Hurricane Emilia was, at the time, the strongest tropical cyclone on record in the Central Pacific Ocean, and the second of such to be classified as a Category 5 hurricane – the highest rating on the Saffir–Simpson hurricane wind scale. However, hurricanes Gilma later that year, Ioke in 2006, and hurricanes Lane and Walaka in 2018 later reached lower barometric pressures in the Central Pacific. In addition, Emilia was the first Category 5 Pacific hurricane since Hurricane Ava in 1973. The fifth named storm and the first of three Category 5 hurricanes of the 1994 hurricane season, Emilia developed from an area of low pressure southeast of Hawaii on July 16. Tracking westward, the initial tropical depression intensified into a tropical storm several hours after tropical cyclogenesis. Subsequently, Emilia entered the Central Pacific Ocean and moved into the area of responsibility of the Central Pacific Hurricane Center (CPHC).
After reaching hurricane intensity the following day, the tropical cyclone began to rapidly intensify, and late on July 19, Emilia reached its record peak intensity with maximum sustained winds of and a minimum barometric pressure of , rating it as a Category 5 hurricane. After slight oscillations in strength, an upper-level trough forced the intense hurricane northwest on July 21, and Emilia began to weaken thereafter. The tropical cyclone encountered an area of vertical wind shear and cool sea surface temperatures, which further weakened the system. The following day, Emilia made its closest approach to the Big Island of Hawaii, but subsequently weakened to below hurricane intensity. This weakening trend continued, and the tropical cyclone fully dissipated on July 25. Though the hurricane did not make landfall, Emilia brought strong surf to the islands of Hawaii and caused gusty winds, which resulted in some property damage. Precipitation was also reported, but remained under moderate levels.
Meteorological history
On June 29, a weak tropical wave exited the west African coast and traversed the Atlantic, showing no signs of organization or convective activity. Moving within the Intertropical Convergence Zone, the tropical disturbance remained inactive until July 14, when it developed into an area of low pressure roughly east-southeast of the Hawaiian Islands. A low-level circulation became evident, and the system was designated as a tropical depression on July 16. Within 12 hours, satellite imagery suggested that the system had intensified into Tropical Storm Emilia with sustained winds. Emilia steadily intensified into a minimal hurricane by the next morning, as it moved west-northwest. At 18:00 UTC, Emilia was upgraded to Category 2 status as it crossed 140°W and entered the Central Pacific Hurricane Center's (CPHC) area of responsibility, which noted that Emilia was "well developed." Emilia then proceeded to rapidly intensify, with maximum sustained winds increasing from over the next 48 hours. At Emilia's peak strength, an Air Force reconnaissance aircraft measured a minimum central pressure of , the lowest pressure ever recorded in a Central Pacific hurricane at that time.
On July 20, Emilia briefly weakened into a Category 4 hurricane, but it was re-upgraded to Category 5 status by the CPHC 12 hours later during the day. Subsequently, Emilia began to weaken for the final time. An upper-level trough in the westerlies caused the cyclone to turn northwest on July 21. Emilia moved over progressively cooler waters, and vertical wind shear from the westerlies negatively impacted the hurricane. The central pressure steadily rose to , and Emilia diminished into a marginal Category 3 hurricane. On July 22, Emilia continued to weaken, and it passed within of the Big Island. It was the closest approach to the islands. Later, Emilia's peak winds dropped to . Emilia gradually turned west-northwest, and the circulation moved with the trade winds. Emilia weakened into a tropical depression on July 24, and a remnant swirl of stratocumulus clouds was noted. The system dissipated on the same day.