4. INTRODUCTION
The air envelope that surrounds the earth is known as
atmosphere.
Here, we can see the structure of atmosphere in detail.
5. Structure of Atmosphere
From the earth’s surface upwards, there is a change in
temperature.
There are different layers of atmosphere.
They are: troposphere, stratosphere,
mesosphere and thermosphere.
6. TROPOSPHERE
Troposphere is the atmospheric layer which is close to
the earth’s surface.
It is derived from the Greek word ‘Tropos’ means to
‘turn’.
The traditional zone between the troposphere and
stratosphere known as tropopause.
7. STRATOSPHERE
It is second layer of atmosphere.
The ultraviolet rays of the sun absorb the oxygen atoms which
laid the formation of ozone in this part of the atmosphere.
Ozone layer lies in stratosphere.
The transitional zone above the stratosphere is strato- pause.
8. MESOSPHERE
It is extended from 50km-80km above the sea level.
It is the transitional zone where the temperature remains
steady.
THERMOSPHERE
It is the area where the temperature increases abruptly.
The part of the atmosphere, from about80km-400km
above the earth surface is called ionosphere.
9. CONCLUSION
Air extends to a height of several kilometers from the
surface of the earth.
The atmosphere is held to the earth by gravitational
force.