The 1949 Florida hurricane was the second recorded storm and the strongest and most intense tropical cyclone of the 1949 Atlantic hurricane season. It was the most intense tropical cyclone to affect the United States during the season, with a minimum central pressure of 954 mbar (28.18 inHg) at landfall. The cyclone originated from an easterly wave near the Leeward Islands, and it rapidly intensified to a hurricane near the Bahamas. It strengthened to a major hurricane northwest of Nassau, Bahamas, and it struck West Palm Beach, Florida as a Category 4 hurricane with maximum sustained winds near 130 mph (210 km/h) and peak gusts near 160 mph (260 km/h) above the surface. It turned north over the Florida peninsula, and it transitioned to an extratropical low pressure area over New England.