Dear students,
We continue studying the layers of the Earth’s atmosphere.
The weather layer. The most important layer of air for people on the earth is the one immediately above the earth's surface. This is the troposphere, or weather layer. Like all of the other layers of the atmosphere, it is widest at the equator and narrowest at the poles. Practically all of the atmosphere's oxygen and all of its water vapor are found in the weather layer.
Air in the weather layer is denser than air in the other layers. The air is densest near the earth's surface. As altitude increases, the air gradually thins. At altitudes above 10,000 feet (3,000 m), people who are not used to the thinner air of higher altitudes find breathing more difficult.
The conditions of the air in the troposphere change very often. These changes are what make weather. You will learn more about these changes and why they take place further. Just remember that all weather changes take place in the troposphere—the earth's weather layer.
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The air-travel
layer. The
upper reaches of the troposphere
gradually merge into the stratosphere
about 10 miles (16
km) above the earth's surface.
The air in
this layer is clearer and much
thinner than air in the weather layer. Because it is
free of water vapor, the stratosphere
has no clouds. It
is also free
of strong up and down movements of air.
For these reasons, jet planes use it for
long distance air travel. The stratosphere is important for another reason. It contains ozone, a special form of oxygen. Ozone protects the earth by blocking out many of the most damaging of the sun's rays. Without the ozone in this layer, much of the life on earth would disappear in a matter of minutes. The radio layer. Radio waves travel in straight lines. They travel only a short distance before the earth curves away beneath them. Without the charged particles called ions in the ionosphere, radio waves would travel far into space and never be received on the ground. But the radio waves hit the ions, which reflect the radio waves back toward the earth, where they can be received hundreds, even thousands, of miles from their sending points. |
I’m looking forward the letters from you,
Mrs. Nicolaev