Hurricane Gordon was an erratic, long-lived, and catastrophic late-season hurricane in 1994. The twelfth and final tropical cyclone of the 1994 Atlantic hurricane season, Gordon formed as a tropical depression in the southwestern Caribbean on November 8. Without strengthening, the depression made landfall on Nicaragua. Later on November 10, the system began to strengthen as it tracked further from land, and it quickly strengthened into Tropical Storm Gordon, the seventh named storm that season. Gordon also made landfalls in Jamaica and Cuba while a minimal tropical storm. It entered the southwestern Atlantic while resembling a subtropical cyclone. By the time it entered the Gulf of Mexico, the storm was fully tropical again. Tropical Storm Gordon later crossed the Florida Keys, and turning to the northeast it made landfall in Fort Myers, Florida. Gordon strengthened after it re-entered the Atlantic Ocean, becoming a hurricane on November 17. It briefly threatened North Carolina while turning to the northwest, although it turned to the south and weakened. Gordon deteriorated into a tropical depression and struck Florida again at that intensity on November 20. It turned to the north and dissipated the next day over South Carolina.
Gordon first caused flooding in northern Costa Rica that destroyed 700 houses and caused $30 million in damage. There were six deaths in the country and an additional two deaths in neighboring Panama. Upon affecting Jamaica, the storm was responsible $11.8 million in damage and four deaths. Damage was heaviest in Haiti, after a prolonged southwesterly flow dropped of rainfall in a 24‑hour period. The rains resulted in extensive mudslides and flooding that disrupted transportation and damaged 10,800 houses, with another 3,500 destroyed. There were 1,122 deaths in the country, partially due to deforested hills, and damage was estimated at $50 million. In the neighboring Dominican Republic, there were five additional deaths, as well as flooding near its capital. In Cuba, Gordon caused $100 million in damage, and 5,906 houses were damaged or destroyed. Due to large-scale evacuations, there were only two deaths in the country. In Florida, the storm caused $400 million in damage (1994 USD, equivalent to about $ million in ), much of it agricultural, and eleven people were killed, eight of them direct. Gordon later affected North Carolina with high waves, causing beach erosion and destroying five houses. Overall damage was $594 million due to Gordon (1994 USD, equivalent to about $900 million in ).
International governments and agencies through the United Nations sent relief supplies and monetary assistance to Haiti, following Gordon's devastating impact there. American soldiers were already stationed in the country to restore the ousted Jean-Bertrand Aristide to the presidency. The troops helped in rescues and worked to restore a damaged road between Port-au-Prince and Jacmel. Despite the high death toll and significant damage recorded, the name was not retired following the season.
Meteorological history
During the first week of November 1994, a large area of disturbed weather developed just north of Panama over the southwestern Caribbean Sea. A tropical wave passed through the area and gave it mild convection. A second wave passed through the area on November 6 and introduced cyclonic circulation to the disturbance. Over the next two days, the system gradually organized and sparked a deep convection off Nicaragua's southeast coast. This organization, with initial maximum sustained winds of , was designated Tropical Depression Twelve. Moving northwest, the storm began to slowly strengthen and its upper-level outflow became favorable to further development. Spots of convection flared on the morning of November 9; banding features appeared as its center made landfall on the northeastern Nicaraguan coast near Puerto Cabezas. A full day later a trough to the storm's northwest over the Gulf of Mexico moved the depression offshore, to the northeast, and over the warm waters of the western Caribbean Sea. Fueled by these warm waters, on the night of November 9, it strengthened into Tropical Storm Gordon with winds.
Lacking firm movement because of weak steering currents, Gordon meandered north-northeast in the presence of mild west-southwesterly wind shear, unable to strengthen under the adverse conditions. By November 11, a trough prodded Gordon to the north-northeast at , and it strengthened by as it moved through the central Caribbean Sea. The trough continued steering Gordon, bending it eastward towards Jamaica on the afternoon on November 12. Despite the warm waters, Gordon did not strengthen that day as strong upper-tropospheric shear hindered development, disorganized the upper-level circulation, and reduced its winds to . The trough over southern Florida and the Gulf of Mexico continued to push Gordon eastward towards Jamaica. In the pre-dawn hours, the storm clipped the eastern edge of the island. Southwesterly wind shear kept the storm from developing beyond , but neither the shear nor the landfall significantly disrupted the cyclone's organization. Accelerating, Gordon turned towards the northeast. Continued shear prevented the upper-level development needed for typical cyclonic organization, but a strong lower-level circulation had formed. Its sustained winds were still only , but as the system approached eastern Cuba a gust of was reported. The center crossed near Guantánamo Bay. Meanwhile, the broad-scale circulation that was covering most of the Caribbean Sea (of which Tropical Storm Gordon was only a part) was interacting with an upper-tropospheric trough near the Straits of Florida. This trough strengthened the broad upper-level cyclone, which in turn strengthened Gordon and spawned several other low-level circulations in the western Caribbean Sea. When Gordon crossed eastern Cuba, the National Hurricane Center determined that it had become the most dominant of these low-level systems and had absorbed their convections. Meteorologist Jose Fernandez-Partagas voiced the minority opinion that Gordon's circulatory center had dissipated over Cuba and that a low-pressure system near the Bahamas was now the dominant system, which would have meant the demise of Tropical Storm Gordon and the emergence of a new tropical storm. By nightfall of November 13, Gordon had not only made two landfalls and survived interactions with three competing systems but also, in assimilating the Bahamian low, had gained the cool central core typical of a subtropical cyclone.
