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This Concept Map, created with IHMC CmapTools, has information related to: Fronts, Cold fronts are More common in the Gulf Coast region, Fronts types are Cold fronts, Boundary between Interacting air masses, More common in the Gulf Coast region because of Migratory tendencies of the Polar jet, Occluded are Rare in the Gulf Coast region, Temperature and moisture differences between Interacting air masses, Rare in the Gulf Coast region due to Tendency of Low pressure centers to migrate across CONUS to the north of the region, Boundary projected as Lines on a surface chart, Fronts have Developmental phases, More common in the Gulf Coast region due to the local influence of Maritime air mass, Developmental phases which are Frontolysis (dissipation), Fronts types are Warm, Stationary fronts are More common in the Gulf Coast region, Warm are Rare in the Gulf Coast region, Fronts types are Occluded, Fronts types are Stationary fronts, Fronts are defined in terms of Temperature and moisture differences, Developmental phases which are Frontogenesis (strengthening), Fronts are the Boundary, Rare in the Gulf Coast region due to the local influence of Maritime air mass