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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
Local Forecasting Knowledge
Gulf Region Climate
Fronts
Fronts at University of Illinois
ColdOcclusion
Cold Occlusions
Warm Occlusions
Occluded Front
Air Masses
Dynamics of Thunderstorms in the Gulf Coast Region
Winter Weather Regime
Modified cP Air Mass in Gulf Region
Air Masses
Mississippi Valley Effects
Transitional Seasons Weather Regime
Winter Weather Regime
Developmental Phases of Thunderstorms in the Gulf Coast Region
Dynamics of Thunderstorms in the Gulf Coast Region
Air Masses
StationaryFronts
Ceiling and Visibility
Stationary
Stationary Fronts
Quasi-Stationary Fronts
Ceiling and Visibility
WarmFront700mbFlow
WarmFrontalSlope
WarmFrontPrecip
Warm Fronts
Warm Occlusions
Frontogenesis
Frontolysis
Cold Fronts - Definitions and Measurements
Cold Fronts - Seasonal Factors
ActiveColdFronts
ColdFrontalSlope
ColdFrontSkew-T
InactiveColdFronts