Astratosphere
Bmesosphere
Cionosphere
Dtropopause
Answer:
D. tropopause
Read Explanation:
Atmosphere
The composition of the atmosphere is somewhat uniform up to about 90 Kilometers from the surface of the earth
This part of the atmosphere is called homosphere.
Beyond this there is no uniformity in the gaseous composition. So the part of the atmosphere beyond 90 km from the earth is called as heterosphere.
The atmosphere can be divided into four layers or zones on the basis of its altitude and thermal condition. Temperature variation are experienced as its altitude increases from the earth. Atmospheric layers:
Troposphere
Mesosphere
Stratosphere
Thermosphere
Troposphere
The height of the troposphere is more in the equatorial regions because of strong convection here. (about 18km)
Almost all the weather and climatic phenomena such as cloud formation, rain, snow, wind, thunder and lightning etc. Take place in this layer
In the troposphere the temperature decreases at a uniform rate of 1° Celcius for every 165 metres of altitude. This is called Normal Lapse Rate.
The zone of transition above the troposphere is called tropopause.