Tropical Storm Alma (1974)

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FormedAugust 12, 1974
DissipatedAugust 15, 1974
Highestwinds65 mph (100 km/h)
Lowestpressure1007 mbar (hPa); 29.74 inHg
Tropical Storm Alma
Tropical Storm Alma at peak intensity on August 13
Meteorological history
FormedAugust 12, 1974
DissipatedAugust 15, 1974
Tropical storm
1-minute sustained (SSHWS/NWS)
Highest winds65 mph (100 km/h)
Lowest pressure1007 mbar (hPa); 29.74 inHg
Overall effects
Fatalities51 total
Damage$5 million (1974 USD)
Areas affectedTrinidad and Tobago, Venezuela
IBTrACSEdit this at Wikidata

Part of the 1974 Atlantic hurricane season

Tropical Storm Alma, the first named storm to develop in the 1974 Atlantic hurricane season, was a short lived tropical cyclone that made a rare Venezuelan landfall. The storm formed from the Intertropical Convergence Zone (ITCZ) on August 12 well to the east of the Windward Islands, but advisories were not issued until the next day when Alma was at peak intensity. Alma entered the southeastern Caribbean Sea at an unusually brisk westward pace of between 20 mph (32 km/h) to 25 mph (40 km/h), prompting numerous watches and gale warnings throughout the nations in this region. After crossing Trinidad, Alma became one of only four tropical storms to traverse the Paria Peninsula of northeastern Venezuela. The storm dissipated on August 15 over the high terrain of Venezuela.

Alma left heavy damage in Trinidad, amounting to about US$5 million (value in 1974), making it the most destructive cyclone of the 20th century on the island at that time. Alma damaged about 5,000 buildings, leaving 500 people homeless. The storm also wrecked 17,750 acres (7,180 ha) of crop fields. There were two deaths in Trinidad, including one person who was struck by flying debris. Alma's heavy rainfall was responsible for a plane crash on Isla Margarita off the Venezuelan coast, killing the 49 people on board.

Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
triangle Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

A disturbance associated with the Intertropical Convergence Zone (ITCZ) left the coast of West Africa on August 9,[1] producing mid-level winds of 75 mph (120 km/h) in Dakar, Senegal.[2] A weak circulation formed near the sea surface on August 10 within an area of thunderstorms.[3] The disturbance moved slowly westward over the Atlantic Ocean, developing into a tropical depression at 18:00 UTC on August 12, around the 10th parallel north,[2] an unusually southern latitude the cyclone would remain around throughout its lifetime.[4] On August 13, the depression intensified into Tropical Storm Alma about 375 mi (605 km) east of Trinidad and Tobago, as indicated by a Hurricane Hunters flight reporting winds of 65 mph (105 km/h).[2] This same flight observed a circular eye with a diameter of 36 mi (58 km), the only report of an eye-like structure from this storm.[5]

The center of Alma was elongated, causing gale-force winds to extend 75 mi (120 km) to the north while extending only 25 miles (40 km) to the south.[6] On August 14 the Hurricane Hunters measured gusts of 80 mph (130 km/h); however, the storm's overall wind pattern weakened after its initial peak.[2] Alma continued westward at 23 mph (37 km/h), which National Hurricane Center (NHC) Director Neil Frank noted was unusually rapid for a tropical cyclone at this time and location.[6] Alma was able to maintain its low latitude westward movement due to a strong subtropical ridge to its north, which was at an unseasonably low latitude for the month of August.[1]

On August 14, Alma made landfall on Trinidad with winds of 55 mph (90 km/h),[7] the southernmost landfall on that island since a storm in 1933.[1] Even though the storm traversed Trinidad in only three hours,[8] its time over land was sufficient to disrupt the circulation.[9] The storm crossed the Gulf of Paria and made its second and final landfall on the Paria Peninsula of Venezuela,[8] one of only four storms on record to do so; the others were in 1605, 1725, and 1933.[10] The high mountains in Venezuela took a toll on the storm, ripping the circulation and causing Alma to be downgraded to a tropical depression on August 15.[2] At 02:00 UTC that day, Alma's circulation passed near Caracas. The convection rapidly diminished, and the storm's presence on satellite imagery faded, though the NHC noted the potential for redevelopment once it reached open waters.[11] The storm did not survive its trek over land; late on August 15, the NHC issued the final advisory after the circulation dissipated near the border of Venezuela and Colombia.[12] The remnants of Alma continued westward across South and Central America, reaching the Pacific Ocean where they would eventually restrengthen into Hurricane Joyce.[13]

Preparations, impact, and aftermath

See also

References

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