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This Concept Map, created with IHMC CmapTools, has information related to: Fog, Summertime is when Fog tends to dissipate in the early to late morning, Fog in the Gulf Coast Region is most likely from December to February, Direct observations e.g., Local winds, Facilitating factors are Frontal passage followed by boundary layer wind from the SE through the SW, Loss of convective heating causes fog to Advect toward shore during the day, Drifts onshore sometimes During the day, Low-level stratiform cloud deck that Drifts onshore, Frontal passage followed by boundary layer wind from the SE through the SW causes fog to Advect toward shore during the day, Low-level stratiform cloud deck that Forms over the Gulf, NEXRAD Radar shows Shallow inversion indicative of fog, Loss of convective heating causes fog to Advect offshore in the PM and over night, Ceiling and visibility can limit Airfield and Port operations, Low-level stratiform cloud deck that Drifts in and out over the land, Mid-level cloud deck causes Loss of convective heating, Fog in the Gulf Coast Region may be Advection fog or "sea fog", GOES IR Channels 2 and 3 show Mid-level cloud deck, GOES IR Channels 2 and 3 show Areas of fog over the Gulf, GOES IR Channels 2 and 3 show Low-level stratiform cloud deck, Advection fog or "sea fog" can occur In low-lying and forested areas near NASP, Advection fog or "sea fog" is a Low-level stratiform cloud deck