A 'Cape Verde-type hurricane' is an
Atlantic hurricane that develops near the
Cape Verde islands, off the west coast of
Africa. The average hurricane season has about two Cape Verde-type
hurricanes, which are usually the most intense storms of the season because they often have plenty of warm open ocean over which to develop before encountering land.
Origin
Cape Verde-type 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 near the Cape Verde Islands, usually in August or September.
Typical tracks

Cape Verde-type hurricane tracks
A typical Cape Verde hurricane will form as a tropical depression just south of the Cape Verde islands. They normally reach hurricane strength in the mid-Atlantic, but sometimes will strengthen closer to Cape Verde or the Caribbean.
Once it begins approaching North America, a Cape Verde hurricane has several basic tracks.
★ It can continue to the west, and if it is far enough south, it will cross the
Lesser Antilles into the
Caribbean Sea. From there it will often continue westward into
Nicaragua,
Honduras, or
Belize.
★ If the storm is further north, it can travel up the
Greater Antilles and into the
U.S. Gulf Coast. In 1998,
Hurricane Georges took a track of this nature. Slightly further north, and the storm will track through the
Bahamas and into
Florida in the manner of 1992's
Hurricane Andrew.
★ A more northerly storm will begin to have its track affected by the high pressure that generally occurs over the eastern Atlantic in late summer. As these storms pass north of the Antilles, their tracks begin to curve to the north. Often this results in the storms making landfall in
North or
South Carolina.
Hurricane Hugo was a typical example. If the storm's track is affected significantly, it will often curve back out to sea, where it becomes extratropical over cooler water. An example of such was
Hurricane Edouard in
1996.
★ Sometimes, the subtropical ridge is farther west than usual such that the storm is driven around the east side of the ridge in the central Atlantic, generally missing land completely. An example of such was
Hurricane Danielle in
2004.
Note that while these tracks are typical, Cape Verde hurricanes are not bound to follow them and often do not.
Because this type of hurricane takes 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 they can go for several weeks without having either affect them, Cape Verde-type hurricanes are some of the longest-lived storms.
Hurricane Faith, the third longest lasting Atlantic hurricane on record, was a Cape Verde hurricane. It lasted 16 days total and was a hurricane for 13.
Major Cape Verde-type hurricanes
The category is the peak intensity of the hurricane, measured on the
Saffir-Simpson Hurricane Scale
See also
★
List of Atlantic hurricane seasons
★
List of notable tropical cyclones
External links
★
NOAA AOML Hurricane Research Division definition of a Cape Verde-type hurricane
★
Talks about hurricanes in general and Cape Verde hurricanes