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  • Understanding Land and Sea Breezes: Temperature Differences Explained
    Land breezes and sea breezes are created by the differences in temperature between land and water.

    Here's how it works:

    Land Breezes:

    * During the night: Land cools down faster than the water. This is because water has a higher heat capacity (meaning it takes more energy to change its temperature).

    * Cooler air over the land becomes denser and sinks, creating higher air pressure over the land.

    * Warmer, less dense air over the water rises, creating lower air pressure over the water.

    * Air flows from high pressure to low pressure, resulting in a breeze blowing from the land towards the sea (a land breeze).

    Sea Breezes:

    * During the day: Land heats up faster than water.

    * Warmer air over the land rises, creating lower air pressure over the land.

    * Cooler, denser air over the water sinks, creating higher air pressure over the water.

    * Air flows from high pressure to low pressure, resulting in a breeze blowing from the sea towards the land (a sea breeze).

    In summary, the difference in temperature between land and water creates differences in air pressure, which drives the flow of air, resulting in land and sea breezes.

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