FloodZoneMap.org

Up-slope east to northeast flow associated with a weak frontal boundary across the area assisted in maintaining a moist and unstable atmosphere across the Texas Panhandle. Scattered to numerous thunderstorms developed during the late afternoon and evening as an upper level disturbance in northwest flow aloft. The strongly sheared environment led to rotating storms, which supported the production of very large hail and damaging winds across western, northern and central parts of the Panhandle. A