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1903 Jamaica hurricane

Category 3 Atlantic hurricane in 1903

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In Martinique, hundreds of homes were deroofed in Fort-de-France, while about 5,000 people were left homeless in the villages of Fond, Fourniols, La Haye, Recluce, and Tivoli, all of which were established after the eruption of Mount Pelée in 1902. The hurricane also left extensive damage to crops and eight fatalities. In Jamaica, several communities were completely or nearly destroyed, including Manchioneal, Port Antonio, and Port Maria. Thousands of homes also suffered damage in the capital city of Kingston. Banana crops were devastated so severely that many growers were forced into bankruptcy. Numerous ships were wrecked, particularly on the north coast of the island. There were at least 65 deaths and about $10 million (1903 USD) in damage. In the Cayman Islands, more than 200 houses and seven of eight churches on Grand Cayman were destroyed or heavily damaged. Of the 23 ships in the harbor, only the Governor Blake survived. Most of the crews on board those ships were reported killed, but loss of life onshore was minimal. The storm also caused heavy damage on the Yucatán Peninsula. Many ships were wrecked and communications were cut off in several places. In the Tampico area, there was considerable damage to the port and many ships were sunk or driven ashore. Much of the land between Tampico and Cárdenas in San Luis Potosí was submerged due to flooding. In all, the storm is believed to have killed at least 149 people.

Meteorological history

A tropical storm was first observed by a ship about 835 mi (1,345 km) northeast of Cayenne, French Guiana, early on August 6, according to historic weather maps. However, the scarcity of observations means that its genesis may have occurred earlier than this time and been undetected operationally. With initial winds of 60 mph (95 km/h), the system moved generally west-northwestward and strengthened into Category 1 hurricane on the modern day Saffir–Simpson hurricane wind scale about 24 hours later. The first indication of the storm to the east of Barbados was on August 8 via telegraph reports. Early on August 9, the cyclone struck Martinique as either a strong Category 1 or a weak Category 2 hurricane. The storm entered the Caribbean shortly thereafter. Around 12:00 UTC, the cyclone intensified into a Category 3 hurricane, becoming the first major hurricane in the Atlantic basin since the second storm of 1900 and the first in the Caribbean since the 1899 San Ciriaco hurricane.

After 06:00 UTC on August 11, the cyclone struck Jamaica near Morant Point with winds of 120 mph (195 km/h). At 06:00 UTC on August 12, while brushing Grand Cayman, the hurricane peaked with maximum sustained winds of the same intensity and a minimum barometric pressure of 958 mbar (28.3 inHg), observed by the Governor Blake. The system weakened to a Category 2 around the time of landfall near Playa del Carmen, Quintana Roo, early on August 13, with winds of 100 mph (160 km/h). By 12:00 UTC, the storm further weakened to a Category 1, based on the Empirical Inland Wind Decay Model. After crossing the Yucatán Peninsula and emerging into the Gulf of Mexico early on August 14, the hurricane failed to re-strengthen. Around 00:00 UTC on August 16, it made landfall north of Tampico, Tamaulipas, with winds of 80 mph (130 km/h). The hurricane soon weakened to a tropical storm and dissipated over San Luis Potosí late on August 16.

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