Hurricane Gilma was one of the most intense Pacific hurricanes on record and the second of three Category 5 hurricanes during the active 1994 Pacific hurricane season. Developing from a westward tracking tropical wave over the open waters of the eastern Pacific Ocean on July 21, the pre-Gilma tropical depression was initially large and disorganized. Gradual development took place over the following day before rapid intensification began. By July 23, the storm intensified into a hurricane and later a Category 5 storm on July 24. As Gilma reached this intensity, it crossed into the Central Pacific basin, the fourth consecutive storm to do so. The storm peaked early on July 24 with winds of and a barometric pressure estimated at 920 mbar (hPa; ). The following day, unknown factors caused the storm to suddenly weaken before increasing wind shear took over. The storm gradually weakened for the duration of its existence, turning slowly to the northwest. Late on July 28, the storm brushed Johnston Atoll, bringing gusty winds and light rainfall to the region. Gilma persisted until July 31 at which time it was downgraded to a tropical depression and dissipated over open waters. Meteorological history Hurricane Gilma originated from a tropical wave that moved off the coast of Africa and traversed the Atlantic Ocean during the second week of July 1994. The wave was of little note until it crossed Central America and entered the Northeastern Pacific hurricane basin on July 15–16. Convection began to increase; however, the system remained disorganized. Tracking westward, gradual development took place, leading to the Dvorak classification being initiated on July 20. Several hours later, the National Hurricane Center (NHC) designated the system as Tropical Depression Seven-E. A strong ridge situated north of the depression steered the system steadily westward. This movement would remain the same throughout most of the storm's existence. The depression was initially hard to locate due to its large size. Following an increase in organization, the depression intensified into a tropical storm early on July 22, at which time it was named Gilma. Deep convection developed around the center of circulation throughout the day and banding features became apparent on the west and south sides of the storm. Only 24 hours after becoming a tropical storm, Gilma quickly intensified into a hurricane. Low wind shear and warm sea surface temperatures, recorded up to by a ship near the hurricane, allowed