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What is the stratosphere?
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| The stratosphere is the next major atmospheric layer above the
troposphere, covering the altitudes from about 8 to 30 miles high.
Air temperature slowly increases with height in the stratosphere, in contrast with the troposphere
where the temperature rapidly decreases with height. This unusual temperature structure is
caused by absorption of sunlight by the
ozone layer. All weather stops at the top of the
troposphere (called the tropopause), and the stratosphere is essentially cloud-free.
If you see a tall thunderstorm with an anvil cloud,
it is likely that the anvil cloud is "bumping up against" the bottom of the stratosphere.
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| Interesting facts:
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| AIRPLANES NOT ALLOWED Very few airplanes can fly as high
as the stratosphere because the air is so thin that there is not enough lift to keep the aircraft
supported. Some spy planes do fly in the lower stratosphere, however, such as the U-2 and the SR-71.
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