Warm air over land rises
Sea Breeze moves inland
Cumuli develop aloft and move seaward
Upper level return land breeze
Cool air aloft sinks over water
Sea Breeze (meso-cold) Front


Cool air over land sinks
Land Breeze moves out over water
Relatively warmer water heats air which then rises
Upper level return sea breeze
Cool air over land sinks

Explains why it can be breezy in the morning and evening after calm days and nights.

As the warm air rises it's replaced by the air from the land or the water.

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