Sea breezes and land breezes are local winds influenced by differential heating of land and water, creating variations in pressure due to temperature differences.
Sea breezes and land breezes are examples of local winds that blow over a limited area influenced by local geography. Sea breezes blow from sea to land during the day when the air over land is warmer than over water, whereas land breezes blow from land to sea during the night when the air over water is warmer than over land.
These local winds are created by differential heating and cooling of land and water, leading to variations in pressure due to the temperature differences between the two surfaces. The unequal heating of Earth's surface generates these local scale circulations, with sea and land breezes being a common example of such phenomena.
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