Hurricane Danny produced 13 significant (F2+) tornadoes in the Southern United States during August 1985, the most spawned by a tropical cyclone until Hurricane Ivan in 2004. The fourth named storm and third hurricane of the season, Danny developed from a tropical wave in the northwestern Caribbean Sea on August 12. The system moved northwestward and initially remained weak. Early on August 13, it brushed Cape San Antonio, Cuba before emerging the Gulf of Mexico later that day. The system then intensified into Tropical Storm Danny on August 14. Danny deepened further and became a hurricane early on the following day, while beginning to re-curve north-northwestward. Late on August 16, Danny attained its peak intensity with winds of 90 mph (150 km/h). Shortly thereafter, the storm made landfall near Grand Chenier, Louisiana at the same intensity. Early on August 17, Danny weakened to a tropical storm and was downgraded to a tropical depression several hours later. It moved east-northeastward across the Southeastern United States, until dissipating over southeastern Virginia on August 18. There was widespread coastal and inland flooding in Louisiana. The storm brought up to of precipitation to Kentwood. Additionally, there were two tornadoes reported in the state. Overall, 33 single-family homes and 26 mobile homes were destroyed, while three condos, 908 single-family houses and 265 mobile homes were damaged. A combination of rainfall and storm surge in southern Mississippi caused severe beach erosion and flooded 70 homes in Hancock County alone. Further north, a tornado in Enterprise severely damaged six homes, three barns, and two roofs; it also destroyed one house. In Alabama, the storm spawned 34 tornadoes, which destroyed 27 single-family residences and 18 mobile homes. About 90 homes, eight mobile homes, and 23 businesses suffered damage. Impact was similar but less severe in several other states, including Georgia, Maryland, South Carolina, Texas, and Virginia. Danny caused five fatalities and about $100 million in damage (1985 USD). Meteorological history A tropical wave emerged into the Atlantic Ocean from the west coast of Africa on July 30. The system moved westward across the Atlantic Ocean without much convection, or thunderstorms. On August 8, the wave crossed the crossing the Windward Islands and entered the Caribbean Sea, whereupon convection increased. A broad low-pressure area was evident on August 10 in the central Caribbean Sea. Two days later, a United States Air Force reconnaissance aircraft observed a poorly-defined circulation near