Cape Verde hurricane: Difference between revisions
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{{about|a type of [[tropical cyclone]] categorized by development location|storms actually affecting the [[Cape Verde]] archipelago|List of West Africa hurricanes}} |
{{about|a type of [[tropical cyclone]] categorized by development location|storms actually affecting the [[Cape Verde]] archipelago|List of West Africa hurricanes}} |
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[[Image:Cape Verde hurricane track.jpg|thumb|right|400px|Cape Verde [[hurricane]] tracks]] |
[[Image:Cape Verde hurricane track.jpg|thumb|right|400px|Cape Verde [[hurricane]] tracks]] |
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A '''Cape Verde hurricane''' or '''Cabo Verde hurricane''' is an [[Atlantic hurricane]] that originates at low-[[latitude]] in the |
A '''Cape Verde hurricane''' or '''Cabo Verde hurricane''' is an [[Atlantic hurricane]] that originates at low-[[latitude]] in the [[tropical Atlantic]] from a [[tropical wave]] that has passed over or near the [[Cape Verde]] islands after exiting the coast of [[West Africa]]. The average [[Atlantic hurricane season]] has about two Cape Verde [[hurricanes]], which are often the largest and most intense storms of the season due to having plenty of warm open ocean over which to develop before encountering land or other factors prompting weakening. A good portion of Cape Verde storms are large, and some, such as hurricanes [[Hurricane Allen|Allen]], [[Hurricane Ivan|Ivan]], [[Hurricane Dean|Dean]], and [[Hurricane Irma|Irma]] have set various records. Most of the longest-lived [[tropical cyclone]]s in the Atlantic basin are Cape Verde hurricanes. While many move harmlessly out to sea, some move across the [[Caribbean Sea]] and into the [[Gulf of Mexico]], becoming damaging storms for [[Caribbean|Caribbean nations]], [[Central America]], [[Mexico]], [[Bermuda]], the [[United States]], and occasionally even [[Canada]]. Research projects since the 1970s have been launched to understand the formation of these storms and their movement through the [[Main Development Region]]. |
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==Origin== |
==Origin== |
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Prior to the early 1940s, the term Cape Verde hurricane referred to August and early September storms that formed to the east of the surface plotting charts in use at the time.<ref name="Dunn1960">{{cite book|title=Atlantic Hurricanes|url=https://archive.org/details/atlantichurrican0000dunn|url-access=registration|author1=Gordon E. Dunn |author2=Banner I. Miller |publisher=[[Louisiana State University Press]]|date=1960| |
Prior to the early 1940s, the term Cape Verde hurricane referred to August and early September storms that formed to the east of the surface plotting charts in use at the time.<ref name="Dunn1960">{{cite book|title=Atlantic Hurricanes|url=https://archive.org/details/atlantichurrican0000dunn|url-access=registration|author1=Gordon E. Dunn |author2=Banner I. Miller |publisher=[[Louisiana State University Press]]|date=1960|asin=B0006BM85S|page=[https://archive.org/details/atlantichurrican0000dunn/page/54 54]}}</ref> Cape Verde hurricanes typically develop from tropical waves which form in the African [[savanna]] during the [[wet season]], then move into the African [[steppe]]s. The disturbances move off the western coast of [[Africa]] and become [[tropical cyclones]] soon after moving off the coast,<ref name="A2">{{cite web|url=http://www.faqs.org/faqs/meteorology/storms-faq/part1/|title=FAQ: HURRICANES, TYPHOONS AND TROPICAL CYCLONES (Part 1 of 2) Subject: A2) What are "Cape Verde"-type hurricanes?|author=Chris Landsea|author-link=Chris Landsea|date=1997-07-18|publisher=Faqs.org|access-date=2009-10-08}}</ref> within 10 to 15 degrees latitude, or {{convert|1100|km|mi}} to {{convert|1600|km|mi}}, of the [[Cape Verde]] Islands;<ref name="Dunn1960"/> this comprises the tropical latitudes east of the [[40th meridian west]]. |
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==Research== |
==Research== |
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Twenty nations took part in the GATE research project in 1974, where [[Douglas DC-6]] aircraft examined [[tropical wave]]s which spawned Cape Verde hurricanes.<ref>{{cite web|url=http://celebrating200years.noaa.gov/magazine/50yrs_hurricane_res/image4.html|title=Feature Stories : Fifty Years of NOAA Hurricane Research|date=2007-02-01|access-date=2010-01-20|author=National Oceanic and Atmospheric Administration|author-link=National Oceanic and Atmospheric Administration|publisher=[[Department of Commerce]]}}</ref> In 2006, there was a two-month research project known as NAMMA-06 (short for NASA African Monsoon Multidisciplinary Activities)<ref>{{cite journal|title=NASA's Three Pronged Approach to Hurricane Research|author=R. K. Kakar|date=Fall 2006|publisher=[[National Oceanic and Atmospheric Administration]]|bibcode=2006AGUFM.A21H..01K}}</ref> which flew [[Douglas DC-8]]s into seedling disturbances in the eastern Atlantic which had the potential to become Cape Verde hurricanes.<ref>{{cite web|url=https://www.npr.org/templates/story/story.php?storyId=6263948|author=Jon Hamilton|title=Off Africa's Coast, a Hurricane Nursery|publisher=[[National Public Radio]]|date=2006-10-17|access-date=2010-01-20}}</ref><ref>{{cite news|url=https://www.washingtonpost.com/wp-dyn/content/article/2006/08/06/AR2006080600514.html|title=Research Team Seeking Clues to a Hurricane's Birth|author=Marc Kaufman|newspaper=[[The Washington Post]]|date=2006-08-07|access-date=2010-01-20}}</ref> |
