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THERMAL STRUCTURE OF EARTHS ATMOSPHERE
NEETHA SUSAN JOSEPHYSICAL SCIENCE
13350020
What is an Atmosphere?
• An atmosphere is a layer
of gases that may surround a material
body of sufficient mass by
the gravity of the body.
From Greek, Atmos -----”vapor”
sphaira------”sphere”
Composition of Earth’s Atmosphere
Nitrogen 78.0842%
Oxygen 20.9463%
Water Vapor about 1%
Argon 0.9342%
Carbon Dioxide 0.0384%
Other gases 0.0020%
Earth’s Atmosphere: Composition• The Earth’s atmosphere differs from those of the other terrestrial
planets in its chemical composition, temperature profile and circulation pattern
• Composition of present-day: 78% Nitrogen, 21% Oxygen
and 1% water vapor and carbon dioxide (greenhouse gas)
• The composition of atmosphere has evolved with time due to presence of living organisms
The atmosphere consists of many gases which below the homopause (near 105 km on Earth) are well mixed due to small scale turbulence and larger scale winds:
Atmospheric layers
• 8 layers are defined by constant trends in average air temperature (which changes with pressure and radiation).
1. Troposphere2. Tropopause3. Stratosphere4. Stratopause5. Mesosphere6. Mesopause7. Thermosphere8. Exosphere
TROPOSPHERE
• Lowest and thinnest layer—16 km at equator, 8 km at poles
• 90% of the atmosphere’s mass
• Temperature decreases with altitude—6°C per kilometer
—Top of troposphere averages –50°C
• Where weather occurs
• Boundary between the troposphere, and the stratosphere is called the tropopause
STRATOSPHERE
• Extends from 10 km to 50 km above the ground
• Less dense (less water vapor)
• Temperature increases with altitude
• Almost no weather occurrence
• Contains high level of ozone
> ozone layer
Upper boundary is called stratopause
MESOSPHERE
• Extends to almost 80 km high
• Gases are less dense.• Temperature
decreases as altitude increases.
Gases in this layer absorb very little UV radiation.
THERMOSPHERE• above the mesosphere
and extends to almost 600 km high
• temperature increaseswith altitude
• readily absorbs solar radiation
• Temperature can go as high as 1,500 °C
• reflects radio waves
Atmospheric Pressure
Measurement of atmospheric pressure with the mercury barometer:
Hg
5
Atmospheric pressure =
= 1.013x10 Pa 1013hPa
= 1013 mb
= 1 atm
B AP P gh
= 760 mm Hg (torr)
vacuum
A Bh
ATMOSPHERIC PRESSURE
Air Density
Air Density and height
THANK YOU
NEETHA SUSAN JOSE