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CLIMATOLOGY - Coggle Diagram
CLIMATOLOGY
Structure of Atmosphere
Troposphere
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Thickness of the troposphere is greatest at the equator because heat is transported to great heights by strong convectional currents
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Tropopause
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After reaching a height of 10 km, i.e., near to of troposphere the rate of decline of temperature suddenly stops
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Stratosphere
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This layer absorbs ultra-violet radiation and shields life on the earth from intense, harmful form of energy
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Mesosphere
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Presence of ARORAS
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When Sun's magnetic particles try to enter in the earths atmosphere and interact with the earths magnetic field a huge lighting is caused
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Temperature
Temperature starts decreasing with the increase in altitude and reaches up to minus 100°C at the height of 80 km
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Heat Budget
What is Budget
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Rule of LAPSE
Whatever received or allocated should be spend/used full in the same time period, otherwise it will lapse
The earth receives almost all of its energy from the sun. The earth in turn radiates back to space the energy received from the sun. As a result, the earth neither warms up nor does it get cooled over a period of time
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