1932 Cuba hurricane
|Category 5 major hurricane (SSHWS/NWS)|
|Formed||October 30, 1932|
|Dissipated||November 14, 1932|
|(Extratropical after November 13, 1932)|
1-minute sustained: 175 mph (280 km/h) |
|Lowest pressure||≤ 915 mbar (hPa); 27.02 inHg|
(Deadliest in Cuban history)
|Damage||$40 million (1932 USD)|
|Part of the 1932 Atlantic hurricane season|
The 1932 Cuba hurricane, known also as the Hurricane of Santa Cruz del Sur or the 1932 Camagüey hurricane, was the deadliest and one of the most intense tropical cyclones in Cuban history. The only Category 5 Atlantic hurricane ever recorded in November, the cyclone had a path through the Caribbean Sea atypical to most hurricanes developing late in the Atlantic hurricane season. The storm's strong winds, storm surge, and rain devastated an extensive portion of central and eastern Cuba, where the storm was considered the worst natural disaster of the 20th century. Though the effects from the hurricane were concentrated primarily on Cuba, significant effects were also felt in the Cayman Islands and the Bahamas, with lesser effects felt elsewhere.
The tropical depression that would later develop into the destructive hurricane was first located east of the Lesser Antilles on October 30, and tracked westward into the Caribbean Sea, reaching tropical storm strength the next day. Moving southwestward towards the southern portion of the Caribbean, the storm reached hurricane strength on November 2 before a period of rapid intensification ensued. On November 6, the tropical cyclone reached its maximum as a Category 5 hurricane with maximum sustained winds of 175 mph (280 km/h). Minimal weakening occurred afterwards as the storm recurved northeast, moving ashore Cuba's Camagüey Province on November 9 with winds of 150 mph (240 km/h). After traversing the island, the storm gradually weakened as it crossed the central Bahamas Islands and near Bermuda. On November 13, the system transitioned into an extratropical cyclone and dissipated the next day.
As an intensifying hurricane in the southern Caribbean Sea, the storm moved near the Netherlands Antilles and Colombia, causing widespread effects. A prolonged passage of Curacao resulted in the damaging of the harbor fortification. The storm lashed the coast of Colombia with strong winds and torrential rainfall, severely hampering the banana crop in the region and disrupting telecommunications. Several towns, particularly those near the coast, sustained significant infrastructural damage. Marked, albeit localized, damage to banana crops was also reported in Jamaica, where strong winds toppled numerous trees. In open waters, the storm's track brought it across numerous shipping lanes, largely disrupting shipping primarily in the central Caribbean and damaging several ships.
The 1932 Cuba hurricane can be traced back to a tropical depression, first identified at 06:00 UTC on October 30 by ship observations roughly 200 mi (320 km) east of Guadeloupe. Tracking generally westward, the depression crossed the Lesser Antilles the next day between Dominica and Martinique. Barometric pressures decrease to as much as 1008 mbar (hPa; 29.77 inHg) in St. Lucia confirmed the presence of a developing tropical cyclone. Shortly after traversing the islands, the disturbance strengthened to tropical storm intensity at 18:00 UTC on October 31. Concurrently as the storm was gradually intensifying, the tropical cyclone began to take an unusual course towards the southwest. On November 2, the storm intensified to hurricane status while north of the Netherlands Antilles.
Steadily strengthening, the hurricane reached Category 2 status on November 3. During the day, the storm passed approximately 50 mi (80 km) north of Punta Gallinas in Colombia, the northernmost extent of South America. However, at the same time the hurricane curved towards the west, causing the storm to move away from Colombia and Venezuela. During the next few days, the hurricane rapidly intensified, reaching major hurricane status late on November 4. The next day, the hurricane's intensity was analyzed to have been the equivalent of a modern-day Category 5 hurricane while curving northward. Although the storm was analyzed operationally to have maximized as a Category 4 hurricane, reanalysis of the hurricane indicated that the tropical cyclone was much more intense than suggested initially based on observations by the S.S. Phemius, the crew of which visually estimated winds of around 200 mph (320 km/h) at the maximum of the storm and measured unusually low pressures. Early on November 6, the hurricane peaked with maximum sustained winds estimated at 175 mph (280 km/h). During that time, the S.S. Phemius recorded a minimum barometric pressure of 915 mbar (hPa; 27.02 inHg); this measurement was the lowest documented throughout the storm's existence. As this report did not occur within the hurricane's eye, the storm's true minimum pressure may have been much less.
Pacing northward, the hurricane gradually weakened after maximum intensity on November 6 but held its Category 5 strength for 72 consecutive hours before finally dropping to Category 4 status. Due to a gradual curve towards the northeast, the hurricane tracked near Cayman Brac on November 9; a minimum barometric pressure of 939 mbar (hPa; 27.73 inHg) was documented on the island. Only slight weakening occurred before the hurricane made landfall on the Caribbean coast of Cuba's Camagüey Province at 14:00 UTC that day. At the time of landfall, the tropical cyclone was estimated to have had a minimum pressure of 918 mbar (hPa; 27.11 inHg) and maximum sustained winds of 150 mph (240 km/h), with these winds extending as far as 40 mi (65 km) from the center of the hurricane. The storm traversed Cuba in six hours before emerging into the Atlantic Ocean late on November 9, after which it began to cross the central Bahamian archipelago. At 07:00 UTC on November 10, the hurricane made a second landfall on Long Island, Bahamas with an intensity equivalent to that of a modern-day Category 3. Continuing to track northeast, the storm moved east of Bermuda two days later. On November 13, the hurricane began to interact with an extratropical cyclone centered over the Canadian Maritimes, and later weakened to tropical storm strength. The tropical cyclone later became extratropical itself before it was last noted at 18:00 UTC on November 14.
