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What causes the weather?
For example, look at these pictures of the average January global temperature,
wind speeds and surface pressure from the
model called BUGS. Near the
equator, the temperatures are fairly constant - it is almost all orange (between
27 and 31 deg C). The surface pressure doesn't change much either, except for
the green blob of lower pressure east of Australia where the ocean is very warm
and storms are common.
But in the northern hemisphere, where it's winter, the temperature changes
pretty quickly as you go north, especially above the oceans.
Look, for example,
at the north Pacific Ocean. Sure enough, there is a large difference in pressure
between Hawaii and Alaska, with a big low pressure center above the Alaskan
Aleutian islands.
Since air flows from high to low pressure, you would expect
the air to flow toward the north. But, because of the
earth's rotation, the air
is deflected as it flows northward, and instead flows to the east. That's why
the air flows around high and low pressures, instead of directly between them.
In the northern hemisphere, the air flows counterclockwise around a low and
clockwise around a high. You can also see that the winds are the strongest where
the differences in pressure and temperature are the strongest.
Next page
->
under pressure, continuedLinks and resources |
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