[1], Meteorological history of Hurricane Katrina, Effects of Hurricane Wilma in the Bahamas, "Hurricane Wilma Tropical Cyclone Report", National Oceanic and Atmospheric Administration, "October 13 Tropical Weather Outlook 21z", "October 14 Tropical Weather Outlook 09z", "October 14 Tropical Weather Outlook 21z", "October 15 Tropical Weather Outlook 15z", "Tropical Depression Twenty-Four Discussion One", "Tropical Depression Twenty-Four Discussion Two", "Tropical Depression Twenty-Four Discussion Three", "Tropical Depression Twenty-Four Discussion Five", "Tropical Depression Twenty-Four Discussion Six", "Did Hurricane Wilma have 209 mph sustained winds? [17] 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). Updated 9 September 2014 for new U.S. damage estimate and ranking Wilma formed … Severe Storms, Image of the Day After the inner eye died off because of an eyewall replacement cycle, Wilma weakened to Category 4 status, and on October 21, it made landfall on Cozumel and on the Mexican mainland with winds of about 150 mph (240 km/h). Convection deepened around the eyewalls,[27] and the inner core of convection, which had previously become disrupted over land, became slightly better defined. The weakening extratropical remnant turned to the east-northeast before being absorbed by another extratropical storm over Atlantic Canada on October 27.
National Hurricane Center forecaster James Franklin remarked, "Confidence at the later ranges [of the forecast track] was unusually low", due to wide divergences between computer models. [24] About 26 hours after making landfall on Cozumel, Wilma emerged into the southern Gulf of Mexico near Cabo Catoche with winds of about 100 mph (160 km/h). The storm continued to the southwest while deep convection laid near the center. A big weather system formed across much of the Caribbean Sea and slowly organized to the southeast of Jamaica. [1], Hurricane Wilma crossed the Florida peninsula in about 4.5 hours while continuing to speed northeastward, and entered into the Atlantic Ocean as a weakened 110 mph (175 km/h) hurricane near Jupiter.
In the beginning, development was slow because of its large size, although thunderstorms slowly organized. Take control of your data. Also, the symbols show whether it is a hurricane, tropical storm or other storm category along the track. 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 170 mph (275 km/h), making Wilma a dangerous Category 5 hurricane on the Saffir-Simpson Hurricane Scale. Keep up with the latest hurricane watches and warnings with AccuWeather's Hurricane Center. [19] Early on October 20 the hurricane weakened to Category 4 status after the small, inner eye dissipated and the 45-mile (72 km) wide outer eyewall became the dominant eye. Looking back at Hurricane Gustav's record 211 mph wind gust, Global warming and the frequency of intense Atlantic hurricanes: model results.
It weakened slightly as it continued northwestward, and struck the Mexican mainland near Puerto Morelos, Quintana Roo, at 0330 UTC on October 22, with winds of 135 mph (217 km/h)[1] and gusts of up to 170 mph (270 km/h). By late on October 15, the system was became strong for the National Hurricane Center to name it Tropical Depression Twenty-Four. A vigorous cold front associated with the mid-level trough moved across the area to the west of Wilma, yet the cooler and drier air behind the front could not fully penetrate the inner core of the hurricane to weaken it. A surface low pressure system gradually became defined [17], Shortly after peaking in intensity, the coldest cloud tops surrounding the eye warmed a little bit and an outer eyewall began to form, meaning that an eyewall replacement cycle was happening. The extratropical remnant continued east-northeast before being absorbed by another extratropical storm on October 27. Despite increasing amounts of wind shear, the hurricane re-strengthened to hit Cape Romano, Florida as a major hurricane. This small eye was surrounded by a ring of deep convection, with cloud-top temperatures of about −125 °F (−87 °C). [14] 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. [1] The overall cloud pattern began to deteriorate, with the eye becoming less distinct and the convection less symmetric. [27], A powerful eastward-moving mid-level trough across the central United States turned the hurricane northeastward and caused it to gradually speed up. [32] By 1117 UTC on October 25, the center was located to the northwest of the primary convection as cold air from the southwest entrained the circulation. Each image covers an area of about 380 kilometers by 1,830 kilometers.
© Copyright TWC Product and Technology LLC 2014, 2020. (The lower the pressure, the stronger the storm.) [25] About 26 hours after making landfall on Cozumel, Wilma emerged into the southern Gulf of Mexico near Cabo Catoche with winds of about 100 mph (160 km/h). The meteorological history of Hurricane Wilma, the strongest tropical cyclone known in the Western Hemisphere, began in the second week of October 2005. The system drifted westward, and early on October 14 the convection became more concentrated and a little better organized as upper-level wind shear lessened slightly. [13], Tropical Storm Wilma began to turn to the west-northwest on October 18,[1] during which the storm developed a small, intermittent and ragged eye feature as well as a mid-level eye feature. The system moved westward,[2] and early on October 14 the convection became more concentrated and a little better organized as upper-level wind shear lessened slightly. Shortly after exiting the Florida coastline, Wilma began to re-intensify,[1] believed to be due to a reduction of friction of the eyewall and warm waters of the Gulf Stream.
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