Marine layer

Weather phenomenon in which an air mass forms over a body of water

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.

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Marine layer

Weather phenomenon in which an air mass forms over a body of water

Texte en anglais

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.

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Texte en anglais Pas encore d'article dans ta langue : extrait en anglais.

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.

Texte : Wikipédia en anglais, CC BY-SA 4.0. · Image : Brocken Inaglory (CC BY-SA 3.0) ·

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