Composition, structure and importance of the atmosphere

COMPOSITION, STRUCTURE AND
IMPORTANCE OF THE ATMOSPHERE
23-08-2019 Kuldeep Manu DIS-IIHS, HPU

• The atmosphere of the earth is a vast expanse of gases enveloping
our entire earth. Within this envelope, we are surviving and all our
activities are confined. It is made up of several gases, water vapour
and minute particles suspended in the gaseous substance of air. The
atmosphere extends several hundred km above the earth surface. It
is not uniform at every height we climb above, but it has drastic
changes with height. The atmosphere is composed of several layers.
At the transition zones of the layers, the change is very sharp but
within a layer, the changes are slow. In this module, we will discuss
about the composition and structure of the atmosphere. Apart
from these, our concern will also be there to through light on its
importance and utility of the atmosphere for us as well as for the
entire living organisms.

Learning Objectives After studying this module,
you will be able to:
 define composition and composition of atmosphere,
 enlist various gases and components of atmosphere,
 enumerate different layers of atmosphere,
 understand the significance of various gases of atmosphere,
 explain various layer of the atmosphere and
 explain the importance of atmosphere as a living planet.

Meaning of Composition of
Atmosphere
The literal meaning of composition is ‘ingredients’
or ‘constituents’ of something. In another words, it
is a manner by which something is made up of.
When we apply the same meaning with
atmosphere, it signify the items or the elements
with which our atmosphere is composed. Our
atmosphere is composed of numerous gases and
other substances, hence, it is a mechanical mixture
of the gases, water vapour and dust particles. Let us
discuss about the composition of atmosphere.

Composition of Atmosphere
The envelope of atmosphere around the earth, a
mechanical mixtures of numerous gases and
other substances are very important to all living
organisms of the planet. The four major gases –
nitrogen, oxygen, argon and carbon dioxide
together constitute 99.99% of the total volume
of dry air. The maximum concentration is of
nitrogen with more than 78 percent while the
oxygen is little less than 21 percent

Atmospheric Gases

• Nitrogen: Nitrogen is the most abundant found in atmosphere constituting 78.084
percent to the total volume of dry gases Figure 1). This is almost chemically inactive
and have nothing to do with any sort of chemical actions in the atmosphere. It does
not combine freely with other elements, hence, it is termed as neutral substance.
This gas is found beyond a height of 100 km, but its concentration is below 50 km
height from the sea level. This gas is significant for the growth and reproduction in
plants and animals. Certain bacteria in the soil are capable of converting a very small
amount of atmospheric nitrogen into nitrates and fix it to the soils and water bodies
to be consumed by animals and plants. This process is called as Nitrogen fixation.
The nitrogen fixed in the earth’s surface is again converted and sent back to the
atmosphere by bacterial action through a chemical reaction called denitrification.
• Oxygen: It is the second largest gas of the atmosphere constituting 20.9476 percent
of the total dry atmospheric gases (Figure 1). It is very essential for the survival of
many of the living organisms of this planet. It is chemically very active gas. It is
combined with several other elements and forms varied compounds. Oxygen is vital
for combustion of fuels. When anything burns, oxygen is consumed and helps in
burning that substance. Though oxygen is found beyond 100 km but it is reasonably
in good proportion within 16 km of height. With increasing height, the amount of
oxygen decreases very rapidly. On mountain slope, the available oxygen for breath is
very scanty and the mountaineers are supposed to carry oxygen for them.

Argon: In terms of percentage, argon is the third largest
gas in the atmosphere constituting 0.934 percent of total
dry atmosphere (Figure 1). It is an inert gas and chemically
it is inactive. It is also found in the earth’s crust and sea
water. It is used in electric bulb and fluorescent lights.
Carbon dioxide: It is the fourth abundant gas of the
atmosphere. It is densest gas and found in lower parts. It
is found upto a height of about 30 km, it is concentrated
in the lower strata. Its percentage is very low, i.e., 0.04
percent (Figure 1) but it is most vital for the growth of
vegetative life of biosphere. It is transparent to the
incoming solar radiation but does not allow to escape the
same. And hence, it is called as greenhouse gas. It plays a
very crucial role in increasing the global temperature.

Carbon dioxide is also known as variable gas as its amount is
dependent upon the combustion, human activities and
vegetative cover of the planet. The carbon dioxide is reaching
to the atmosphere due to several human activities like energy
utilization, transport, industry, agriculture, waste generation
etc. (Figure 2). Apart from these human induced sources,
some natural sources are like plant respiration and release to
air from stored carbon in the rocks through natural process of
denudation. All these are leading to increase in the
atmosphere. This gas is on rise with the advancement in
economic development of the society. Economically
developed countries/ regions are generating big amount of
carbon dioxide gases

Methane: Methane is the also a greenhouse gas
which absorbs the radiation and cause more
temperature of the air. Paddy cultivation also
generates methane in the air. It is also produced
from the wetlands and waterlogged soils and
released in the atmosphere. Fossil fuel is also a
source to release of methane in the
atmosphere. Its amount in the atmosphere is
variable. The numerous sources of methane

