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Cape Verde hurricane


Cape Verde hurricane

Hurricane Ivan was one of the lowest-tracking Atlantic hurricanes on record, remaining at or below 12N prior to the Caribbean.

A Cape Verde hurricane is an Atlantic hurricane that originates at low-latitude in the deep tropics, titularly from a tropical wave that has passed over or near the Cape Verde islands after exiting the coast of West Africa. The average 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, some setting 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.


  • Origin 1
  • Typical tracks 2
  • Significant Cape Verde hurricanes 3
  • Research 4
  • See also 5
  • References 6
  • External links 7


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 storms or tropical cyclones soon after moving off the coast,[2] within 10 to 15 degrees longitude, or 10,760 kilometres (6,690 mi) to 16,140 kilometres (10,030 mi), of the Cape Verde Islands;[1] this comprises the tropical latitudes east of the 40th meridian west. In the years since the phrase's coining, increasing detection has allowed meteorologists to determine that Cape Verde hurricanes have formed as early as July 4 (Hurricane Bertha of 1996) or as late as September 26 (Hurricane Flora).

Typical tracks

Cape Verde hurricane tracks

A Cape Verde hurricane forms from a tropical depression or tropical wave which passed through or near the Cape Verde islands, and strengthens into a named system (eventually becoming a hurricane at some point) in the mid-Atlantic. The initial track of a Cape Verde storm tends to be generally westward from Cape Verde, with a turn to the north at some stage in the track for most storms lasting more than a few days. Once the cyclone begins approaching South America, a Cape Verde hurricane can take several basic tracks and from there diverge, become extra-tropical, or dissipate.

  1. Allen (1980), on a southern track.
    It can continue to the west, and if it is far enough south, it will cross the Windward Islands into the Caribbean Sea, possibly affecting Venezuela to some degree. From there it will often continue westward into Nicaragua, Honduras, or Belize.[3] For example, Hurricane Joan–Miriam took this southerly route in 1988, causing severe flooding in South America, making landfall in Central America, and continuing into the Pacific Basin, just as Hurricane Irene–Olivia did in 1971. Rarely, a storm will make landfall in South America. Some storms pass unabated into the Gulf of Mexico. Hurricane Ivan of 2004 began with a very southerly route yet it made landfall far to the north in Alabama. Somewhere in the middle of these extremes, storms such as 1980's Hurricane Allen track toward the coast of Mexico, affecting areas from the Yucatán Peninsula to Texas. Many of these southerly hurricanes strike Jamaica, like the Galveston Hurricane of 1915 and Hurricane Gilbert of 1988. Hurricane Janet of 1955 will be remembered as one of the deadliest and strongest storms to strike the Yucatán Peninsula of Mexico.
  2. Georges (1998), on a Caribbean track.
    If the storm is further north, it may travel past the Mississippi. Slightly further north, and the storm will track through the Bahamas and into Florida in the manner of 1992's Hurricane Andrew.[3] Many of these storms passing through the center of the Caribbean will strike the islands of Hispaniola and Cuba, like Hurricane David and Hurricane Frederic did, both in 1979. Some storms on this track will turn to the west once in the Gulf, and thereby make landfall in Texas, as the Galveston Hurricane of 1900 and Hurricane Ike of 2008. Similarly, Hurricane Inez of 1966 followed a Caribbean track that took the storm into the Bahamas where it weakened, only to turn sharply west and make a final landfall in Mexico.
  3. Gloria (1985) struck the East Coast.
    A more northerly storm will often have its track affected by the high pressure that typically occurs over the eastern Atlantic in late summer. As these storms pass north of the Antilles, their tracks begin to curve to the north and to the east of the Florida Peninsula, often sending them away from land. A few storms will track northwest, making landfall in North or South Carolina. Hurricane Hugo of 1989 and Hurricane Fran of 1996 are typical examples. Occasionally storms following this track can accelerate to the north and strike New England. The New England Hurricane of 1938 and Hurricane Gloria in 1985 were two such cases.[3]
  4. Edouard (1996) grazed the East Coast.
    When a storm tracks very far north, its potential for landfall is much less. Some storms do, however, track west-northwest to strike the Atlantic coast of the U.S. and the maritime provinces of Canada, such as 1933 Chesapeake–Potomac hurricane and Hurricane Isabel of 2003, which struck the mid-Atlantic. Both Hurricane Bill (2009) and Hurricane Daisy (1962) were Cape Verde storms that made landfall in Canada, just as Hurricane Luis (1995), Hurricane Earl (2010), and Hurricane Igor (2010) did. If the storm's track is affected significantly, it will often pass near the Eastern U.S., Nova Scotia, and Newfoundland Island and curve back out to sea, where it becomes extratropical over cooler water. An example of such was Hurricane Edouard in 1996. At the extreme, Cape Verde hurricanes can track so far north as to curve all the way to Europe, such as Hurricane Katia of 2011, Hurricane Helene of 2006, Hurricane Isaac of 2000, all of which affected Ireland.