Preparations and impact
Caribbean Sea, Jamaica, and northern South America
As the hurricane moved slowly through the eastern and southern Caribbean, the rough seas and strong winds disrupted shipping routes. On November 6, the American schooner Abundance encountered the storm east of Jamaica, resulting in a destroyed rudder and a beaching on Jamaica's Morant Point. However, the ship's six crew were extracted from the disabled vessel and were transported to the United States. Although the S.S. Phemius would later return safely to port in Cuba, reports that the ship had lost its smokestack and the relaying of an SOS message prompted the United Fruit Company liner Tela to search for the initially missing ship, which failed due to poor visibility conditions. This was followed by a search operation undertaken by the USS Overton (DD-239) and USS Swan (AM-34). On November 8, the S.S. Phemius was found damaged and later towed to shore by a salvage tug. However, during the same period of time both the steamer Tacira and the freighter San Simeon were disabled after encountering the storm, requiring towing to safety. Several other ships in the immediate area were also hampered by the storm.
Some damage was reported in northern South America as the hurricane swept near the coast. In Colombia, rail telecommunications were interrupted near Santa Marta, and banana plantations in the area were believed to have suffered to some extent due to the storm's winds and rain. In Santa Marta itself, several homes were inundated and automotive traffic was hampered by the storm's effects. Docks on Santa Marta's port were also damaged. Heavy rains also washed out some railways and bridges, further disrupting the distribution of banana shipments. Elsewhere along the coast, many of Colombia's seaports were damaged by the storm's effects, while inland farms suffered extensive flood damage. Due to sparse reports from the remainder of Colombia, the extent of damage in Barranquilla remains unspecified, with other nearby towns reporting "heavy" damage. The village of Sevilla, Valle del Cauca was almost entirely destroyed. Providencia Island just off of Colombia sustained significant agricultural damage and the loss of 36 homes. To the northeast in Curacao, the passing hurricane destroyed the island harbor's fortifications. A seawall near the entrance to Sint Anna harbor suffered partial collapse, while a pontoon bridge linking both sides of the harbor was completely destroyed. In nearby Bonaire, a pier succumbed to the driving rain and rough seas.
With the hurricane threatening Jamaica, Pan American World Airways cancelled its flights servicing Kingston, Jamaica. In Jamaica, the storm's passage to the west caused intense winds as strong as 71 mph (114 km/h) to sweep across the island, destroying over 2 million trees. Although effects overall were generally minimal, some localized areas on the island experienced as much as a 50% loss of banana trees due to the storm. The cost of damage on Jamaica was US$4 million.
The storm devastated the Cayman Islands, especially Cayman Brac which was inundated by the storm surge, which was reported to be as high as 10 m (33 ft). Many homes and buildings were washed out to sea as a result of the storm and many people had to climb trees to escape the floodwaters. 110 people died on the islands; one of them was on Grand Cayman and the rest were on Cayman Brac. The ship Balboa also sank as a result of the storm.
Although no warnings were issued initially, the National Observatory of Cuba voiced concerns that the intense tropical cyclone presented a danger to Cuba, particularly Camagüey Province, as early as November 5. However, the observatory indicated that forecasting the future motion of the hurricane was difficult as the storm's intensity and previous motion was not consistent with climatology. On November 8, a hurricane warning was issued for the southeastern extent of Cuba. As a precautionary measure, shipping routes servicing ports in eastern Cuba were suspended.
The town of Santa Cruz del Sur in Camagüey Province was virtually obliterated by a massive storm surge which measured 6.5 m (21.3 ft) in height. Few buildings remained standing in the area. In that coastal town alone, a total of 2,870 people lost their lives. In total, 3,033 people died in Cuba and damage there was estimated at $40 million (1932 USD; $694.9 million today).
- List of deadliest Atlantic hurricanes
- Hurricane Flora – Stalled over eastern Cuba, causing widespread flooding and numerous deaths
- Hurricane Ike – Costliest tropical cyclone in Cuban history; traversed the length of Cuba and exacerbated impacts from preceding storms
- Hurricane Paloma – Intense November hurricane which struck the same areas of Cuba as the 1932 hurricane with lesser effects
- José Carlos Millás; Observatorio Nacional; Secretaria De Agricultura, Comercio Y Trabajo (1933). Memoria Del Huracán De Camagüey De 1932 (PDF) (Report). Havana, Cuba: United States National Oceanic and Atmospheric Administration's National Weather Service. Retrieved September 3, 2014.
- Landsea, Chris; et al. (April 2014). "Documentation of Atlantic Tropical Cyclones Changes in HURDAT". National Hurricane Center. Retrieved September 1, 2014.
- Millás, p. 1
- National Hurricane Center; Hurricane Research Division (July 6, 2016). "Atlantic hurricane best track (HURDAT version 2)". United States National Oceanic and Atmospheric Administration. Retrieved December 5, 2016.
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- Cayman Islands
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- Christopher Landsea; et al. (2003). "Hurricane Vulnerability in Latin America and The Caribbean" (PDF). NOAA. Archived (PDF) from the original on October 26, 2007. Retrieved 2007-10-15.