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Sea Breeze:
This process takes place for the duration of the day. Both the sea, as well as the land surface is heated up by the sun. The sea heats up slower than the land because it has a much higher heat capacity. Thus, the temperature over the land surface increases, in turn, heating up the air around it. An expansion occurs in the less dense warm air and an area over the land having low pressure is developed. At the same time on the top of the sea, a high-pressure area develops. Due to the difference in pressure and the air flows from the high pressure over the sea to the low pressure over the land. This flow of air from the sea to the land is termed as the sea breeze.
Land Breeze:
This process takes place for the duration of the night and the above-mentioned process gets reversed. Both, the land as well as the sea starts cooling down when the sun sets. As the heat capacity of land is different than the sea it cools down quicker. Thus, a low-pressure situation develops over the sea as the temperature above it is higher when compared to the land. Due to this, the air flows from the land to the sea which is termed the land breeze.