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Answer:

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Explanation:

Because water has higher specific heat capacity than water, land usually gets heated and loses heat faster than water.

During a warm day, the air above land gets heated quickly more than the air above water. This warm, less dense air above land begins to rise, creating a low pressure in the process. This paves way for the denser, cold air above water to replace the vacuum created by the warm air above land.

The directional movement of air from water to land is what is known as the sea breeze in coastal areas.

Air moves near the coast on a warm day because water has higher specific heat capacity than water, land usually gets heated and loses heat faster than water.

  • Sea breezes alternate with land breezes along the coastal regions of oceans or large lakes in the absence of a strong large-scale wind system during periods of strong daytime heating or nighttime cooling.
  • During a warm day, the air above land gets heated quickly more than the air above water. This warm, less dense air above land begins to rise, creating a low pressure in the process. This paves way for the denser, cold air above water to replace the vacuum created by the warm air above land.
  • The directional movement of air from water to land is what is known as the sea breeze in coastal areas.

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