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Hurricane Anna (1961)

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Through Atmospheric circulation and Atmospheric pressure

As a developing tropical cyclone over the Leeward Islands, Anna produced strong winds over Grenada, though damage was limited to some crops, trees, and telephone poles. Other islands experienced gusty winds, but no damage. Passing just north of Venezuela, the hurricane produced strong winds over the country, peaking as high as 70 mph (110 km/h). Strong winds caused widespread damage in northern Honduras. Throughout the country, at least 36 homes were destroyed and 228 were damaged. Severe damage in the Gracias a Dios Department left hundreds of people homeless. Additionally, high winds toppled approximately 5,000 coconut trees. Overall, Anna caused a fatality and $300,000 in damage (1961 USD), primarily in Central America.

Meteorological history

The origins of Hurricane Anna were likely from an easterly wave located over Africa. On July 16, Television Infrared Observation Satellite (TIROS) imagery showed a cloud mass situated about 1,020 miles (1,640 km) west-southwest of the southernmost islands of Cape Verde. The existence of an easterly wave was not confirmed by United States Navy reconnaissance aircraft and ship reports until the following day, at which time the system was located over 445 miles (716 km) east of Antigua. Although no circulation existed while the wave approached the Windward Islands, significant amounts of deep convection was associated with the system and located near the Intertropical Convergence Zone (ITCZ). Early on July 20, ship reports indicated a developing circulation between Grenada and Trinidad; squalls on the former island produced wind gusts as strong as 50 mph (80 km/h). According to HURDAT – the North Atlantic hurricane database – the system developed into Tropical Storm Anna at 0000 UTC on July 20, as confirmed by a reconnaissance aircraft flight.

Situated about 25 miles (40 km) east-northeast of Tobago with an initial wind speed of 40 mph (64 km/h), Anna immediately began to strengthen while moving slightly north of due west. The first advisory on Anna, issued at 1330 UTC on July 20, reported sustained winds of 60 mph (97 km/h). Later that day, the storm was upgraded to a hurricane after a reconnaissance aircraft reported hurricane-force winds. Anna then deepened more steadily, becoming a Category 2 hurricane early on July 21. At 1200 UTC on the next day, Anna attained its peak intensity with maximum sustained winds of 105 mph (169 km/h) and a minimum barometric pressure of 976 mbar (28.8 inHg). Early on July 23, Anna weakened to a Category 1 hurricane while approaching the northern coast of Honduras. Around 12:00 UTC on the following day, Anna made landfall in a rural area of Stann Creek District, Belize, with winds of 80 mph (130 km/h). Late on July 24, the system weakened to a tropical storm and then dissipated.

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