A strong upper trough ejected northeast across Eastern Colorado and into the Central Plains during the daytime hours of March 28th, which drove a dryline east into much of East Texas, Southeast Oklahoma, and adjacent sections of Southwest Arkansas during the afternoon, slowly mixing east across the remainder of Southwest Arkansas and North Louisiana during the evening through early morning hours of the 29th. Ample warm, moist air was readily available ahead of this surface feature, with large scale forcing adequate enough for scattered to numerous showers and thunderstorms developing across the broad warm sector near and ahead of the dryline. However, much of the available instability diminished during the evening with the loss of afternoon heating, but strong wind shear and convergence that persisted along and ahead of the dryline contributed to the development of an isolated severe thunderstorm over Caldwell Parish Louisiana, which produced large hail near Columbia and damaging winds which downed trees near Grayson before these storms exited the region into Northeast Louisiana by mid-evening.