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1949 Florida hurricane

Category 4 Atlantic hurricane in 1949

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Through Gulf Stream and Atmospheric pressure

The hurricane produced strong winds in the Bahamas, including a wind gust of 120 mph (190 km/h) on Bimini. A wide expanse of the east coast of Florida, stretching from Miami Beach to St. Augustine, observed hurricane-force winds, while much of the state recorded winds of at least 50 mph (80 km/h). Closer to the location of landfall, the Lake Worth Inlet observed a sustained wind speeds of 127 mph (204 km/h). Palm Beach County was one of the worst impacted areas, with 65 homes destroyed and 13,283 others damaged to some degree. Just to the north, Martin County also received extensive impact, with severe damage inflicted to about 40% of homes and commercial buildings in Stuart, where winds gusted to 160 mph (260 km/h) prior to the worst conditions. The storm generated the most severe impacts observed on Lake Okeechobee since the 1928 Okeechobee hurricane, but unlike the latter storm, did not manage to breach the local levees. Overall, the hurricane damaged about 18,000 homes, while roughly 1,000 other structures suffered severe damage or destruction in Florida. About $45 million in damage occurred in the state, which included $20 million in damage to crops, $18 million to property, $4 million electrical and communications, and $500,000 to road infrastructure.

Damage throughout the United States totaled about $52.35 million and three deaths occurred, two in Florida and one in Georgia.

Meteorological history

At 06:00 UTC on August 23, a moderate tropical storm developed about 200 mi (320 km) east of Sint Maarten. (Operationally, the system was treated as an easterly wave until it moved through the Bahamas a few days later. The system likely originated near the Cape Verde islands, but was first observed near the Leeward Islands.) The cyclone steadily tracked west-northwestward and intensified over the succeeding three days. At 12:00 UTC on August 24, while situated north of San Juan, Puerto Rico, the tropical storm strengthened to a minimal hurricane with maximum sustained winds of 75 mph (121 km/h). Subsequently, it organized rapidly, and was "well developed" when it passed near Nassau on the morning of August 26—at that time bearing winds of 115 mph (185 km/h), equivalent to a major hurricane on the Saffir–Simpson scale.

Later on August 26, the storm strengthened further over the Gulf Stream, and its eye made landfall on the city of Lake Worth, Florida, at 23:00 UTC. At that time, the storm was equivalent to a Category 4 hurricane with winds of 130 mph (210 km/h). Nearby, an airport in West Palm Beach registered calm conditions and a barometric pressure of 28.17 inHg (954 mb). (Prior to reanalysis, the system was designated as a Category 3 hurricane, based on the minimum central pressure reading, which corresponded to Category 3 on the Saffir–Simpson scale. However, modern analysis applies Saffir–Simpson rankings based on maximum sustained wind speeds.) Because the eye was first encountered in Delray Beach, a short distance southward of the landfall location, the storm earned the moniker Delray Beach hurricane.

Once inland over South Florida, the hurricane moved over the northern portion of Lake Okeechobee, following a similar path to that of the 1928 Okeechobee hurricane. On August 27, the hurricane recurved over the Florida peninsula, and then weakened to a Category 1 hurricane northeast of Tampa. The system diminished to a tropical storm near Cedar Key, and entered southern Georgia during the morning of August 28. The system passed over the Carolinas as a weak tropical storm, and was operationally noted as a "weak disturbance" at the time. The cyclone passed through the Mid-Atlantic states and New England on August 29, became extratropical over New Hampshire, and was last detected over the North Atlantic Ocean near Ireland on September 1.

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