Warning:
JavaScript is turned OFF. None of the links on this page will work until it is reactivated.
If you need help turning JavaScript On, click here.
This Concept Map, created with IHMC CmapTools, has information related to: Gulf of Mexico Effects, Advective Fog is most dense when Warm air advects from over the Gulf, Sea breeze is caused by Convection, Sea breeze are Microscale (Tertiary) winds, Warm air advects from over the Gulf to Near-shore inland areas, Arctic air masses in Winter, Relatively warm water temperatures contributes to the formation and enhancement of Sea breeze, Advective Fog is discussed in a Case Study, Relatively warm water temperatures decrease likelihood of Freezing temperatures, Relatively warm water temperatures contributes to the formation and enhancement of Hurricanes, Polar air masses in Winter, Gulf of Mexico (effects on regional weather) is a Major source of moisture, Advective Fog generally dissipates by Late morning, Relatively warm water temperatures lessen impact of approaching Arctic air masses, Major source of moisture contributes to the formation and enhancement of Advective Fog, Advective Fog most prevalent in Late Fall through early Spring, Coastal regions defined as Within 10 nautical miles of the coast, Summer involves Solar Heating of the Land, Warm air advects from over the Gulf creates Warm air over cold air condition, Air temperature reaches 10 degrees above the sea surface temperature due to Solar Heating of the Land, Sea breeze range up to 40 nautical miles inland