1964 Atlantic hurricane season
Approaching the east coast of Florida, Dora's motion became erratic, making a few cyclonic loops. Around 04:00 UTC on September 10, the hurricane made landfall near St. Augustine, Florida, with winds of . Two hours later, Dora weakened to a Category 2 hurricane. However, deterioration then slowed, with the hurricane falling to tropical storm intensity on September 11. Dora then briefly drifted over southwestern Georgia, until turned east-northeastward late the next day. Early on September 14, the storm re-emerged into the Atlantic Ocean near Cape Hatteras, North Carolina, and became extratropical several hours later. The remnants of Dora moved rapidly northeastward and dissipated offshore Newfoundland early on September 16.
2012 Atlantic hurricane season
Tropical Storm Debby dropped immense amounts of precipitation near its path. Rainfall peaked at in Curtis Mill, Florida, located in southwestern Wakulla County. The Sopchoppy River, which reached its record height, flooded at least 400 structures in Wakulla County. Additionally, the Suwannee River reached its highest level since Hurricane Dora in 1964. Further south in Pasco County, the Anclote River and Pithlachascotee River overflowed, flooding communities with "head deep" water and causing damage to 106 homes. An additional 587 homes were inundated after the Black Creek overflowed in Clay County. Several roads and highways in North Florida were left impassable, Interstate 10 and U.S. Route 90. Coastal flooding also inundated U.S. Routes 19 and 98. In Central and South Florida, damage was primarily caused by tornadoes, one of which caused a fatality. Overall, Debby resulted in at least $210 million in losses and 10 deaths, 8 in Florida and one each in Alabama and South Carolina.
A tropical wave developed into Tropical Depression Five on August 1, while located about 810 miles (1,305 km) east of the Lesser Antilles. Wind shear initially caused the depression to remain weak, though by August 2, it was upgraded to Tropical Storm Ernesto. The next day, Ernesto entered the Caribbean Sea. As the storm approached the western Caribbean on August 5, wind shear and dry air briefly halted strengthening; convection diminished, exposing the low-level circulation, which had become somewhat less defined. After the wind shear and dry air decreased, Ernesto regained deep convection and became a hurricane on August 6. Early on August 8, it made landfall in Costa Maya, Quintana Roo as with winds of 100 mph (160 km/h). A few hours later, a minimum barometric pressure of 973 mbar (28.7 inHg) was recorded. After weakening to a tropical storm and moving into the Bay of Campeche, the storm struck Coatzacoalcos, Veracruz on August 9. It weakened over Mexico and dissipated on August 10. The remnants contributed to the development of Tropical Storm Hector in the eastern Pacific.