The Windsor Locks, Connecticut Tornado of 3 October 1979: An Analysis of an Intermittent Severe Weather Event

Abstract

Abstract On 3 October 1979 a violent F4 tornado struck without warning at Windsor Locks, Connecticut just before 1900 UTC. It was the most destructive storm ever to occur in Connecticut. Our case study of the storm was motivated by the rarity of tornadoes in Connecticut and the unfavorable time of the year for such storms in New England. The history of the storm is traced by means of synoptic and subsynoptic scale analyses. Vigorous midtropospheric ascent occurred just in advance of a cold-core cutoff vortex that was opening up due to synoptic scale deformation while moving northeastward toward southern New England. The probable destabilization mechanism was the intersection of the northeastward moving pocket of cool air aloft with a tongue of high equivalent potential temperature surface air that originated over the relatively warm ocean water and was channeled northward through the Connecticut River Valley. The convective cell that eventually became associated with the Windsor Locks tornado was detected...