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This Concept Map, created with IHMC CmapTools, has information related to: Cold Front Operationalizations and Measurements, Cold Fronts in the Gulf Coast (definitions and measurements) form when Advancing cold air mass (Arctic or Polar) displaces a warmer (Maritime or Tropical) air mass, Altocumulus (mid-level) to Cumulus (mid and low level), Humidity progresses to Low dewpoint and humidity after frontal passage, Cold Fronts in the Gulf Coast (definitions and measurements) are identified by Precipitation, Cumulus (mid and low level) to Cumulonimbus (storm producing), Cold Fronts in the Gulf Coast (definitions and measurements) are identified by Temperature differences of 10-30 degrees, Cirrus (high level) to Altocumulus (mid-level), Advancing cold air mass (Arctic or Polar) displaces a warmer (Maritime or Tropical) air mass typically involves Temperature differences of 10-30 degrees, Clouds are usually Cumuloform, Humidity progresses from High humidity and dewpoints ahead of the front, Cumulus (mid and low level) indicates Instability, Cold Fronts in the Gulf Coast (definitions and measurements) are identified by Clouds, Cold Fronts in the Gulf Coast (definitions and measurements) are identified by Humidity, Cumulonimbus (storm producing) indicates Instability, Pressures fall steadily Ahead of passage, Winds shift to West to northwest after frontal passage, Cumuloform i.e., Cumulonimbus (storm producing), Precipitation normally Intermittent showers and thunderstorms, Cold Fronts in the Gulf Coast (definitions and measurements) have Seasonal Tendencies, Pressures rise steadily After passage