Fog, like its elevated cousin stratus, is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass.
View moreThe thickness of a fog layer is largely determined by the altitude of the inversion boundary, which in coastal or oceanic locales is also the top of the marine layer, above which the air mass is warmer and drier.
View moreThe thickness of a fog layer is largely determined by the altitude of the inversion boundary, which in coastal or oceanic locals is also the top of the marine layer, above which the air mass is warmer and drier.
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