By: Morgan Vaughan

Upper Level Clouds

Middle Level Clouds

Lower Level Clouds

Vertical Clouds


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Radiation Fog

This fog results when the round loses heat through radiation, usually at night. As the heat radiated away from the ground passes through the lowest layer to the higher area the air closest to the ground cools as heat flows to the relatively cool ground and fog condenses in the cool air at the Dew Point.

Advection Fog

when warm, moist air moves horizontally over a cold surface, such as snow-covered ground or a cold ocean current.

Upslope Fog

Created by adiabatic cooling when humid air climbs a topographic slope

Evaporation Fog

Water vapor is added to cold air that is already near saturation