How does a sea breeze develop during the day?
A sea breeze is a local coastal circulation produced when land heats faster than the sea during the day.
Formation process and geographic mechanism
Air over warming land expands and rises, lowering surface pressure relatively. Cooler marine air moves inland at the surface, with a return flow aloft. As the sea-breeze front advances inland it may bring lower temperature, higher humidity and a wind shift. With enough moisture and instability it can initiate clouds or showers.
Spatial outcomes, measurement and management
At night, faster land cooling can produce a weaker land breeze. Coast shape, mountains, regional wind and sea-surface temperature alter strength. Urban heat islands may affect inland penetration. Although cooling, a sea breeze can carry pollutants inland or recirculate them toward the coast.
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