Recent Articles



































Cape Verde-type hurricane



         


A Cape Verde-type hurricane is a tropical cyclone that develops near the Cape Verde islands, and becomes a hurricane in the Atlantic Ocean. Each season averages about two Cape Verde-type hurricanes, which are usually the most intense storms of the season.

[Top]

Origin

Cape Verde hurricanes start as mesoscale convective complexes or MCC's. These clusters of thunderstorms develop in the Intertropical convergence zone. MCC's typically develop in the African savanna during their wet season and move into the African steppes. The disturbances move off the western coast of Africa and become tropical near the Cape Verde Islands (in August or September).

Cape Verde-type hurricanes can be very intense because they have plenty of room out in the Atlantic Ocean to develop. Some notable Cape Verde-type hurricanes include:


All of these hurricanes were at category four or five on the Saffir-Simpson Hurricane Scale at their peak intensity.

[Top]

Typical 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.

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 second longest lasting Atlantic hurricane on record, was a Cape Verde hurricane. It lasted 26 days total and was a hurricane for 13.

[Top]

See also

[Top]




  View Live Article   This article is from Wikipedia. All text is available under the terms of the GNU Free Documentation License