Hurricane Andrew
Post-analysis on Andrew revealed that the storm was often stronger than operationally reported between early on August 22 and early on August 26. In real time, the National Hurricane Center assessed its peak intensity as , which was upgraded to 155 mph (250 km/h) in a post-storm analysis after the season ended. However, a 2004 paper by Christopher Landsea and others concluded that Andrew became a Category 5 hurricane near the Bahamas on August 23 and reached maximum sustained winds of 175 mph (280 km/h). The paper also indicated that Andrew briefly re-intensified into a Category 5 hurricane around the time of landfall in South Florida early on August 24. The storm was found to have been slightly stronger while approaching Louisiana, but the landfall winds were decreased from 120 mph (195 km/h) to 115 mph (185 km/h).
1986 Atlantic hurricane season
While active, Andrew posed a threat to the Carolinas. Gale warnings were posted from an area ranging from Cape Lookout to south of Virginia Beach, Virginia on June 7. Waves reached heights of off the coast of the Carolinas, which killed a person on Ocracoke Island. Three companions were also swept out, all of whom made it back to shore. At Wrightsville Beach and Carolina Beach, at least 40 swimmers were caught in the currents, four of whom were hospitalized. The precursor to the storm produced heavy rainfall across Jamaica that caused a deadly flood event.
During late June, a frontal trough drifted into the northeastern Gulf of Mexico, and by June 22 a surface circulation formed. Tracking west-northwestward, it developed into Tropical Depression Two on June 23 while located about 330 miles (535 km) south of Pensacola, Florida. The next day, it attained tropical storm status, and with continued favorable conditions attained hurricane status on June 25 to the south of Louisiana. Bonnie turned to the northwest and made landfall near Sea Rim State Park in Texas. The storm quickly weakened over land as it turned to the north and northeast, and on June 28 it was absorbed by an approaching frontal zone in southeastern Missouri.