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Hurricane Allen

Category 5 Atlantic hurricane in 1980

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The VISSR instrument onboard the NOAA SMS-2 satellite captured this visible image of Hurricane Allen on August 7, 1980, at 22:00 UTC (18:00 EDT). At the time this image was captured, Allen was a Categ
The National Oceanic and Atmospheric Administration (NOAA) · Public domain

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Through Atmospheric pressure, Atlantic Ocean and Western Hemisphere

Throughout its track, Allen moved through the deep tropics on a westward to northwestward course across the tropical Atlantic Ocean, Caribbean Sea, and Gulf of Mexico before making its final landfall near the United States–Mexico border. At peak strength, the hurricane passed near Haiti, causing hundreds of deaths and heavy damage. After crossing the Gulf of Mexico, Allen weakened as it struck the lower Texas coast, causing high winds, a significant storm surge, and heavy rainfall, which resulted in considerable damage to South Texas. Overall, Allen killed at least 281 people and left $1.57 billion in damages (1980 US dollars), mostly in Haiti and the United States. Due to the hurricane's impact, the name Allen was retired from the six-year revolving list of Atlantic tropical cyclone names in 1981 and replaced by Andrew. The remnants of the storm caused a brief lapse in the heat wave of 1980 in places like Dallas/Fort Worth, Texas, which had recorded 69 days of 100 °F (38 °C) heat.

Meteorological history

Allen was an early-season Cape Verde-type hurricane, originating from a tropical wave that left the African coastline on July 30. The system developed quickly as it moved westward, becoming a tropical depression the following day. However, the National Hurricane Center did not initiate advisories on Allen until almost 24 hours later, when it was centered 1,300 mi (2,100 km) east of the Windward Islands. Early on August 2, as the depression moved quickly westward towards the Caribbean, it intensified into the first named storm of the 1980 Atlantic hurricane season. Allen rapidly strengthened as it continued westward. By the time an aircraft reconnaissance plane entered the tropical cyclone's center late on August 3, it had already achieved major hurricane status, with maximum sustained winds of 125 mph (200 km/h) and a minimum central pressure of 967 mbar (28.6 inHg), making Allen a Category 3 hurricane. The storm's central pressure dropped to 951 mbar (28.1 inHg) that night as its eye passed north of Barbados on August 4.

Allen continued to move quickly westward and entered the Caribbean Sea shortly after passing south of St. Lucia. Allen's rapid intensification continued during this time, as it was steered by a mid- to upper-level ridge to its north. Shortly before 0000 UTC on August 5, the hurricane's minimum pressure decreased to 924 mbar (924 hPa; 27.3 inHg), which was noted as equivalent to Hurricane David in the previous season. Another reconnaissance aircraft shortly thereafter discovered Allen had become an extremely strong Category 5 hurricane, with sustained winds of 180 mph (290 km/h) and a minimum pressure of 911 mbar (26.9 inHg) the following day. This was the lowest central pressure ever recorded in the eastern Caribbean Sea. Allen maintained its extreme intensity for most of the day. However, late on August 5, the storm began to weaken as it underwent an eyewall replacement cycle and interacted with the mountainous terrain of Hispaniola, with the storm taking a northwestward jog south of the island, a common track deviation for most hurricanes that have passed through the area.

Allen resumed a more westward course as it left behind Hispaniola and passed north of Jamaica and the Cayman Islands on August 6. The very warm waters of the northwestern Caribbean Sea allowed the storm to begin another phase of rapid intensification. Allen reached its second and greatest peak intensity on the afternoon of August 7, with maximum sustained winds of 190 mph (305 km/h) and a minimum barometric pressure of 899 mbar (26.5 inHg). This makes Allen tied with Hurricane Melissa for the highest maximum sustained winds ever recorded in an Atlantic hurricane. Its minimum pressure of 899 millibars was the second-lowest pressure on record for the basin at the time. The major hurricane was also very large at this time, with hurricane-force winds extending 144 mi (232 km) from its center and tropical-storm-force winds extending 345 miles. Allen's circulation filled nearly the entire Gulf of Mexico, and was regarded at the time as the second-largest Atlantic hurricane on record, after 1961's Hurricane Carla. Continuing westward, the southern portion of Allen's circulation passed over the Yucatán Peninsula, causing the cyclone to weaken again. Allen bottomed out with winds of 130 mph (210 km/h) on August 8. Continued movement west over the warm waters of the Gulf of Mexico allowed Allen to restrengthen into a Category 5 hurricane for a third time as it moved over the open waters of the Gulf. The hurricane's central pressure dropped back to a tertiary low of 909 mbar (909 hPa; 26.8 inHg). Pressure falls over the southern United States at this time indicated Allen would soon slow its forward motion as it approached Texas. Allen's forward speed slowed considerably in the hours before it made landfall near Brownsville as a low-end Category 3 major hurricane on August 10. The storm rapidly weakened as it moved inland, eventually dissipating over the mountainous terrain of northern Mexico the following day.

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