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. 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 125 mph while about 340 miles (545 km) east of Jacksonville, Florida. During the time, the large circulation of Wilma absorbed smaller Tropical Depression Alpha over the Bahamas. Shortly thereafter, the wind shear combined with its rapid forward motion of 50 mph (80 km/h) resulted in a slow weakening trend. The overall cloud pattern began to be disorganized, with the eye becoming less visible and the convection less symmetric. By 1170 UTC on October 25, the center was to the northwest of the primary convection as cold air from the southwest disturbed the circulation. The remaining convection continued to diminish, and early on October 26 Wilma turned into an extratropical cyclone while about 230 miles (370 km) southeast of Halifax, Nova Scotia. The extratropical remnant continued east-northeast before being absorbed by another extratropical storm on October 27.