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.

Selected named cyclone - show another

Hurricane Pali at peak intensity, over the Central Pacific on January 13

Hurricane Pali was the earliest-forming Pacific hurricane on record, being the first Pacific hurricane to occur in January since Hurricane Ekeka of 1992. The first tropical cyclone of the 2016 Pacific hurricane season, Pali originated as an area of low pressure within a persistent trough, near the equator on January 6, 2016. Deep convection gradually built up around the center of the disturbance as the system curved northward, before it organized into a tropical depression on the next day, making the system the earliest recorded tropical cyclone in the Pacific hurricane basin. The system quickly intensified into a tropical storm, resulting in it being named Pali. During the next few days, Pali slowly moved northward while slowly curving towards the west, strengthening somewhat before weakening due to the presence of wind shear. On January 10, Pali slowly turned eastward and proceeded to re-strengthen as wind shear diminished.

On January 12, Pali strengthened into a Category 1 hurricane on the Saffir–Simpson scale (SSWHS) while curving towards the south. The next day, Pali reached its peak intensity as a Category 2 hurricane, with 1-minute maximum sustained winds of 100 mph (155 km/h) and a minimum central pressure of 978 mbar (hPa; 28.88 inHg). Afterward, Pali quickly began to weaken, as the storm encountered stronger wind shear, with the storm weakening into a Category 1 hurricane several hours later, before weakening into a tropical storm later that day. On January 14, Pali weakened into a tropical depression before degenerating into a remnant low the next day, since conditions became increasingly hostile. Later that day, Pali's remnants dissipated near the same location where they had formed roughly a week ago. Pali formed and tracked near the equator, forming at a latitude of 3.3°N and tracking as low as 2.6°N as a tropical depression. This made Pali the second-lowest latitude tropical cyclone on record in the Western Hemisphere at the time, which was extremely unusual, given the unfavorable conditions that are usually in place around the equator. (Full article...)

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This is how forecast model tracks appear within ATCF. This example is from 2006 Ernesto's first advisory. The NHC official forecast is light blue, while the storm's actual track is the white line over Florida.

The Automated Tropical Cyclone Forecasting System (ATCF) is a piece of software originally developed to run on a personal computer for the Joint Typhoon Warning Center (JTWC) in 1988, and the National Hurricane Center (NHC) in 1990. ATCF remains the main piece of forecasting software used for the United States Government, including the JTWC, NHC, and Central Pacific Hurricane Center. Other tropical cyclone centers in Australia and Canada developed similar software in the 1990s. The data files with ATCF lie within three decks, known as the a-, b-, and f-decks. The a-decks include forecast information, the b-decks contain a history of center fixes at synoptic hours, and the f-decks include the various fixes made by various analysis center at various times. In the years since its introduction, it has been adapted to Unix and Linux platforms. (Full article...)

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The map of global tropical cyclone tracks from 1985 to 2005 includes hundreds of systems that affected over a dozen countries. This picture was made using NASA imagery and data from various meteorological agencies.

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The 2016 Atlantic hurricane season was the first above-average hurricane season since 2012, producing 15 named storms, 7 hurricanes and 4 major hurricanes. The season officially started on June 1 and ended on November 30, though the first storm, Hurricane Alex which formed in the Northeastern Atlantic, developed on January 12, being the first hurricane to develop in January since 1938. The final storm, Otto, crossed into the Eastern Pacific on November 25, a few days before the official end. Following Alex, Tropical Storm Bonnie brought flooding to South Carolina and portions of North Carolina. Tropical Storm Colin in early June brought minor flooding and wind damage to parts of the Southeastern United States, especially Florida. Hurricane Earl left 94 fatalities in the Dominican Republic and Mexico, 81 of which occurred in the latter. In early September, Hurricane Hermine, the first hurricane to make landfall in Florida since Hurricane Wilma in 2005, brought extensive coastal flooding damage especially to the Forgotten and Nature coasts of Florida. Hermine was responsible for five fatalities and about $550 million (2016 USD) in damage.

The strongest, costliest, and deadliest storm of the season was Hurricane Matthew, the southernmost Category 5 Atlantic hurricane on record and the first to reach that intensity since Felix in 2007, ending the longest streak of seasons without a hurricane of such intensity in the Satellite Era. With at least 603 deaths attributed to it, Matthew was the deadliest Atlantic hurricane since Stan of 2005. Furthermore, damage from Matthew is estimated to be at least $16.5 billion, making it the ninth costliest Atlantic hurricane on record at the time. Hurricane Nicole became the first major hurricane to directly impact Bermuda since Hurricane Fabian in 2003, leaving widespread but relatively moderate damage on the island. The final tropical cyclone of the season – Hurricane Otto – brought severe flooding to Central America in November, particularly in Costa Rica and Nicaragua. Otto left 23 deaths and about $190 million in damage. On November 25, the storm emerged into the Eastern Pacific basin, the first such occurrence since Hurricane Cesar–Douglas in 1996. Most of the season's tropical cyclones impacted land, and nine of those storms caused loss of life. Collectively, the storms left at least 736 fatalities and $17.49 billion in damage, making the season the costliest since 2012. (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): Tropical Low 12U

