Tropical Storm Vamei near the equator in December 2001
Typically, tropical cyclones form at least 5.0 degrees of latitude north and south of the equator , or at least 300 nautical miles (556 km , 345 mi ) of the equator. Despite the presence of sufficiently warm sea surface temperatures and generally low wind shear , tropical cyclogenesis is uncommon at these latitudes, due to a lack of the Coriolis force , which causes cyclones to spin. On rare occasions, tropical cyclones can develop within 5º of the equator, though it is more prevalent in the northwestern Pacific Ocean .
Background
For centuries, sailors haven't worried about tropical storms near the equator. It's a rule that cyclones are not supposed to develop there.
Various factors converge to produce a tropical cyclone, including sufficiently warm sea surface temperatures , low wind shear , ample moisture, and enough atmospheric instability to produce thunderstorms. In addition, weather disturbances typically need to be far enough away from the equator to spin, known as vorticity . This is due to increasing Coriolis force closer to the poles, and which is zero at the equator.[ 2] [ 3] [ 4] One associated phenomenon often seen with low-latitude cyclones is the equatorial westerly wind burst , which allows for sufficient shear vorticity on both sides of the equator to support tropical cyclogenesis.[ 5] Westerly wind bursts are typically the most common in the equatorial Western Pacific Ocean.[ 6]
List
Satellite image of Cyclone Agni in October 2004 in its formative stage near the equator
Note: Only systems that were of tropical depression strength or higher within 5.0 degrees of the equator are included.
See also
References
^ "Breaking the Typhoon Rules" . Jet Propultion Laboratory. Retrieved March 31, 2024 .
^ "Tropical Cyclone Introduction" . National Oceanic and Atmospheric Administration. September 8, 2023. Retrieved March 31, 2024 .
^ "Tropical Cyclone Introduction" . National Weather Service. Retrieved 23 April 2023 .
^ Chun-yuen, Chau. "Why do Tropical Cyclones always Form more than 5 degrees of Latitude away from the Equator?" . Hong Kong Observatory. Retrieved 23 April 2023 .
^ "Linkage Between Westerly Wind Bursts and Tropical Cyclones" . American Geophysical Union. October 10, 2018. Retrieved May 21, 2024 .
^ "Generation of westerly wind bursts by forcing outside the tropics" . Nature.com. January 13, 2021. Retrieved May 21, 2024 .
^ "2001 VAMEI (2001361N01106)" . The International Best Track Archive for Climate Stewardship (IBTrACS). Retrieved 19 May 2017 .
^ Report on Cyclonic Disturbances Over North Indian Ocean During 2004 (PDF) (Report). India Meteorological Department. January 2005. Retrieved 2015-05-24 .
^ "1956 01W:SARAH (1956081N02154)" . The International Best Track Archive for Climate Stewardship (IBTrACS). Retrieved 19 May 2017 .
^ "1979 ALICE (1978361N02180)" . The International Best Track Archive for Climate Stewardship (IBTrACS). Retrieved 19 May 2017 .
^ "2014 PEIPAH (2014093N02148)" . The International Best Track Archive for Climate Stewardship (IBTrACS). Retrieved 19 May 2017 .
^ "WWJP27 RJTD 040600" . Japan Meteorological Agency. 4 March 2023. Archived from the original on 4 March 2023. Retrieved 4 March 2023 .
^ "TROPICAL CYCLONE REPORT - TROPICAL DEPRESSION NINE-C" (PDF) . Central Pacific Hurricane Center . 22 December 2016. Archived from the original (PDF) on 25 March 2024. Retrieved 25 March 2024 .
^ "1977 PATSY (1977082N03165)" . The International Best Track Archive for Climate Stewardship (IBTrACS). Retrieved 19 May 2017 .
^ "2002 Moderate Tropical Storm Abaimba (2002247S03067)" . International Best Track Archive for Climate Stewardship. Retrieved April 2, 2024 .
^ "TROPICAL CYCLONE REPORT - HURRICANE PALI" (PDF) . Central Pacific Hurricane Center . 13 December 2018. Archived from the original (PDF) on 26 January 2019. Retrieved 26 January 2019 .
^ "Extremely Severe Cyclonic Storm "FANI" over eastcentral equatorial Indian Ocean and adjoining southeast Bay of Bengal (26 April – 04 May, 2019): Summary" (PDF) . India Meteorological Department. Retrieved May 17, 2024 .
^ "Best Track Data on Very Intense Tropical Cyclone Fabien (10)" . Météo-France . Retrieved 25 March 2024 .
^ "1959 HARRIET (1959356N05152)" . The International Best Track Archive for Climate Stewardship (IBTrACS). Retrieved 19 May 2017 .
^ "CYCLONE AND CYCLONIC ACTIVITY LA REUNION" . 22 May 2024. Archived from the original on 22 May 2024.
^ Annual Report on the Activities of the RSMC Tokyo - Typhoon Center 2012 (PDF) (Report). Japan Meteorological Agency. Retrieved April 2, 2024 .
^ WMO / ESCAP Panel on Tropical Cyclones Annual Review 2002 (PDF) (Report). World Meteorological Organization. Retrieved April 2, 2024 .
^ "1970 Super Typhoon Kate (1970286N06143)" . International Best Track Archive for Climate Stewardship. Retrieved April 2, 2024 .
^ "1992 Typhoon Axel (1992003N03176)" . International Best Track Archive for Climate Stewardship. Retrieved April 2, 2024 .
^ Tropical Cyclones 1992 (PDF) (Report). Central Pacific Hurricane Center. Retrieved April 2, 2024 .
^ "1973 Severe Tropical Cyclone FLORESCYCLO (1973116S05131)" . International Best Track Archive for Climate Stewardship. Retrieved April 2, 2024 .
^ "1982 Severe Tropical Cyclone Bernie (1982091S03159)" . International Best Track Archive for Climate Stewardship. Retrieved April 2, 2024 .
^ Report on Cyclonic Disturbances Over North Indian Ocean During 2005 (PDF) (Report). India Meteorological Department. 2006. Retrieved May 17, 2024 .
^ Report on Cyclonic Disturbances Over North Indian Ocean During 2006 (PDF) (Report). India Meteorological Department. 2007. Retrieved May 21, 2024 .
External links