As the air (above the sand) warms, it rises. The cool moist air above the water begins to move toward the sand, (forming the sea breeze). The hot sand heats the cool moist air in a process called conduction, causing the air to rise, (cool), and the gaseous water to form a cloud through condensation.
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I would say, strictly speaking, there's quite often no difference at all in the sea temperature. Water is very good at spreading energy through great volume, so sea temperatures when you look at the deep ocean temperatures or say the North Sea or the English Channel they might be within point five of a degree for days at a time. So you won't get a diurnal change.
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Answer:
As the air (above the sand) warms, it rises. The cool moist air above the water begins to move toward the sand, (forming the sea breeze). The hot sand heats the cool moist air in a process called conduction, causing the air to rise, (cool), and the gaseous water to form a cloud through condensation.
ANSWER
I would say, strictly speaking, there's quite often no difference at all in the sea temperature. Water is very good at spreading energy through great volume, so sea temperatures when you look at the deep ocean temperatures or say the North Sea or the English Channel they might be within point five of a degree for days at a time. So you won't get a diurnal change.