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Temperature inversion may occur during the passage of a cold front or result from the invasion of sea air by a cooler onshore breeze. Overnight radiative cooling of surface air often results in a nocturnal temperature inversion that is dissipated after sunrise by the warming of air near the ground.
The strength of the inversion is often measured by the temperature difference between the top and base of the inversion layer, with a larger temperature difference indicating a stronger inversion. Stronger (weaker) than normal high pressure is usually associated with a stronger (weaker) than normal inversion layer.CL vs. Inversion Base. The relative location of the LCL and the inversion base determine if marine stratus clouds will form. It is the relative location of both the LCL and the base of the Inversion Layer that determine if marine layer clouds will form.