Because most Cape Verde hurricanes take a near-westward path that starts in the eastern Atlantic, they can avoid the two situations that typically end the life of a tropical cyclone: interaction with land, and movement over cool water. Since storms that far out at sea can go over a week without moving over cooler water or near a landmass, Cape Verde hurricanes are some of the longest-lived storms. Hurricane Faith, the third longest lasting Atlantic hurricane on record,[3] was a Cape Verde hurricane. It lasted 16 days total and was a hurricane for 14.[4] Hurricane Joan–Miriam of 1988 and Hurricane Irene–Olivia of 1971 lasted longer, both having crossed narrow parts of Central America and regaining cyclonic motion in the Pacific.

Significant Cape Verde hurricanes

Annular Hurricane Isabel near peak intensity. Isabel holds the record for the highest instantaneous wind speed ever recorded in an Atlantic hurricane, 233 mph (375 km/h).[5]
Year Name Category
1899 1899 Hurricane San Ciriaco 4
1900 Galveston Hurricane of 1900 4
1926 1926 Miami Hurricane 4
1928 1928 Okeechobee Hurricane 5
1938 New England Hurricane of 1938,
or the Long Island Express
1947 1947 Fort Lauderdale Hurricane 4
1957 Hurricane Carrie 4
1958 Hurricane Cleo 5
1960 Hurricane Donna 5
1963 Hurricane Flora 4
1964 Hurricane Cleo 4
1966 Hurricane Faith 3
1966 Hurricane Inez 4
1979 Hurricane David 5
1979 Hurricane Frederic 4
1980 Hurricane Allen 5
1980 Hurricane Frances 3
1985 Hurricane Gloria 4
1989 Hurricane Hugo 5
1992 Hurricane Andrew 5
1995 Hurricane Luis 4
1996 Hurricane Bertha 3
1996 Hurricane Fran 3
1998 Hurricane Georges 4
1999 Hurricane Floyd 4
2002 Hurricane Lili 4
2003 Hurricane Isabel 5
2004 Hurricane Frances 4
2004 Hurricane Ivan 5
2004 Hurricane Jeanne 3
2005 Hurricane Emily 5
2005 Hurricane Dennis 4
2007 Hurricane Dean 5
2008 Hurricane Ike 4


Twenty nations took part in the GATE research project in 1974, where Douglas DC-6 aircraft examined tropical waves which spawn Cape Verde hurricanes.[6] In 2006, there was a two-month research project known as NAMMA-06 (short for NASA African Monsoon Multidisciplinary Activities)[7] which flew Douglas DC-8's into seedling disturbances in the eastern Atlantic which had the potential to become Cape Verde hurricanes.[8][9]

See also


  1. ^ a b Gordon E. Dunn and Banner I. Miller (1960). Atlantic Hurricanes.  
  2. ^  
  3. ^ a b c d National Hurricane Center; Hurricane Research Division (May 7, 2015). "Atlantic hurricane best track (HURDAT version 2)". United States National Oceanic and Atmospheric Administration. Retrieved July 5. 
  4. ^ Colin J. McAdie, Christopher W. Landsea, Charles J. Neumann, Joan E. David, Eric S. Blake, and Gregory R. Hammer (2009). Historical Climatology Series 6-2: Tropical Cyclones of the North Atlantic Ocean, 1851–2006 (with 2007 and 2008 track maps included) (PDF). National Climatic Data Center. p. 161. Retrieved 2009-10-08. 
  5. ^ Richard J. David and Charles H. Paxton (2005). "How the Swells of Hurricane Isabel Impacted Southeast Florida" (PDF). Bulletin of the American Meteorological Society: 1065–1068.  
  6. ^  
  7. ^ R. K. Kakar (Fall 2006). "NASA's Three Pronged Approach to Hurricane Research".  
  8. ^ Jon Hamilton (2006-10-17). "Off Africa's Coast, a Hurricane Nursery".  
  9. ^ Marc Kaufman (2006-08-07). "Research Team Seeking Clues to a Hurricane's Birth".  

External links

  • NOAA AOML Hurricane Research Division definition of a Cape Verde hurricane
  • Talks about hurricanes in general and Cape Verde hurricanes
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