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Sea Breeze During
the day, a coastline will experience a sea breeze. Because
the air over the land heats faster, it rises and causes the
cool air over the ocean to blow inland. Land Breeze During
the night along the coast the temperature of the land can
become cooler than that of the ocean. This causes a breeze
to blow towards the ocean. These two examples are common and show clearly
how wind is formed at ground level. However, this situation
happens all over the planet even when a large body of water
is not present. The ground will heat at different rates in
a given area due to many circumstances. Summary
To say that the Sun alone causes wind would be untrue. In
our example, the sun created heat, which then rose. As this
air rises, surrounding cooler air will rush in to take its
place. This rush of air to fill space is wind. Other factors play a part in influencing the
wind, such as the rotation of the Earth, location of mountains,
latitude, elevation and many others. The difference however
is that surface heat is a major player. Surface heat will
not completely determine the direction of wind flow, but it
will be very influential.
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