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Hurricane Alicia

Category 3 Atlantic hurricane in 1983

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Alicia was the first hurricane to make landfall on the United States since Hurricane Allen struck South Texas in August 1980 over three years prior, ending the longest period of the twentieth century without a landfalling hurricane on the U.S. coast. Alicia's approach precipitated the evacuation of 60–80 thousand people from coastal communities along the coasts of Southeast Texas and Louisiana. Along the coast, a 12 ft (3.7 m) storm tide flooded communities, with the rough surf sinking several ships and resulting in three offshore fatalities. Most of the damage attributed to the storm was caused by strong winds estimated to have peaked at 130 mph (210 km/h) in southwestern Galveston Island. Alicia was the first major hurricane to form in the Gulf of Mexico since Hurricane Anita of 1977.

Widespread damage was wrought in Galveston and Houston, where thousands of homes were destroyed. In Downtown Houston, nearly all skyscrapers saw the loss of approximately half of lower-level windows, littering the urban streets with debris. Widespread power outages and flooding impacted much of Southeast Texas, with observed rainfall totals peaking at 9.95 in (253 mm). In addition to the strong winds, rough surf, and heavy rain, Alicia also generated 22 tornadoes centered around the Houston–Galveston area; most were rated F0, but the strongest, rated F2, tore through Corsicana further north.

The impacts of Alicia tapered inland past the point of landfall, though the weakening system still produced damaging winds and flooding in the Dallas–Fort Worth metroplex and Oklahoma; light rain associated with Alicia was observed as far north as Michigan. In total, Alicia caused 21 fatalities and 7,288 injuries.

Meteorological history

The origin of Hurricane Alicia can be traced to a frontal boundary that extended from New England to the Gulf of Mexico. This weak front was initially stationary over the Southeastern United States but moved slowly southward into the north-central and northeastern fringes of the gulf, producing strong convective activity beginning on the night of August 13, 1983. On August 14, a small area of low pressure developed on the western end of the front and moved off the coasts of Mississippi and Alabama, intensifying as it progressed further into the open gulf waters. The thunderstorms associated with the small low-pressure area—described as a mesoscale convective complex—aided in the development of additional storms in the northern Gulf of Mexico by facilitating favorable conditions for convective initiation. By the evening of August 14, the disturbance had largely separated from the parent frontal trough and continued to organize around a surface-level circulation. A United States Air Force reconnaissance aircraft investigated the precursor system and determined that it had developed into a tropical depression at 12:00 UTC (7:00 a.m. CDT) on August 15 while 160 mi (260 km) south of New Orleans, Louisiana. Within six hours of developing, the disturbance intensified further into a tropical storm, attaining the name Alicia and becoming the hurricane season's first named storm. Due to Alicia's formation in a region with high environmental pressures, the storm remained relatively small throughout its lifetime. The presence of a ridge of high pressure to Alicia's north steered the nascent tropical cyclone slowly westward in the early part of its development. The ridge eventually drifted eastward, resulting in Alicia slowly curving towards the northwest beginning mid-day on August 16.

The storm's slow movement—averaging just 5 mph (8 km/h)—and lack of strong steering currents allowed Alicia to reap highly favorable conditions characterized by warm sea surface temperatures in excess of 84 °F (29 °C) and favorable winds in the upper troposphere due to an upper-level anticyclone, resulting in unabated intensification until landfall. Radar analyses indicated that Alicia was stationary at times as it transitioned to a northwesterly heading. An eye began to emerge on satellite imagery by the afternoon of August 16. On August 17, Alicia strengthened into a hurricane with its pressure falling at a steady 1 mbar (hPa; 0.03 inHg) per hour. At 06:00 UTC (1:00 a.m. CDT) on August 18, Alicia became a major hurricane and made landfall an hour later on Galveston Island—25 mi (40 km) southwest of Galveston, Texas—with maximum sustained winds of 115 mph (185 km/h) and a minimum barometric pressure of 962 mbar (hPa; 28.41 inHg) as measured by aircraft reconnaissance, making it a low-end Category 3 on the Saffir–Simpson hurricane wind scale. Alicia was the first hurricane to strike the continental United States since Hurricane Allen moved ashore South Texas in August 1980, ending the longest break in contiguous U.S. hurricane landfalls of the 20th century. The hurricane was also the first major hurricane to impact the Greater Houston area since Hurricane Carla in 1961.

Alicia weakened as it accelerated northwest into the Texas interior, with the hurricane's center passing just west of Downtown Houston on the morning of August 18 as a Category 1 hurricane; the storm was initially slow to weaken as it was able to rein in moist air from the warm Gulf of Mexico. Later that day, the continued inhibitory impacts of friction and dry air weakened Alicia to a tropical storm near College Station, Texas, and degenerated into a tropical depression early on August 19 near the Dallas–Fort Worth metroplex. Despite having remained over land for 36 hours, Alicia remained well-organized while tracking into Oklahoma on August 20. The tapering system transitioned into an extratropical cyclone later that day; these remnants persisted for another day before they were absorbed by a passing trough over eastern Nebraska on August 21.

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