South Pacific (2023–24): No active systems

South Atlantic (2023–24): No active systems

Last updated: 07:47, 13 April 2024 (UTC)

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Tropical cyclone anniversaries

April 17

2008 - Typhoon Neoguri reaches peak intensity with 1-minute winds of 185 km/h (115 mph) over in the South China Sea.
2016 - While moving through the Seychelles, Cyclone Fantala became the strongest recorded tropical cyclone in the south-west Indian Ocean, with 10-minute winds of 255 km/h (155 mph).
2021 - Typhoon Surigae (pictured) reaches peak intensity with 1-minute sustained winds of 305 km/h (190 mph) and a minimum barometric pressure of 895 hPa, making it the strongest Northern Hemisphere tropical cyclone to form before the month of May.

April 18

2000 - Tropical Storm Innocente (pictured) reached its peak intensity with winds of 65 km/h (40 mph) in the central Indian Ocean. Innocente did not affect any land.
2000 - Cyclone Paul begins weakening after it attained peak strength as a Category 5 severe tropical cyclone by BoM.

April 19

1945 - Tropical Storm Ann, the first named tropical system in the Northwest Pacific, develops over in Micronesia.
1959 - Typhoon Tilda attains peak intensity with 1-minute sustained winds of 230 km/h (145 mph) as it was west of Guam.
2000 - Cyclone Rosita (pictured) reached its peak intensity with a central pressure of 930 hPa (mbar) to the north of Broome, Western Australia.

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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 1The aftermath of Hurricane Katrina in Gulfport, Mississippi. (from Tropical cyclone preparedness)
Image 2Hurricane Isabel (2003)'s effect on the North Carolina Outer Banks (from Effects of tropical cyclones)
Image 3Flooding 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 4The aftermath of Hurricane Katrina in Gulfport, Mississippi. Katrina was the costliest tropical cyclone in United States history. (from Effects of tropical cyclones)
Image 5Cyclone on Mars, imaged by the Hubble Space Telescope (from Cyclone)
Image 6Hurricane response involves working in hazardous conditions, including contamination and electrocution hazards from floodwater.
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 8The 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 9Aerial image of destroyed houses in Tacloban, following Typhoon Haiyan (from Effects of tropical cyclones)
Image 10The 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 11Personnel and equipment from the National Guard of the United States en route to Hurricane Florence response efforts in 2018
Image 12Tropical 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 13An extratropical cyclone near Iceland (from Cyclone)
Image 14Subtropical Storm Alex in the north Atlantic Ocean in January 2016 (from Cyclone)
Image 15Radar image of Hurricane Erika making landfall over Northeastern Mexico (from Tropical cyclone observation)
Image 16An example of a chart for Matthew showing its five-day forecast track (from Tropical cyclone preparedness)
Image 17Percentages of hurricane deaths in the United States from 1970 to 1999. (from Effects of tropical cyclones)
Image 18
Pacific hurricane
(from Cyclone)
Image 192017 Atlantic hurricane season summary map (from Cyclone)
Image 20Comparison between extratropical and tropical cyclones on surface analysis (from Cyclone)
Image 21A 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 22
Australian region cyclone
(from Cyclone)
Image 23
North Indian Ocean cyclone
(from Cyclone)
Image 24
South Pacific cyclone
(from Cyclone)
Image 25Surface weather map of the 1935 Labor Day hurricane moving up the west coast of Florida (from Tropical cyclone observation)
Image 26A polar low over the Sea of Japan in December 2009 (from Cyclone)
Image 27
Atlantic hurricane
(from Cyclone)
Image 28
South-West Indian Ocean cyclone
(from Cyclone)
Image 29Hurricane Catarina, a rare South Atlantic tropical cyclone viewed from the International Space Station on March 26, 2004 (from Cyclone)
Image 30Broken 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 31
Pacific typhoon
(from Cyclone)
Image 32All 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 33Chart with concurrent information for Hurricane Arlene and Tropical Storm Bret logged and plotted (from Tropical cyclone preparedness)

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

Arizona has been affected by hurricanes on numerous occasions. Usually, these storms originate in the eastern Pacific Ocean, make landfall in the Mexican states of Baja California or Sonora, and dissipate before crossing into the United States. Thus, in most cases, it is only the tropical cyclones' remnant moisture that produces heavy rainfall—and in some occasions, flooding—in portions of Arizona. However, approximately every five years, a tropical cyclone retains sufficient strength to enter the state as a tropical storm or a tropical depression. Arizonans can expect indirect flash floods caused by the remnants of tropical cyclones to occur about every two years.

Tropical cyclones in Arizona are not common, since the predominant wind pattern steers most storms that form in the Eastern Pacific either parallel or away from the Pacific coast of northwestern Mexico. As a result, most storms that could affect Arizona are carried away from the United States, with only 6% of all Pacific hurricanes entering US territory. Not all Arizona hurricanes originate from the Pacific Ocean, however; in July 2008 an Atlantic hurricane named Hurricane Dolly produced rainfall in the eastern portion of the state, and another Atlantic storm reached Arizona as a tropical depression. Many, but not all, of these systems also impacted California. (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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