Hurricane Carol was among the worst tropical cyclones to affect the New England region of the United States. It developed from a tropical wave near the Bahamas on August 25, 1954, and slowly strengthened as it moved northwestward. On August 27, Carol intensified to reach winds of 105 mph (169 km/h), but weakened as its motion turned to a northwest drift. A strong trough of low pressure turned the hurricane northeastward, and Carol intensified to attain Category 3 status on the Saffir–Simpson Hurricane Scale. The well-organized hurricane made landfall on Long Island and Connecticut on August 30 near peak intensity, and quickly became extratropical over land.
Carol was similar to the New England Hurricane of 1938, as they were near the same intensity when affecting New England, in addition to both storms accelerating toward the region. Both systems hit within 40 miles (64 km) of each other at high tide, resulting in a substantial storm surge in Narragansett Bay. At the time, Carol was the third costliest United States hurricane, and the nineteenth costliest U.S. hurricane when adjusted for inflation, as of 2004.
Read more about Hurricane Carol: Meteorological History, Impact, Aftermath
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