By early on October 9, the depression consisted of a circulation center without any of the associated deep convection that is one of the prerequisites of being a tropical cyclone. Several hurricane forecast models predicted Kyle to weaken until dissipation. After 24 hours without significant convection, thunderstorms reformed to the southeast of the center on October 10 as the depression entered an area of warmer water temperatures. Environmental conditions became more favorable, with weakening wind shear and decreasing dry air. The depression continued tracking around a ridge, turning to the west and west-northwest toward the coast of Florida. Convection increased markedly early on October 11 as it turned northward ahead of an approaching cold front, and Kyle regained tropical storm status about 35 miles (60 km) east of the border between Florida and Georgia.
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