Portal:Tropical cyclones

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The Tropical Cyclones Portal

Hurricane Isabel in 2003 as seen from the International Space Station
Hurricane Isabel

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.

Cyclone Veronica at peak intensity nearing its landfall in Western Australia on 21 March

Severe Tropical Cyclone Veronica was a large and powerful tropical cyclone which brought major impacts to the Pilbara region of Western Australia during March 2019. The nineteenth tropical low, eighth tropical cyclone and fifth severe tropical cyclone on the 2018–19 Australian region cyclone season, Veronica first appeared as a tropical low near East Timor on 18 March 2019. The system was slow to develop initially while tracking southwestwards through the Timor Sea, but began to consolidate the following day. The storm was upgraded by the Australian Bureau of Meteorology (BOM) to a Category 1 tropical cyclone on the Australian scale at 18:00 UTC on 19 March, by which time a steady development trend had begun. Upon attaining Category 2 status at 06:00 UTC on 20 March, Veronica underwent a period of explosive intensification. The system became a severe tropical cyclone six hours later, and Category 4 just six hours after that. Veronica reached peak intensity at 06:00 UTC the following day as a high-end Category 4 severe tropical cyclone, with ten-minute sustained winds estimated at 195 km/h (120 mph), and a central barometric pressure of 938 hPa (27.70 inHg). The United States' Joint Typhoon Warning Center estimated that the system was generating one-minute sustained winds of 230 km/h (145 mph), equivalent to a mid-range Category 4 major hurricane on the Saffir-Simpson hurricane wind scale. Veronica proceeded to weaken very gradually over the following few days as it turned towards Western Australia's Pilbara coastline. The system weakened to Category 3 while located just off the Pilbara coast, where it became almost stationary for 24 hours. Veronica began to weaken more quickly as it accelerated westwards on 25 March, tracking parallel to the coast. The system was downgraded below tropical cyclone intensity on 26 March, and after making landfall on North West Cape later that day, the system began to track away from the Australian mainland. Ex-Tropical Cyclone Veronica dissipated on 31 March over the eastern Indian Ocean.

When Veronica struck Australia in March 2019, it flooded major areas and caused about AUS$1.7 billion (US$1.2 billion) in economic losses, primarily from disruptions to iron ore exports. This storm formed near the time when Cyclone Trevor made landfall in Queensland. Most of the coastal regions of Pilbara suffered some level of damage. (Full article...)
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A tropical cyclone rainfall climatology is developed to determine rainfall characteristics of past tropical cyclones. A tropical cyclone rainfall climatology can be used to help forecast current or upcoming tropical cyclone impacts. The degree of a tropical cyclone rainfall impact depends upon speed of movement, storm size, and degree of vertical wind shear. One of the most significant threats from tropical cyclones is heavy rainfall. Large, slow moving, and non-sheared tropical cyclones produce the heaviest rains. The intensity of a tropical cyclone appears to have little bearing on its potential for rainfall over land, but satellite measurements over the last several years show that more intense tropical cyclones produce noticeably more rainfall over water. Flooding from tropical cyclones remains a significant cause of fatalities, particularly in low-lying areas. (Full article...)
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Hurricane Mitch near peak intensity. When this photo was taken, Mitch was in the Caribbean Sea off the coast of Central America.


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The 2003 Atlantic hurricane season was a very active season with tropical cyclogenesis occurring before and after the official bounds of the season—the first such occurrence since the 1970 season. The season produced 21 tropical cyclones, of which 16 developed into named storms; seven of those attained hurricane status, of which three reached major hurricane status. The strongest hurricane of the season was Hurricane Isabel, which reached Category 5 status on the Saffir–Simpson hurricane scale northeast of the Lesser Antilles; Isabel later struck North Carolina as a Category 2 hurricane, causing $3.6 billion in damage (2003 USD) and a total of 51 deaths across the Mid-Atlantic region of the United States.

Although the bounds of the season are typically from June 1 to November 30, the season began early with the formation of Subtropical Storm Ana on April 20, and it ended relatively late on December 11 with the dissipation of Tropical Storm Peter. In early September, Hurricane Fabian struck Bermuda as a Category 3 hurricane, where it was the worst hurricane since 1926; on the island it caused four deaths and $300 million in damage (2003 USD). Hurricane Juan caused considerable destruction to Nova Scotia, particularly Halifax, as a Category 2 hurricane, the first hurricane of significant strength to hit the province since 1893. Additionally, Hurricanes Claudette and Erika struck Texas and Mexico, respectively, as minimal hurricanes. In December, Tropical Storm Odette struck the Dominican Republic, and Tropical Storm Peter formed in the eastern portion of the basin. (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)

Tropical cyclone anniversaries

June 4

  • 2006 - Cyclone Gonu (pictured) became the strongest tropical cyclone on record in the Arabian Sea, with 3-minute winds of 155 km/h (100 mph); two days later, Gonu struck the Arabian Peninsula, killing 49 people and causing about $4 billion of damage.
  • 2012 - Typhoon Mawar reaches peak intensity as a Category 3 typhoon.
  • 2014 - Tropical Storm Boris makes landfall over Southwestern Mexico and kills 6 people with US$46.8 million in damages.

June 5

June 6


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The 2008 Atlantic hurricane season was an event in the annual tropical cyclone season in the north Atlantic Ocean. An above-average Atlantic hurricane season season, it was the first on record to have a major hurricane in every month from July to November.

The season officially began on June 1, 2008, and ended on November 30, 2008, dates that conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin. The season's first storm, Tropical Storm Arthur, formed on May 30, and the last, Hurricane Paloma, dissipated on November 10. Pre-season forecasts noted a high possibility for an above average number of tropical cyclones, primarily due to lingering La Niña effects and abnormally warm sea surface temperatures across the Atlantic basin. Altogether, 16 of the 17 tropical cyclones observed during the season developed into tropical storms. Of these, eight became hurricanes with five intensifying further into major hurricanes. With the exception of Tropical Storm Nana, every tropical cyclone during the season affected land to an extent. (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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