The deep-layered cyclone within which Gordon was embedded steered the storm west-northwest, south of Turks and Caicos and the Bahamas, on November 14. A large ridge of high-pressure near the U.S. Mid-Atlantic coast increased the pressure gradient around the storm, so although its sub-tropical elements (namely a lack of deep convection) precluded a core of strong winds immediately around the storm's nucleus, strong winds were supported outside the storm's circulatory center. These winds inched up to but did not strengthen any further. The ridge continued to steer the storm west-northwestward past the western Bahamas. This brought the southern portion of the storm's circulation over northern Cuba. The storm's fourth landfall occurred on November 15 when Gordon passed over the Florida Keys near Key West, Florida. The storm then continued west over the lower Keys and into the Straits of Florida, where the storm's center began to warm and deep convection signaled the return of Gordon's purely tropical characteristics. Steering currents remained weak giving the storm a chance to fully re-develop its deep convection while immobile at sea.
After stalling offshore for almost a day, a mid- to upper-tropospheric trough over the central U.S. slowly pulled Tropical Storm Gordon northward then north-northeastward towards Florida's west coast. The storm made landfall between Ft. Myers and Naples with winds. The eastward component of the storm's movement increased, and Gordon moved northeastward onto the Florida Peninsula at . The storm barely weakened as it crossed the landmass keeping its winds. Crossing the peninsula in a mere six hours, the storm continued to pick up speed. Early on November 17, back over the open ocean, the storm's central pressure began to fall. Improved organization was not apparent and wind shear was pulling at the core of the deep convection when, on November 17, Gordon suddenly spawned winds and was upgraded to a Category 1 hurricane.
The shortwave trough that had been steering Gordon across Florida moved ahead of the storm and its influence was replaced by a mid-tropospheric ridge over the eastern United States. Under the influence of this new ridge, the storm, which had been speeding northeast at , turned to the north late on November 17. The hurricane's loop continued, and as it moved to a west-northwesterly heading Gordon briefly threatened North Carolina's Outer Banks before stalling offshore once again. In the presence of weak steering currents once again, Gordon lost strength and slipped back to tropical storm status with winds. On November 18, about off the Outer Banks, Gordon began a southward drift away from the North Carolina coast. Warm waters improved its organization, but this did not result in stronger winds and the storm continued to weaken. Strong upper-level winds battered the storm from the northwest. They sheared away Gordon's upper-level convection while polluting the storm with colder and drier air that weakened its lower level convection. A high-pressure system over the central United States drifted east and added a westward component to Gordon's southward motion, pulling the storm southwest towards Florida. The persistent shear and a continued lack of deep convection eventually reduced the storm's winds to below tropical storm force, and on the morning on November 20, Gordon became a tropical depression. The high pressure system over the continent continued pulling the depression towards the west until it made its final landfall near Cape Canaveral that night with winds of . The storm moved northward across Florida, northeastward across Georgia, and finally merged with a frontal system over South Carolina.
Preparations When Gordon was approaching Jamaica on November 12, a tropical storm watch, and later warning, was issued for the island. The same day, a tropical storm warning was issued for southeastern Cuba from Camagüey to Guantanamo. On November 13, a tropical storm warning was issued for the southwest peninsula of Haiti, and later that day the same warning was issued for the Bahamas. Due to the storm, 65,000 people evacuated to safer locations in Cuba. Schools were closed in New Providence and Grand Bahama due to the storm, and Nassau International Airport was briefly shut down. A flight between Havana and Miami was canceled. In Cuba, officials forced 36,518 people to evacuate their homes, and workers also moved 68,780 livestock.