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Structure of the 
atmosphere
• We have learned the factors 
which influencing the 
temperature 
• From the earth surface upward 
there is a change in 
temperature, based on this 
change atmosphere has been 
divided into different layers
Structure of the Stmosphere
•Troposphere 
•Stratosphere 
•Mesosphere and 
•thermosphere
Structure of the Stmosphere
Troposphere 
• The atmospheric layer close to the earths 
surface is called Troposphere 
• The word Troposphere is derived from the 
Greek word tropos which means turn, air is 
very turbulent in this region 
• Based on the laltiude and season , its heights 
varies 
• At the poles it is 8 km and 17 km over 
equator. It is based on the temperature
Structure of the Stmosphere
• In the tropics convection 
current of air extends greater 
height , but in cold region it is 
very less 
• Temperature in Troposphere 
decreases steadily with 
increase in height, called 
normal lapse rate
Structure of the Stmosphere
Structure of the Stmosphere
• Extension of convectional current determine 
the height of troposphere 
• Temperature in Troposphere decreases 
steadily with increase in height at the rate of 
1 degree per 165 mtr 
• All the weather like cloud, rain, thunder are 
taking place in Troposphere water vapour 
and dust particles are found only here. 
• above the Troposphere s the Tropopause, 
where temperature is steady
Structure of the Stmosphere
Structure of the Stmosphere
•Tropopause is the 
transitional zone 
between troposphere 
and stratosphere
stratosphere 
• It situates just above troposphere 
• In the lower part, temperature is constant 
• this means when height increases temperature will 
not increases . It is for about 30 km from the 
surface 
• Then up to 50 km temperature increases with 
increasing height 
• Ultraviolet rays of the sun absorb by oxygen 
molecules and split into oxygen atoms and forms 
ozone layers 
• Here temperature increases due to release of latent 
heat
• Jet planes that fly very height create 
a white line in the sky this because 
when planes fly in stratosphere. 
Steam they release condense and 
form it . since there is a less 
movement of air here , thus it 
visible for a long time 
• The transitional zone above 
stratosphere is called stratopause
Structure of the Stmosphere
Structure of the Stmosphere

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Structure of the Stmosphere

  • 1. Structure of the atmosphere
  • 2. • We have learned the factors which influencing the temperature • From the earth surface upward there is a change in temperature, based on this change atmosphere has been divided into different layers
  • 6. Troposphere • The atmospheric layer close to the earths surface is called Troposphere • The word Troposphere is derived from the Greek word tropos which means turn, air is very turbulent in this region • Based on the laltiude and season , its heights varies • At the poles it is 8 km and 17 km over equator. It is based on the temperature
  • 8. • In the tropics convection current of air extends greater height , but in cold region it is very less • Temperature in Troposphere decreases steadily with increase in height, called normal lapse rate
  • 11. • Extension of convectional current determine the height of troposphere • Temperature in Troposphere decreases steadily with increase in height at the rate of 1 degree per 165 mtr • All the weather like cloud, rain, thunder are taking place in Troposphere water vapour and dust particles are found only here. • above the Troposphere s the Tropopause, where temperature is steady
  • 14. •Tropopause is the transitional zone between troposphere and stratosphere
  • 15. stratosphere • It situates just above troposphere • In the lower part, temperature is constant • this means when height increases temperature will not increases . It is for about 30 km from the surface • Then up to 50 km temperature increases with increasing height • Ultraviolet rays of the sun absorb by oxygen molecules and split into oxygen atoms and forms ozone layers • Here temperature increases due to release of latent heat
  • 16. • Jet planes that fly very height create a white line in the sky this because when planes fly in stratosphere. Steam they release condense and form it . since there is a less movement of air here , thus it visible for a long time • The transitional zone above stratosphere is called stratopause