Clouds
By: Morgan Vaughan
Upper Level Clouds
Middle Level Clouds
Lower Level Clouds
Vertical Clouds
Fog
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