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There is a thin buffer zone between the troposphere and the next layer called the tropopause. Virtually all human activities occur in the troposphere.
The next layer, the stratosphere, continues from 15 km to about 50 km. Most commercial airline traffic occurs in the lower part of the stratosphere. The stratosphere gets warmer at higher altitudes. In fact, this warming is caused by ozone absorbing ultraviolet radiation. Warm air remains in the upper stratosphere, and cool air remains lower, so there is much less vertical mixing in this region than in the troposphere.
Above the stratosphere is the mesosphere and above that is the ionosphere (or thermosphere), where many atoms are ionized (have gained or lost electrons so they have a net electrical charge)...
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Common topics in this essay:
- OZONE LAYER
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