attained Category 5 status on the Saffir–Simpson hurricane scale, reaching peak winds of 175 mph (280 km/h) a short distance off Eleuthera island in the Bahamas at 18:00 UTC. Despite its intensity, Andrew was a small tropical cyclone, with winds of extending out only about 90 mi (150 km) from the center. After reaching that intensity, the hurricane underwent an eyewall replacement cycle. At 21:00 UTC on August 23, Andrew made landfall on Eleuthera as a Category 5 hurricane, with winds of . The cyclone weakened further while crossing the Bahama Banks, and at 01:00 UTC on August 24, Andrew hit the southern Berry Islands of the Bahamas as a Category 4 hurricane, with winds of . As it crossed over the warm waters of the Gulf Stream, the hurricane rapidly re-intensified as the eye decreased in size and its eyewall convection deepened. At 08:40 UTC on August 24, Andrew struck Elliott Key as a Category 5 hurricane, with winds of and a pressure of . About 25 minutes after its first Florida landfall, Andrew made another landfall just northeast of Homestead, with a slightly lower pressure of . This barometric pressure made Andrew the most intense hurricane to strike the United States since Hurricane Camille in 1969 and the strongest tropical cyclone to make landfall in Florida since the Labor Day hurricane of 1935. The United States would not experience another landfall from a hurricane at Category 5 intensity until Hurricane Michael in 2018. As the eye moved onshore in Florida, the convection in the eyewall strengthened due to increased convergence, and Hurricane Hunters reported a warmer eyewall temperature than two hours prior. However, Andrew weakened as it continued further inland, and after crossing southern Florida in four hours, the storm emerged into the Gulf of Mexico with winds of 130 mph (210 km/h). In the Gulf of Mexico, the eye remained well-defined as the hurricane turned to the west-northwest, a change due to the weakening of the ridge to its north. Andrew steadily re-intensified over the Gulf of Mexico, reaching winds of 145 mph (235 km/h) late on August 25. As the high pressure system to its north weakened, a strong mid-latitude trough approached the area from the northwest. This caused the hurricane to decelerate to the northwest, and winds decreased as Andrew approached the Gulf Coast of the United States. At 08:30 UTC on August 26, the