Atmosphere - Components and structure of Atmosphere. Study notes for all competitive Examination.
The composition and structure of the
atmosphere
The air which
surrounds the earth is called the atmosphere. The atmosphere is held to the
earth due to its gravitational pull. The total weight of earth atmosphere is
about 500 million tons. The atmosphere is essential for the existence of life
on earth.
Composition of the atmosphere
The
atmosphere is a mixture of colourless, odourless
and tasteless gases. The atmosphere contains two main gases oxygen ( 21%) and Nitrogen
(78%).
Other gases
found in small quantities include Argon carbon dioxide, neon,, hydrogen, helium,
methane etc.
Besides these
gases the lower layer of the atmosphere contains water vapour, dust particle, smoke, salt etc.
Heavier gas
like oxygen is mostly found in the lower layer. All living organisms need
oxygen to breath.
Nitrogen
helps in the growth of living organisms.
Carbon dioxide absorbs the heat radiated by
the earth and keeps the planet warm. Plants use carbon dioxide to prepare food
through the process of photosynthesis.
Structure of the atmosphere
The
atmosphere has a layered structure. On the basis of composition, density, temperature
and other properties the atmosphere can be divided into five layers –
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
Troposphere
The
troposphere is the lowest layer and is closest to the earth’s surface.
It extends up to a height of about 8 km near the poles
and about 18 km over the equator.
This layer
protects us from the excessive heat of the sun during the day and keeps the earth’s
surface warm at night.
The
troposphere is the home of clouds, lightning, thunderstorm and other weather
phenomenon.
With increase
in height the temperature decreases at rate of 1° C per 165m of ascent called normal
lapse rate.
Troposphere
has about 90% of the air in the atmosphere. Water vapour and dust particles are found only
in this layer of atmosphere
Stratosphere
Stratosphere
lies above the troposphere and it spread about 50 kilometre above the sea
level.
The lower part of the stratosphere between 15
km to 35 km has concentration of ozone and is thus called ozonosphere.
Ozone act as
a barrier for ultraviolet radiation of the sun to reach the earth’s surface add
protect life on earth.
Mesosphere
The
mesosphere lies above the stratosphere. It extends from about 50 km to about 80
km above the mean sea level.
This is the
coldest layer in the atmosphere.
Meteors which comes from outer space burn up
in this layer because of friction with the atmosphere.
The
temperature decreases with height and reaches about -100° C at the heights of
80km.
Thermosphere
The Thermosphere
lies above the mesosphere. It extends from about 80 km to about 400 km above
the mean sea level.
The lower
part of the Thermosphere is called ionosphere as it has Ionized molecules.
In the
thermosphere the temperature may reach
up to 1500°C at it’upper limit.
This layer
reflects low frequency radio waves to earth. Thus It helps in long distance
communication.
Exosphere
The exosphere
is the uppermost layer.
The density of air is very low and it is in a
rarefied form.
Very light
gases like hydrogen and helium are found in this layer.
The exosphere merges is gradually into outer
space.