oman in 2007. Tropical cyclone damage in the Arabian Peninsula is chiefly due to flooding. (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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