Ozone: Ozone’s concentration lays in a belt between the heights of 15 to 50
km of atmosphere. Instead of normal two atoms of oxygen, ozone has three
atoms of oxygen formed together denoted by O3. It is formed when
atmospheric oxygen molecules are broken by ultraviolet solar radiation. It
may even be formed at the time of electrical discharge during thunderstorms.
This gas is also termed as variable as its formation and disintegration is
dependent upon numerous activities. Though ozone is very less in quantity
(0.00006 percent), this thin layer is very significant for the survival of living
world as it absorbs the dangerous ultraviolet rays and protects the earth.
Neon, helium, krypton, hydrogen, xenon are other minor gases. Some gases
are still extremely less in quantity, they are termed as trace gases. Important
among them are ammonia, carbon monoxide, sulphur dioxide, nitrogen
dioxide, nitrous oxide and sulphur hexafluoride etc.

Water Vapour: Water vapour is small in amount but it is one of the
most important part of atmosphere with respect to the distribution of
vegetation and life. Water vapour exists all the time in the atmosphere
but with varying degree of amount depending upon the season
(temperature condition) and the supply of water for evaporation and
evapotranspiration. Air is hardly completely dry. In summer, the water
holding capacity of the air is large as the temperature is high while in
winter it is low. Availability of sufficient amount water on the earth
surface or water body in an area witness greater vapour while less
availability of avoidance of the same shows low vapour. Examples may
be taken as equatorial region rich in water bodies (high vapour) and
subtropical hot desert region with less to no water availability (low
vapour). Though, vapour and air both are in gaseous form, their mixing
and movement are quite natural but the same homogeneity it not
seen. At any particular point of time, the amount of vapour is not more
than four present of the total volume of atmosphere. It is found in the
troposphere only and its concentration is in the lower level. About 90
percent of the total vapour lays below six km. It is estimated that the
about 50 percent is within two km of height. Water vapour plays a vital
role in keeping the earth warm as it has greenhouse characteristics.

Dust Particles: Huge amount of dust particles are available in the lower layer
of atmosphere in a suspended form. These dust particles are solid substances
generated from various sources and being carried by winds. Greater velocity
wind have greater amount of dust particles. It is not only a matter of
suspended solid particles, they are transported to great distances as well.
They varies widely in sizes. They may be big sized suspended only when the
drafting ability of the wind is great, but settles swiftly when the carrying
capacity of the wind is reduced. You must have observed yourselves too
during gales/ storms. Huge number of microscopic dust particles are
suspended even in completely calm air. Dust particles are variable and it is
more during dry seasons as the soils are loose and easily carried by winds, but
reverse is the case when it is rainy season when they are settled and
compacted. Over the globe, it is less in equatorial and polar areas while more
in subtropical hot desert areas. Minute dust particles are found several km
above the surface while the coarse sized are abundant near the surface.
Microscopic particles are nuclei for condensation and precipitation and they
have a great importance in this respect.

Aerosols: Aerosols are extremely fine-sized solid particles or liquid
droplets which continue to be in suspended form in gas for very-very
long time. They could be seen when their concentration is more
otherwise they are invisible. Aerosols themselves are non-gaseous
microscopic substance released in the atmosphere from various
sources – natural and human created. They could be pollen, minute
earthly dust, sea salt, carbon soot from burning fuels, volcanic dust
etc. Human activities also help the aerosols to enter the atmosphere.
Their concentration is more over the industrial and urban areas.
Burning of fossil fuels and generation of smoke also pump the aerosols
in the air. Therefore, the source of aerosols are both natural as well as
human generated (Figure 5). They are grouped into two – hygroscopic
(moisture absorbing and retaining) and non-hygroscopic (moisture
non-absorbing). Hygroscopic aerosols form the nuclei for condensation
and in this way, they help in precipitation.

Meaning of Structure of Atmosphere
Structure means the arrangement of different part
into one. In another words, it is the skeleton or
organization or anatomy of a whole by looking at
the relationships with its parts. According this
background, the study of different parts of the
atmosphere and the relationship with its parts is
said to be the structure of the atmosphere.
Vertically, the atmosphere is divided into different
layers/ parts. Therefore, the study of different
layers is known as structure of atmosphere.

Structure of Atmosphere
Based on chemical composition, the atmosphere is classified into two.
They are homosphere and heterosphere.
Homosphere
Homosphere is that part of atmosphere where the chemical
composition of the air is uniform or similar. It is the lowest layer in
terms of chemical composition. It extends from the earth’s/ ocean
surface to about 85 km (Figure 6). The density of the air changes very
rapidly with increasing altitude but the proportion of the major gases
found there remain alike throughout this layer with the exception of
water vapour, pollutants, ozone and some trace/ very minor gases.
On the basis of the changes in temperature, the atmosphere is divided
into five layers (Figure 7) out of them, three lower layers falls under
homosphere (i.e. within 85 km of altitude). They are troposphere,
stratosphere and mesosphere.

