Decoupling (meteorology)

ID: decoupling-meteorology

In meteorology, "decoupling" refers to a process in which the atmospheric boundary layer (ABL) becomes less coupled with the underlying surface, typically during the nighttime or under stable atmospheric conditions. This phenomenon can significantly affect temperature, humidity, and wind patterns. When the ABL is coupled with the surface, heat and moisture can be exchanged freely between the ground and the air above.

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