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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.
Cyclogenesis can only occur when temperature decreases polewards (to the north, in the northern hemisphere), and pressure perturbation lines tilt westward with height. Cyclogenesis is most likely to occur in regions of cyclonic vorticity advection, downstream of a strong westerly jet.The combination of vorticity advection and thermal advection created by the temperature gradient and a low pressure center cause upward motion around the low.he process in which an extratropical cyclone undergoes a rapid drop in atmospheric pressure (24 millibars or more) in 24 hour period is referred to as explosive cyclogenesis, and is usually present during the formation of a nor'easter.