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Hurricane Dean was the strongest tropical cyclone of the 2007 Atlantic hurricane season. It was the most intense North Atlantic hurricane since Hurricane Wilma of 2005 , tying for ninth overall. Additionally, it made the fourth most intense Atlantic hurricane landfall .
Hurricane Dean was one of two storms in the 2007 Atlantic hurricane season to make landfall as a Category 5 hurricane and was the seventh most intense Atlantic hurricane ever recorded, tied with Camille and Mitch. After its first landfall, Hurricane Dean crossed the Yucatán Peninsula and emerged, weakened, into the Bay of Campeche.
The effects of Hurricane Dean in Mexico were more severe than anywhere else in the storm's path. Hurricane Dean , the most intense storm of the 2007 Atlantic hurricane season, formed in the Atlantic Ocean west of Cape Verde on August 14, 2007.
The 2007 Atlantic hurricane season was the first season since 2003 to feature tropical activity both before and after the official bounds of the season. There were an above-average number of named storms during the season – 15, however many storms were weak and short-lived.
The effects of Hurricane Dean in the Greater Antilles were spread over six countries and included 20 deaths. Hurricane Dean formed in the Atlantic Ocean west of Cape Verde on August 14 as part of the 2007 Atlantic hurricane season. The Cape Verde-type hurricane tracked steadily westward into the Caribbean, where it rapidly intensified.
Another major storm to impact Jamaica was Hurricane Dean in 2007. The Category 4 storm did not make landfall but passed close enough to Jamaica to kill one person and cause $300 million USD in ...
The November 1932 Cuba hurricane and Hurricane Irma in 2007 spent the longest combined time at Category 5 strength at 78 and 77 hours, respectively, according to the National Oceanic and ...
The 2007 Atlantic hurricane season was an event in the annual tropical cyclone season in the north Atlantic Ocean. A near average Atlantic hurricane season, [nb 1] September had a record-tying eight storms, although the strength and duration of most of the storms was low. [2]