Meteorological History of Hurricane Wilma - Peak Strength

Peak Strength

By early on October 17, the outer rainbands, which had previously dominated the structure of the cyclone, dissipated, while deep convection developed near and to the south of the center. Computer models predicted steady strengthening as the depression tracked westward before turning to the north. Of the intensity models, the Geophysical Fluid Dynamics Laboratory predicted an intensity of 135 mph (217 km/h) within 36 hours, with other forecasts being more conservative in their predictions. Deep convection continued to develop to the south of the center, and the depression intensified into Tropical Storm Wilma at 0600 UTC on October 17, while located about 200 miles (320 km) southeast of Grand Cayman. Upon becoming a tropical storm, the National Hurricane Center predicted Wilma to track west-northwestward, reaching winds of 105 mph (169 km/h) before striking the northeastern portion of the Yucatán Peninsula.

The storm continued to the southwest while deep convection persisted near the center. National Hurricane Center forecaster James Franklin remarked, "Confidence at the later ranges was unusually low", due to wide divergences between computer models. Late on October 17, a Hurricane Hunters flight into Wilma recorded winds of 50 mph (80 km/h), but an unusually low pressure of 989 mbar (29.21 inHg), which would be more typical of a minimal hurricane. This was due to unusually low pressures across the region, which resulted in a lesser pressure gradient and thus lighter winds. Convection continued to develop near the center and became much more symmetrical.

Tropical Storm Wilma began to turn to the west-northwest on October 18, during which the storm developed a small, intermittent and ragged eye feature. It continued to intensify, and at 1200 UTC on October 18, Wilma attained hurricane status while located about 225 miles (362 km) south-southeast of Grand Cayman. Shortly after reaching hurricane strength, the hurricane began undergoing explosive deepening, subsequent to the development of a "pinhole" eye 9 miles (14 km) in diameter. This small eye was surrounded by a ring of deep convection, with cloud-top temperatures of about −125 °F (−87 °C).

Early on October 19, Wilma attained major hurricane status while continuing to rapidly intensify, and by 0600 UTC, the storm's maximum sustained winds increased to 165 mph (266 km/h), making Wilma a dangerous Category 5 storm on the Saffir-Simpson Hurricane Scale. In the span of just 24 hours, Wilma had intensified from a 70 mph (110 km/h) tropical storm to a 175 mph (282 km/h) Category 5 hurricane, an unprecedented event for an Atlantic hurricane. The eye continued to contract to a diameter of about 3 miles (4.8 km), the smallest known eye in an Atlantic hurricane, and at 1200 UTC on October 19, Wilma attained peak winds of 185 mph (298 km/h). The central pressure rapidly dropped 54 mbar (1.65 inHg) from 0000 to 0600 UTC, and at 0800 UTC, a Hurricane Hunters flight recorded a minimum central pressure of 884 mbar (26.10 inHg) in a dropsonde near the center of the extremely small eye. As the dropsonde did not reach the calm winds in the center, the pressure was estimated at 882 mbar (26.05 inHg), the lowest pressure in an Atlantic hurricane on record. The pressure continued to fall as the Hurricane Hunters left the hurricane, and it is possible the pressure was slightly lower. Operationally, the peak intensity was estimated at 175 mph (282 km/h). At the time of its peak intensity, hurricane force winds extended only 50 miles (80 km) from the small center of Wilma, with tropical storm force winds extending only about 160 miles (260 km).

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