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Introduction to Atmosphere
Atmosphere is a layer of gases surrounding a planet or other material body of sufficient mass that help on the gravity of the body. The atmosphere is a mixture of nitrogen (78%), oxygen (21 %) and other gases (15 %) that is surrounded earth. It is more likely to be retained if the gravity is high and the atmospheric temperature is low.
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The atmosphere is divided into four layers, as follows:
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- Troposphere:
Troposphere is the layer of atmosphere which is closest to the Earths surface, extending up to about 10- 15 km above the earth surface. It contains 75% of the atmosphere&aos;s mass. It is wider at the equator than at the poles. It is the place where all weather take place. If we moves higher then troposphere then the temperature and pressure drops. - Stratosphere:
Stratosphere lies directly above the troposphere and is about 35 km deep. It extends the layer from about 15 to 50 km above the Earths surface. - Mesosphere:
Above the stratosphere, it extending from 50 to 80 km above the earths surface. It is cold layer where the temperature decreases with increasing altitude. - Ionosphere
It is also called thermosphere and it is extends from 80 km above the earths surface to outer space.
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