Tropical Storm Arlene was a rare off-season tropical cyclone that hit Cuba and the Bahamas in May 1981. Its formation was unusual, originating from a tropical disturbance that crossed from the eastern Pacific Ocean into the Caribbean Sea; few Atlantic hurricanes develop in this manner. On May 6, a tropical depression developed, and the next day it became Tropical Storm Arlene near the Cayman Islands, three weeks before the start of the hurricane season. This marked the first Atlantic tropical storm in May since 1970's Hurricane Alma. Arlene moved northeastward throughout its life, bringing rainfall and locally gusty winds as it crossed Cuba and the southeastern Bahamas. On May 9, the storm dissipated when a large non-tropical storm absorbed Arlene. There were no reports of deaths or significant damage. Meteorological history The origins of Arlene were from a cloud mass that developed in the eastern Pacific Ocean in early May 1981. The system crossed Central America, and by the afternoon of May 5, a low-level circulation was evident near Roatán, off the coast of Honduras. Convection was initially disorganized, preventing classification as a tropical cyclone. It was not until late on May 6 that Dvorak satellite intensity estimates began on the system. Around that time, it is estimated it became a tropical depression, while located near the Cayman Island. It was a rare example of an Atlantic depression forming from a disturbance that originated in the eastern Pacific. After becoming a tropical depression, the system evolved rapidly as a spiral band formed around the circulation. Based on satellite imagery, the National Hurricane Center upgraded the depression to Tropical Storm Arlene on May 7. Shortly thereafter, Hurricane Hunters confirmed the intensity, while reporting a pressure of . By then and through much of its lifetime, the circulation was located along the western edge of the deep convection. Arlene strengthened slightly further to winds of 50 mph (85 km/h), before it moved ashore in eastern Cuba early on May 8. As it approached land, the convection was weakening, although its center maintained a steady northeast path, due to a high pressure system to its north. While crossing eastern Cuba, the circulation of Arlene became ill-defined, although re-strengthening over water was considered possible. When it reached open waters, Arlene was already a depression, and there was considered little likelihood of redevelopment, with strong shear pushing the convection far east of the center. Nevertheless,