Coast states, with a peak total of in Avon Park, Florida. Subtropical Storm One Tropical Depression One formed over the Bay of Campeche on June 22. As shower and thunderstorm activity associated with the depression diminished, convection flared over the eastern Gulf of Mexico on June 24, while a reconnaissance aircraft flight revealed that a closed circulation had developed over the south-central Gulf of Mexico. Therefore, it is estimated that a subtropical depression formed around 18:00 UTC on June 24. Early the following day, the subtropical depression intensified into a subtropical storm. Accelerating northeastward, the subtropical storm strengthened slightly further before making landfall near Clearwater, Florida, just after 06:00 UTC with winds of 50 mph (85 km/h). Although centered over Florida, the system intensified further, peaking with winds of 65 mph (100 km/h) around 12:00 UTC on June 25. After exiting Florida, the cyclone quickly began extratropical later that day, with the remnants dissipating offshore North Carolina on June 27. Portions of Florida experienced heavy precipitation, particularly the Tampa Bay Area. A peak rainfall total of was observed at the St. Pete–Clearwater International Airport. The storm brought flooding and erosion to parts of west Central Florida. Overall, approximately $24.8 million in damage occurred in Florida, with roughly half of that total incurred to beaches, bridges, drainage systems, roads, sewers, and utilities. Three deaths were reported in the state, all due to drowning. Subtropical Storm Two A convective area of cloudiness existed northeast of the Bahamas in mid July in response to a stationary frontal boundary. On July 15, satellite imagery suggested the presence of a weak circulation within the system. Around 00:00 UTC on the following day, a subtropical depression formed about northeast of the Bahamas. Moving northeastward, the cyclone slowly strengthened, becoming a subtropical storm at about 12:00 UTC on July 17. Late on the next day, the ship Export Adventurer observed winds of and a barometric pressure of . Based on these observations, the storm peaked with maximum sustained winds of 50 mph (85 km/h) on July 18. By the next day, the cyclone began weakening. Around 00:00 UTC on July 20, the subtropical storm was absorbed a large extratropical low, which dissipated well east of Newfoundland several hours later. Subtropical Storm Three A frontal wave formed along a stationary front which ended from near Cape Hatteras northeastward. At 12:00 UTC on August 10, a subtropical storm developed