page_title: Hurricane Andrew
section_title: Meteorological history
hierarchical_section_title: Hurricane Andrew / Meteorological history
caption_attribution_description: English: Track map of Hurricane Andrew of the 1992 Atlantic hurricane season. The points show the location of the storm at 6-hour intervals. The colour represents the storm's maximum sustained wind speeds as classified in the Saffir–Simpson scale (see below), and the shape of the data points represent the nature of the storm, according to the legend below. Saffir–Simpson scale Tropical depression≤38 mph≤62 km/h Category 3111–129 mph178–208 km/h Tropical storm39–73 mph63–118 km/h Category 4130–156 mph209–251 km/h Category 174–95 mph119–153 km/h Category 5≥157 mph≥252 km/h Category 296–110 mph154–177 km/h Unknown Storm type Tropical cyclone Subtropical cyclone Extratropical cyclone / Remnant low / Tropical disturbance / Monsoon depression
context_page_description: Hurricane Andrew was a powerful and destructive Category 5 Atlantic hurricane that struck the Bahamas, Florida, and Louisiana in August 1992. It is the most destructive hurricane to ever hit Florida in terms of structures damaged or destroyed, and was the costliest in financial terms until Hurricane Irma surpassed it 25 years later. It was the strongest landfalling hurricane in decades and the costliest hurricane to make landfall anywhere in the United States, until it was surpassed by Katrina in 2005. In addition, Andrew is one of only four Category 5 hurricanes to make landfall in the United States, alongside the 1935 Labor Day hurricane, Hurricane Camille in 1969, and Hurricane Michael in 2018. Andrew caused major damage in the Bahamas and Louisiana, but the greatest impact was felt in South Florida, where the storm made landfall as a Category 5 hurricane, with 1-minute sustained wind speeds as high as 165 mph and a gust as high as 174 mph. Passing directly through the city of Homestead in Dade County, Andrew stripped many homes of all but their concrete foundations.
context_section_description: A tropical wave moved off the west coast of Africa on August 14. A ridge of high pressure to its north caused the wave to move quickly westward. An area of convection developed along the wave axis to the south of the Cape Verde islands, and on August 15, meteorologists began classifying the system with the Dvorak technique. The thunderstorm activity became more concentrated, and narrow spiral rainbands began to develop around a center of circulation. It is estimated that Tropical Depression Three developed late on August 16, about 1,630 mi (2,620 km) east-southeast of Barbados. Embedded within the deep easterlies, the depression tracked west-northwestward at 20 mph (32 km/h). Initially, moderate wind shear prevented strengthening, until a decrease in shear allowed the depression to intensify into Tropical Storm Andrew at 12:00 UTC on August 17.
  By early August 18, the storm maintained convection near the center with spiral bands to its west as the winds increased to 50 mph (80 km/h). Shortly thereafter, the storm began weakening because of increased southwesterly wind shear from an upper-level low. On August 19, a Hurricane Hunters flight into the storm failed to locate a well-defined center and on the following day, a flight found that the cyclone had degenerated to the extent that only a diffuse low-level circulation center remained; observations indicated the barometric pressure rose to an unusually high 1,015 mbar (29.97 inHg). The flight indicated that Andrew maintained a vigorous circulation aloft. After the upper-level low weakened and split into a trough, the wind shear decreased over the storm. A strong high pressure system then developed over the southeastern United States, which built eastward and caused Andrew to turn to the west. Convection became more organized as upper-level outflow became better established. An eye formed, and Andrew attained hurricane status early on August 22, about 650 mi (1,050 km) east-southeast of Nassau, Bahamas. In the forecast issued six hours after becoming a hurricane, the cyclone was predicted to make landfall near Jupiter, Florida, with winds of 105 mph (170 km/h) on August 25. This underestimated both the strength and the speed of the storm, which would eventually make landfall in South Florida.
  The hurricane accelerated westward into an area of highly favorable conditions, and began to rapidly intensify late on August 22; in a 24‑hour period the atmospheric pressure dropped by 47 mbar (1.388 inHg) to a minimum of 922 mbar (27.23 inHg). On August 23, the storm 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 35 mph (56 km/h) 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 160 mph (260 km/h). 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 150 mph (240 km/h). 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 165 mph (266 km/h) and a pressure of 926 mbar (27.34 inHg). About 25 minutes after its first Florida landfall, Andrew made another landfall just northeast of Homestead, with a slightly lower pressure of 922 mbar (27.23 inHg). 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 
caption: Map plotting the track and the intensity of the storm, according to the Saffir–Simpson scale
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