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This Concept Map, created with IHMC CmapTools, has information related to: Winter Weather Regime, High-speed jet streaks contribute to the formation of Fog, Positive vorticity advection is a measure of Net divergence aloft, Warm and cold fronts are associated with Low pressure systems, Advection at upper levels seen in 500 millibar chart, Warm and cold fronts lead to formation of Thunderstorms, Mid-latitude cyclogenesis can lead to the formation of Extra-tropical cyclones in the Gulf of Mexico, Interaction of air masses i.e., Maritime tropical air mass, Net convergence at the surface causes The rising of air, Temperature differentials which affect the degree of Mid-latitude cyclogenesis, Upper-air includes Upper-level troughs, Pressure gradient between Upper-level troughs, Upper-level troughs define regions of Net convergence at the surface, Gulf Coast Winter Weather Regime involves the influence of Upper-air, Gulf Coast Winter Weather Regime involves the influence of Maritime tropical air mass, The rising of air seen on Meteograms, Low pressure at the surface results in Mid-latitude cyclogenesis, High-speed jet streaks contribute to the formation of Low ceilings, Temperature differentials contribute to formation of Warm and cold fronts, Gulf Coast Winter Weather Regime is characterized as a Baroclinic regime, Upper-level troughs create Positive vorticity advection