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.
Effects of Hurricane Andrew in The Bahamas
Hurricane Andrew first made landfall on August 23 as a Category 5 hurricane on the Saffir-Simpson scale, with winds of 260 km/h (160 mph). The hurricane struck the island of Eleuthera, which has a population of around 8,000, and is generally about 1.6 km (1 mi) in width. Prior to its arrival, the hurricane caused the coastline to recede about 3 mi (5 km), which was followed by what was described as a "mighty wall of water", or a storm surge. The Current, a small village in the northwestern portion of the island, recorded a surge of 7.2 m (25 ft). There, more than half of the houses in the village were destroyed, and the rest of the buildings sustained minor to major damage. On nearby Current Island, the hurricane destroyed 24 of the 30 houses in the village. The island's only road was heavily damaged, with parts still flooded more than a week after the storm.