Meteorological history of Hurricane Andrew
In 2002, the "Atlantic Basin Hurricane Database Reanalysis Project" examined Hurricane Andrew and this corridor of extreme winds embedded within Andrew's northern eyewall. The project concluded that Category 5 conditions on land occurred only in a small region of southern Dade (now Miami-Dade) County, specifically close to the coast in Cutler Ridge. The remaining areas affected by Andrew's initial landfall in Florida likely experienced sustained Category 4 and 3 hurricane conditions. Andrew was officially re-classified as a Category 5 storm in 2004, and the reanalysis provided a more comprehensive and detailed examination of Andrew's wind field structure upon landfall than originally assessed in 1992.
Hurricane Earl (1998)
Around 0600 UTC (1:00 am EDT) on September 3, Hurricane Earl made landfall near Panama City, Florida with winds of 80 mph (130 km/h). Shortly after landfall, the storm weakened to a tropical storm and rapidly accelerated as it quickly underwent an extratropical transition. By this time the NHC issued their final advisory on Earl. Several hours later, Earl finished its transition and continued to rapidly track through the Southeast United States. After entering the Atlantic Ocean, the remnants of Earl began re-intensify due to the effects of a baroclinic zone. Relatively cool sea surface temperatures near Atlantic Canada prevented tropical development; however, during a 36-hour span, Earl rapidly intensified, as the central barometric pressure decreased by 40 mbar (hPa; 1.18 inHg) to 957 mbar (hPa; 28.26 inHg). By the time the system made landfall over eastern Newfoundland, sustained winds had intensified to 65 mph (100 km/h). On September 8, the remnants of Earl significantly weakened and were soon absorbed by a larger extratropical cyclone associated with the remnants of Hurricane Danielle.