Twenty nations took part in the GATE research project in 1974, where [[Douglas DC-6]] aircraft examined [[tropical wave]]s which spawned Cape Verde hurricanes.<ref>{{cite web|url=http://celebrating200years.noaa.gov/magazine/50yrs_hurricane_res/image4.html|title=Feature Stories : Fifty Years of NOAA Hurricane Research|date=2007-02-01|access-date=2010-01-20|author=National Oceanic and Atmospheric Administration|author-link=National Oceanic and Atmospheric Administration|publisher=[[Department of Commerce]]}}</ref> In 2006, there was a two-month research project known as NAMMA-06 (short for NASA African Monsoon Multidisciplinary Activities)<ref>{{cite journal|title=NASA's Three Pronged Approach to Hurricane Research|author=R. K. Kakar|journal=AGU Fall Meeting Abstracts|date=Fall 2006|volume=2006|publisher=[[National Oceanic and Atmospheric Administration]]|bibcode=2006AGUFM.A21H..01K}}</ref> which flew [[Douglas DC-8]]s into seedling disturbances in the eastern Atlantic which had the potential to become Cape Verde hurricanes.<ref>{{cite web|url=https://www.npr.org/templates/story/story.php?storyId=6263948|author=Jon Hamilton|title=Off Africa's Coast, a Hurricane Nursery|publisher=[[National Public Radio]]|date=2006-10-17|access-date=2010-01-20}}</ref><ref>{{cite news|url=https://www.washingtonpost.com/wp-dyn/content/article/2006/08/06/AR2006080600514.html|title=Research Team Seeking Clues to a Hurricane's Birth|author=Marc Kaufman|newspaper=[[The Washington Post]]|date=2006-08-07|access-date=2010-01-20}}</ref> |
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==See also== |
==See also== |
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Latest revision as of 22:27, 27 June 2024
A Cape Verde hurricane or Cabo Verde hurricane is an Atlantic hurricane that originates at low-latitude in the tropical Atlantic from a tropical wave that has passed over or near the Cape Verde islands after exiting the coast of West Africa. The average Atlantic hurricane season has about two Cape Verde hurricanes, which are often the largest and most intense storms of the season due to having plenty of warm open ocean over which to develop before encountering land or other factors prompting weakening. A good portion of Cape Verde storms are large, and some, such as hurricanes Allen, Ivan, Dean, and Irma have set various records. Most of the longest-lived tropical cyclones in the Atlantic basin are Cape Verde hurricanes. While many move harmlessly out to sea, some move across the Caribbean Sea and into the Gulf of Mexico, becoming damaging storms for Caribbean nations, Central America, Mexico, Bermuda, the United States, and occasionally even Canada. Research projects since the 1970s have been launched to understand the formation of these storms and their movement through the Main Development Region.
Origin
[edit]Prior to the early 1940s, the term Cape Verde hurricane referred to August and early September storms that formed to the east of the surface plotting charts in use at the time.[1] Cape Verde hurricanes typically develop from tropical waves which form in the African savanna during the wet season, then move into the African steppes. The disturbances move off the western coast of Africa and become tropical cyclones soon after moving off the coast,[2] within 10 to 15 degrees latitude, or 1,100 kilometres (680 mi) to 1,600 kilometres (990 mi), of the Cape Verde Islands;[1] this comprises the tropical latitudes east of the 40th meridian west.
Research
[edit]Twenty nations took part in the GATE research project in 1974, where Douglas DC-6 aircraft examined tropical waves which spawned Cape Verde hurricanes.[3] In 2006, there was a two-month research project known as NAMMA-06 (short for NASA African Monsoon Multidisciplinary Activities)[4] which flew Douglas DC-8s into seedling disturbances in the eastern Atlantic which had the potential to become Cape Verde hurricanes.[5][6]
See also
[edit]
References
[edit]- ^ a b Gordon E. Dunn; Banner I. Miller (1960). Atlantic Hurricanes. Louisiana State University Press. p. 54. ASIN B0006BM85S.
- ^ Chris Landsea (1997-07-18). "FAQ: HURRICANES, TYPHOONS AND TROPICAL CYCLONES (Part 1 of 2) Subject: A2) What are "Cape Verde"-type hurricanes?". Faqs.org. Retrieved 2009-10-08.
- ^ National Oceanic and Atmospheric Administration (2007-02-01). "Feature Stories : Fifty Years of NOAA Hurricane Research". Department of Commerce. Retrieved 2010-01-20.
- ^ R. K. Kakar (Fall 2006). "NASA's Three Pronged Approach to Hurricane Research". AGU Fall Meeting Abstracts. 2006. National Oceanic and Atmospheric Administration. Bibcode:2006AGUFM.A21H..01K.
- ^ Jon Hamilton (2006-10-17). "Off Africa's Coast, a Hurricane Nursery". National Public Radio. Retrieved 2010-01-20.
- ^ Marc Kaufman (2006-08-07). "Research Team Seeking Clues to a Hurricane's Birth". The Washington Post. Retrieved 2010-01-20.