Atmosphere is divided into five distinct layers or zones: troposphere, stratosphere, mesosphere, thermosphere (ionosphere) and exosphere.
Troposphere:
It is the lowest region of the atmosphere which contains air and is subject to differential heating.
It extends from the surface of Earth up to 8 to 20 km. The changes in the atmosphere resulting in the change of weather occurs in this layer.
Stratosphere:
It extends to 30-35 miles above the earth’s surface.
It contains much of the ozone in the atmosphere and the increase in temperature with height occurs because of absorption of ultraviolet (UV) radiation from the sun by this ozone.
Mesosphere:
It lies above 30-50 miles from the earth surface.
The air here is thin, and the molecules are a large distance apart.
The mesosphere is the coldest atmospheric layer surrounding the earth.
Thermosphere:
It rises several hundred miles from the earth surface and lies from 50-400 miles. Temperature in this layer can be as high as 2000 degree centigrade.
The thermosphere is home to the International Space Station as it orbits Earth.
Exosphere:
It extends from top of the thermosphere to 6200 miles. The layer contains very few atmospheric molecules which can escape into space.
The air in the exosphere is very thin, and is made up mostly of helium, and hydrogen.