FloodZoneMap.org

In a seasonably very unstable airmass south of a frontal boundary and ahead of an approaching upper level shortwave, scattered storms developed across central Mississippi in the early morning. In the presence of robust mid-level wind shear, these storms rapidly became severe and produced several instances of hail as large as 1.5 inches. A break in severe thunderstorm activity was noted from mid morning into mid afternoon when diurnal building instability fostered redevelopment of robust and seve