The Yankee hurricane of 1935 was a uncommon Class 2 hurricane that affected the Bahamas and South Florida in November. The cyclone produced winds of 60 mph (97 km/h) on Grand Bahama. On November 3, a ship reported a minimal stress of 964 mbar (28.48 inHg) north of the Abaco Islands. Staff in the Florida Keys had been transported to concentration points in Miami and Homestead. This web page was final edited on 6 October 2023, at 22:Forty nine (UTC). Douglas, Marjory Stoneman (1958). “The Florida Keys, 1935”. Rinehart and Company. On November 4, the hurricane, with most sustained winds of one hundred mph (160 km/h), made landfall north of Miami Seashore close to the present location of Bal Harbour, Florida. The cyclone turned south, beneath the influence of northerly winds from a high pressure system. The Associated Press (1935). “Hurricane Passes Over Miami”. It attained its peak depth on November 3, and it made landfall near Miami Beach on November 4. The hurricane’s unusual approach towards Florida and late arrival earned it the nickname of the Yankee Hurricane. 35 people have been handled for injuries at local hospitals. United Press (1935). “Florida Storm Swings Into Gulf”. By utilizing this site, you conform to the Phrases of Use and Privacy Policy. On November 1, the storm strengthened to a Category 1 hurricane, and it attained peak winds of eighty mph (130 km/h). The tropical cyclone temporarily threatened the Carolinas. On November 6, the tropical system weakened to a powerful tropical storm, and it turned northwest. The demise toll in Florida was low because of properly executed warnings and advisories. It strengthened to a hurricane on November 1, initially posing a risk to the Carolinas. In Fort Lauderdale, winds unroofed a number of properties, and canals overflowed. Later, the cyclone entered the Gulf of Mexico north of Cape Sable. No. 15. Piqua, Ohio. The cyclone’s wind subject remained slender, and Hatteras recorded peak gusts of forty mph (sixty four km/h). United States Nationwide Hurricane Middle. April 5, 2023. Retrieved November 19, 2024. This article incorporates text from this supply, which is in the public domain. The hurricane produced gentle rainfall in Miami that peaked at 4.04 inches (103 mm). Maritime interests within the Gulf of Mexico have been also warned, although the cyclone’s remnants remained off the west coast of Florida. Subsequently, the cyclone turned southwest. Willis E. Hurd (1935). “The Atlantic-Gulf of Mexico Hurricane of October 30 to November 8, 1935” (PDF). Gradually, instability most likely supported convective activity, and the cyclone slowly acquired tropical traits. The Piqua Day by day Name. United Press (1935). “Rescue, Survey Events Search Debris of Miami”. On November 7, the circulation turned east, and the cyclone weakened to a remnant low strain area. Building requirements were improved in the aftermath of the 1928 Okeechobee Hurricane, reducing damages in subsequent storms. On November 2, the hurricane reached its closest approach to Cape Hatteras; the middle was situated less than 145 miles (233 km) off the coast. Text is obtainable beneath the Artistic Commons Attribution-ShareAlike 4.Zero License; further terms may apply. Later, hurricane warnings have been issued from Palm Seaside to Naples. The sixth tropical cyclone and fifth hurricane of the 1935 Atlantic hurricane season, it developed 227 miles (365 km) east of Bermuda. The easterly move blew over a long fetch of open waters, thus producing low-degree convergence. 200 men were evacuated from the Snake Creek space in the higher Florida Keys. Southeastern Miami was flooded by three feet (910 mm) of water. The hurricane’s lowest central stress in Florida was recorded at 973 millibars (28.7 inHg) in Miami, Florida. The cyclone brought on 14 deaths within the islands. In South Florida, the hurricane dismantled communication strains, and “telegraph companies relayed” messages via Jacksonville and Atlanta. Retailers and residences have been “boarded up” in Nassau. The system was remoted from a large upper-stage trough that stretched from the Lesser Antilles to a low stress space near the Faroe Islands. Precipitation damaged tools at the Hollywood Seashore Lodge, the place many windows had been broken. Complete damages in Florida reached $5,500,000 within the Miami-Fort Lauderdale area. A polar ridge of high strain was situated north of Bermuda, producing anomalous easterly trades at an unusually excessive latitude. Precautionary hurricane alerts were hoisted along the Florida east coast from Titusville to Miami, and the center was anticipated to make landfall between Miami and West Palm Seaside. David A. Glenn (2005). “A Reanalysis of the 1916, 1918, 1927, 1928, and 1935 Tropical Cyclones of the North Atlantic Basin” (PDF). High waves flooded Miami Seashore. The hurricane traversed southern Florida and weakened over land. Wikipedia® is a registered trademark of the Wikimedia Basis, Inc., a non-profit organization. On November 8, the system dissipated 50 miles (eighty km) southwest of Saint Petersburg. Initially, the cyclone moved westward. Ten ft (3.Zero m) of the Miami Seaside causeway was eroded, and police halted visitors between Miami Seashore and the mainland. Winds shattered numerous plate glass home windows in Miami’s business district, whereas signs, roofing materials, and vegetation littered streets. 50 houses misplaced their roofs in Hollywood and Dania, and the oceanfront boardwalk was destroyed. The duration of hurricane-pressure winds ranged from 1-3 hours within the Abaco Islands, and 5 sponge fishing vessels were lost due to the hurricane. On October 30, The Village Resort and Spa Pattaya the system turned a tropical storm with most sustained winds of forty mph (64 km/h). 5 deaths had been reported in Florida.