Marine layer
Air mass forming over a large body of water
Marine layer
A marine layer is an air mass that develops over the surface of a large body of water, such as an ocean or large lake, in the presence of a temperature inversion. The inversion itself is usually initiated by the cooling effect caused when cold water on the surface of the ocean interacts with a comparatively warm air mass.
Read on Wikipedia · Image Brocken Inaglory, CC BY-SA 3.0
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