Meteorological history of Hurricane Wilma

Meteorological history of Hurricane Wilma
Hurricane Wilma was the most intense tropical cyclone in the Atlantic basin on record in terms of minimum barometric pressure, with an atmospheric pressure of . Wilma's destructive journey began in the second week of October 2005. A large area of disturbed weather developed across much of the Caribbean and gradually organized to the southeast of Jamaica. By late on October 15, the system was sufficiently organized for the National Hurricane Center to designate it as Tropical Depression Twenty-Four.
The depression drifted southwestward, and under favorable conditions, it strengthened into Tropical Storm Wilma on October 17. Initially, development was slow due to its large size, though convection steadily organized. From October 18, and through the following day, Wilma underwent explosive deepening over the open waters of the Caribbean; in a 30-hour period, the system's central atmospheric pressure dropped from to the record-low value of , while the winds increased to . At its peak intensity, the eye of Wilma was about in diameter, the smallest known eye in an Atlantic hurricane. After the inner eye dissipated due to an eyewall replacement cycle, Hurricane Wilma weakened to Category 4 status, and on October 21, it made landfall on Cozumel and on the Mexican mainland with winds of about .
Wilma weakened over the Yucatán Peninsula, and reached the southern Gulf of Mexico before accelerating northeastward. Despite increasing amounts of vertical wind shear, the hurricane re-strengthened to hit Cape Romano, Florida, as a major hurricane. Wilma weakened as it quickly crossed the state, and entered the Atlantic Ocean near Jupiter, Florida. The hurricane again re-intensified before cold air and wind shear penetrated the inner core of convection. By October 26, it transitioned into an extratropical cyclone, and the next day, the remnants of Wilma were absorbed by another extratropical storm over Atlantic Canada.
Formation
During the second week of October, an unusually large, monsoon-like lower-level circulation and a broad area of disturbed weather developed over much of the Caribbean Sea. The system was enhanced by diffluence from an upper-level low across the southwestern Atlantic. By October 13, a broad area of low pressure developed and persisted about southeast of Jamaica, possibly aided by the passage of tropical waves through the area at the time. Convection increased and became slightly better organized, though upper-level wind shear initially prevented development. 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.
Later on October 14, the system became much better defined, with increasingly organized shower and thunderstorm activity, as conditions in the upper levels of the atmosphere became significantly more favorable. It was then that the National Hurricane Center first indicated that it was possible for a tropical depression to develop in the area. Dvorak classifications were initiated on October 15. The system continued to organize, with the National Hurricane Center remarking the system could ultimately become a hurricane. By late on October 15, the surface circulation became defined well enough, with sufficiently organized deep convection, for the National Hurricane Center to designate the system as Tropical Depression Twenty-Four while it was located about east-southeast of Grand Cayman.
The depression tracked slowly westward, a motion due to weak steering currents caused by a high-pressure area to its north across the Gulf of Mexico. Initially, the center of circulation was broad without a defined inner core; forecaster Lixion Avila remarked, "The area of minimum pressure could [have been] anywhere within of its [initial advisory position]." Initially, the tropical depression was forecast to drift west-southwestward before turning to the north; within five days of the forecast's issuance, the system was predicted to be located about south of the Isle of Youth as a hurricane. However, the National Hurricane Center noted in the first advisory on the depression that there were "all indications that there could a dangerous hurricane in the northwestern Caribbean Sea in 3 to 5 days." This was due to the depression being located within an environment very conducive for development, specifically low amounts of wind shear and very warm water temperatures.
As Tropical Depression Twenty-Four drifted southwestward, it steadily organized; by early on October 16, rainbands began to gradually consolidate with well-established outflow, and a large upper-level anticyclone developed over the depression. Although deep convection and banding features increased, mid-level dry air from the north prevented significant organization, and the convection was split into two primary areas. Surface buoy reports indicated that, due to its large size, the system failed to strengthen beyond tropical depression status, even though it received tropical storm strength Dvorak classifications from The National Hurricane Center's Tropical Analysis and Forecast Branch and the National Oceanic and Atmospheric Administration's Satellite Analysis Branch. Continued reconnaissance flights reported peak winds of about .
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 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 southeast of Grand Cayman. Upon becoming a tropical storm, the National Hurricane Center predicted Wilma to track west-northwestward, reaching winds of 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 [of the forecast track] was unusually low", due to wide divergences between computer models. Late on October 17, a hurricane hunters flight into Wilma recorded winds of , but an unusually low pressure of , 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 south-southeast of Grand Cayman. Shortly after reaching hurricane strength, the hurricane began undergoing explosive deepening, after the development of a "pinhole" eye in diameter. This small eye was surrounded by a ring of deep convection, with cloud-top temperatures of about .
