Hurricane Belt

The hurricane belt is an area in the Atlantic Ocean, including the Caribbean Sea and Gulf of Mexico, which is prone to hurricanes during the Atlantic hurricane season. The only inhabited Caribbean islands not in the hurricane belt are Barbados, Grenada, Bocas del Toro, Trinidad and Tobago, Bonaire, Curaçao, Aruba, Providencia Island, San Andrés, and the islands off Venezuela (although they do occasionally get impacted as well).

According to an Azores High hypothesis of geographer Kam-biu Liu, an anti-phase pattern is expected to exist between the Gulf of Mexico coast and the North American Atlantic coast. During the quiescent periods (3000–1400 BCE, and 1000 CE to present), a more northeasterly position of the Azores High would result in more hurricanes being steered towards the Atlantic coast. During the hyperactive period (1400 BCE to 1000 CE), more hurricanes were steered towards the Gulf coast as the Azores High was shifted to a more southwesterly position near the Caribbean. Such a displacement of the Azores High is consistent with paleoclimatic evidence that shows an abrupt onset of a drier climate in Haiti around 3200 years BP, and a change towards more humid conditions in the Great Plains during the late-Holocene as more moisture was pumped up the Mississippi Valley through the Gulf coast. Preliminary data from the northern Atlantic coast seem to support the Azores High hypothesis. A 3,000-year proxy record from a coastal lake in Cape Cod suggests that hurricane activity has increased significantly during the past 500–1,000 years, just as the Gulf coast was amid a quiescent period of the last millennium.

Famous quotes containing the words belt and/or hurricane:

    The shore is composed of a belt of smooth rounded white stones like paving-stones, excepting one or two short sand beaches, and is so steep that in many places a single leap will carry you into water over your head; and were it not for its remarkable transparency, that would be the last to be seen of its bottom till it rose on the opposite side. Some think it is bottomless.
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