Thunderstorm Wind in Livingston Parish, Louisiana

Powerlines downed by thunderstorm winds.

A trough axis extending from the eastern Great Lakes into the Mid-Atlantic states and a ridge centered over the central and southern Plains placed the forecast area directly between both features. A weak front approached the area from the north. This front was the initial focal point for convective activity to begin developing in the afternoon hours. This activity capitalized on a warm, moist, and unstable environment to produce slow moving strong thunderstorms in the Baton Rouge area. These storms produce isolated flash flooding and severe wind gusts.