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 , making Wilma a dangerous Category 5 storm on the Saffir–Simpson scale. In the span of just 24 hours, Wilma had intensified from a tropical storm to a Category 5 hurricane, an unprecedented event for an Atlantic hurricane. The eye continued to contract to a diameter of about , the smallest known eye in an Atlantic hurricane, and at 1200 UTC on October 19, Wilma attained peak winds of . The central pressure rapidly dropped from 0000 to 0600 UTC, and at 0800 UTC, a hurricane hunters flight recorded a minimum central pressure of 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 , 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 . It is estimated by Dr. Eric Uhlhorn of NOAA's Hurricane Research Division that the winds may have peaked at between 189 and 229 mph rounded to 190 and 230 mph respectively following that Hurricane Hunter mission. At the time of its peak intensity, hurricane-force winds extended only from the small center of Wilma, with tropical storm force winds extending only about .
First landfall
Shortly after peaking in intensity, the coldest cloud tops surrounding the eye warmed slightly and an outer eyewall began to develop, signifying an eyewall replacement cycle was occurring. By late on October 19, the winds in Hurricane Wilma decreased to as the inner wide eye weakened and the wind field expanded. Early on October 20 the hurricane weakened to Category 4 status after the small, inner eye dissipated and the wide outer eyewall became the dominant eye. At the time, the pressure measured , the second-lowest known pressure for a Category 4 hurricane (Super Typhoon Judy had an 887 mb pressure at peak intensity), and Wilma retained the large eyewall as it turned northwestward. Initially, the hurricane was forecast to re-intensify into a Category 5 hurricane, with one forecast predicting it to make landfall on the Yucatán Peninsula with winds of , though Wilma remained a strong Category 4 hurricane as it tracked northwestward.
Steering currents remained weak, though a series of troughs eroded the high-pressure system across the Gulf of Mexico, resulting in a turn towards the north-northwest. Environmental conditions remained favorable, with the eye becoming more distinct early on October 21. At about 2145 UTC on October 21, Wilma made landfall on the island of Cozumel with winds of . 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 and gusts of up to .
Second landfall and demise
On October 22, the mid-level ridge to the north of Wilma essentially dissipated, leaving the hurricane drifting northward across the northeastern Yucatán Peninsula. As the hurricane moved further inland, the eye became cloud-filled as the deepest convection began to warm, and the winds gradually weakened during its passage over land. About 26 hours after making landfall on Cozumel, Wilma emerged into the southern Gulf of Mexico near Cabo Catoche with winds of about . Upon reaching open waters, reconnaissance aircraft reported the remains of an inner eyewall and an outer eyewall oscillating between in diameter. Convection deepened around the eyewalls, and the inner core of convection, which had previously become disrupted over land, became slightly better defined.
A powerful eastward-moving mid-level trough across the central United States turned the hurricane northeastward and caused it to gradually accelerate. Vertical wind shear increased as strong upper-level southwesterly flow increased, though in spite of the shear Wilma continued to intensify. Early on October 24, Wilma attained major hurricane status while located about west-southwest of Key West, Florida. It gradually became better organized, with the large eye becoming very distinct on satellite and radar imagery. Wilma was able to retain its strength because large eyes in tropical cyclones are more stable and more resistant to vertical wind shear. Despite wind shear values of about , Wilma strengthened further to reach winds of . It weakened slightly as it approached Florida, and made landfall at Cape Romano with winds of at around 1030 UTC on October 24.
Hurricane Wilma crossed the Florida peninsula in about 4.5 hours while continuing to accelerate northeastward, and emerged into the Atlantic Ocean as a weakened hurricane near Jupiter. 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. Shortly after exiting the Florida coastline, Wilma began to re-intensify, believed to be due to a reduction of friction of the eyewall and warm waters of the Gulf Stream. Early on October 25, the hurricane reached a secondary peak intensity of while located about east of Jacksonville, Florida. During the time, the large circulation of Wilma absorbed the much smaller Tropical Depression Alpha over the Bahamas.
Shortly after its secondary peak intensity, the wind shear, combined with its rapid forward motion of , resulted in a steady weakening trend. The overall cloud pattern began to deteriorate, with the eye becoming less distinct and the convection less symmetric. 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. The remaining convection continued to diminish, and by late on October 25 Wilma transitioned into an extratropical cyclone while located about southeast of Halifax, Nova Scotia, and still at Category 1 intensity. The weakening extratropical remnant turned to the east-northeast before being absorbed by another extratropical storm over Atlantic Canada on October 27.
See also
Meteorological history of Hurricane Katrina
Effects of Hurricane Wilma in Florida
Effects of Hurricane Wilma in the Bahamas
List of Florida hurricanes
References
Hurricane Wilma
Wilma
Wilma meteorological history