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Dynamics of Thunderstorms in the Gulf Coast Region, Air mass thunderstorms are not as likely to be Severe, Type of lifting mechanism can be Convective lifting, Frontal thunderstorms e.g., Induced by sea breeze front, Interaction of air masses can form a Dry line, Mechanical Lifting produces Frontal thunderstorms, Relatively unstable air is lifted on the leeward side of mountain ranges causing Condensation, Interaction of air masses i.e., Maritime tropical warm, moist, unstable air mass, Conduction of heat results in Condensation, Air Mass or Non-frontal thunderstorms caused by an Interaction of air masses, Convective lifting results in Condensation