Tropical Storm Gamma was the 25th storm of the 2005 Atlantic hurricane season. Gamma formed on November 18 from a tropical wave which had left the coast of Africa on November 3. Between November 13 and November 16 the system was designated Tropical Depression Twenty-Seven and moved westward through the Windward Islands into the Caribbean. Although its winds were not of tropical storm force, the storm brought damagingly heavy rainfall to Trinidad and to St. Vincent and the Grenadines. On November 18, after a period of disorganization during which it appeared to be dissipating, the system strengthened and was upgraded to a tropical storm off the coast of Honduras and given the name Gamma. There, its torrential rainfall triggered deadly landslides. Gamma's winds and rains also reached into Belize, where they were less deadly. The storm dissipated on November 22, having killed 39 people. Meteorological history Tropical Storm Gamma originated out of a tropical wave that moved off the western coast of Africa on November 3. For a late-season tropical wave, the system kept an unusually high amount of convection as it trekked across the Atlantic Ocean. The National Hurricane Center (NHC) began to actively track the wave when it was located about off the coast of Barbados. The low pressure area changed little during November 13, producing locally heavy rains in the Caribbean Islands, but not developing. However upper-level shearing winds abated, making conditions conducive for tropical development, and by November 14 the system had formed Tropical Depression Twenty-Seven. An upper-level trough near the Greater Antilles continued to provide westerly shear that briefly stalled the development, but the system's strong convection persisted. A break in the shear on November 15 enabled the storm to briefly strengthen. Post season analysis showed during this period the system reached tropical storm-status and should have been christened Gamma, but as this was not seen at the time, the storm remained classified Tropical Depression Twenty-Seven. A deeplayered subtropical high pressure ridge over the southwestern Atlantic Ocean and Gulf of Mexico propelled the system westward across the Caribbean at more than and the storm's upper circulation was entirely separated from its deep convection and low level circulatory center. The NHC, believing that the system was dissipating, announced that it was issuing its last advisory on November 16. Soon after, the system slowed down on November 17. A tropical wave, which had formed over Panama in