Troposphere: It is the lowest and densest layer of the atmosphere. It extends
till a height of about 8 km over pole but over equator, it is 18 km. About 80
percent of the total mass of the atmosphere lays in this layer. With increase in
height, the temperature keeps on declining till the limit of this layer. On an
average, the decrease in temperature with height is 6 degree Celsius par km.
The upper boundary is known as troposphere laying between 8 and 18 km. At
this level, the average temperature reaches to minus 50 degree to minus 60
degree Celsius (Figure 8). Water vapour is found in this layer in abundance
and about 99 percent of the total atmospheric water vapour is concentrated
here but wide variation is seen in terms of height and longitudes. Vapour
plays very vital role in regulating the temperature of the earth by creating
greenhouse effect. All weather phenomena are occurring in this layer only.
Troposphere is the home of all types of clouds, atmospheric turbulence and
mixing of the air. Both horizontal and vertical mixing is quite prominent here.
In fact, the term troposphere is derived from the Greek word ‘tropos’ means
‘turn’. Sphere is signifying ‘ball’ or a structure which is round in shape
attaining a three-dimensional space. Therefore, the troposphere is a three-
dimensional object with turning or mixing characteristics. Every sort of living
life is confined to the biosphere which include land water and air. The upper
limit of troposphere is tropopause which is a transition zone another upper
layer known as stratosphere.

Stratosphere: Stratosphere is the upward second layer as well as middle layer
of the homosphere. It starts from tropopause to approximate height of 50
km. The temperature at the tropopause remains almost constant till the
height of 20 km. After that, it starts increasing and continue the trend till the
height of 50 km (Figure 8). At this level, the estimated temperature is about
minus 10 to minus 15 Celsius. Though the temperature is on rise, but there is
no atmospheric turbulence. This layer is completely free from clouds and
other weather conditions. That is why, it has an advantage for flying long-
distance supersonic jets/ aeroplanes through this layer. The increase in
temperature in this layer is caused by absorption of solar radiation by ozone
(O3). Ozone is abundant in this layer and its 90 percent is concentrated (found
between 15 km to 50 km) in this layer only. The upper limit is stratopause
which is a very narrow strip of transition zone beyond which mesosphere is
found.

Stratosphere is also termed as ozonosphere, a layer made up
of ozone. This layer protects the living world of the planet
from the harmful effects ultra-violet rays. The ozone depletion
and hole over Antarctic was discovered in 1985. Since then,
we have observed that this layer has reached to a dangerous
level of depletion of ozone. The main ozone depleting
substances are received from the release of
chlorofluorocarbon (CFCs), hydro-chlorofluorocarbon (HCFCs)
and carbon tetrachloride. When the molecules of chlorine
atom come into contact with ozone (O3), it turns O3into O2
which is normal oxygen. One chlorine atom can destroy more
than a lakh atoms of ozone. Therefore, the chain of depletion
is very serious. O3 turned into O2, an ordinary oxygen
molecule is not capable to absorbing ultra-violet rays.

Mesosphere: Mesosphere is the third but the upper-most layer of the homosphere.
After this layer, heterosphere starts. The literal meaning of mesosphere is the middle
sphere. It is separated by tropopause below from troposphere and mesopause on the
top from thermosphere. It is extended from 50 km to 85 km from the earth’s surface
(Figures 7 and 8). The air pressure is very low. It is 1 millibar at the lower limit whereas
it is 0.01 millibar at the highest limit. This layer is characterised by decreasing
temperature and the coldest/ lowest atmospheric temperature is recorded in this
layer. The lowest temperature estimated near the mesosphere is around minus
130Celsius. It is colder that the lowest temperature recorded over Antarctic.
Between 75 to 85 km from the earth, noctilucent clouds are normal affairs in the
summer nights between 50 to 70 north and south latitudes. Its literal meaning is night
shining. It is a deep twilight seen only when the sun is on horizon but the sunlight is
still falling at that height. The seen clouds are made up of ice crystals. Meteoric dust
particles work like nuclei for ice crystallization which are falling as well as produced
due to burning of meteor caused by friction.

Heterosphere
The atmosphere laying beyond the homosphere is termed as
heterosphere. The term itself is self-explanatory and it is used
for that part of atmosphere where the air is not uniform. In
this part of atmosphere, the air is rare and the molecules are
wide apart. Relatively heavier gas molecules are concentrated
in the lower part whereas the lighter are forced to be above.
Beyond 85 km height, the composition of the atmosphere
with increasing altitude vary significantly. The mixing of the
gases are not possible as the turbulence is not happening
there. Different layers of prominently different gases are
nitrogen layer, oxygen layer, helium layer and hydrogen layer
are differentiated. However, the heterosphere, is divided into
two main spheres – thermosphere and exosphere.

Thermosphere: This sphere extends from mesopouse i.e., 85 km to about 650 km
from earth. The temperature is on rise in this layer due to absorption of solar radiation
by small amount of oxygen molecules present. It is highly dependent upon the solar
activities. The temperature reaches beyond 1200C at an altitude of about 350 km but
by 650 km it may even rise to 2000C. This much high temperature is primarily defined
by average speed with which molecules are moving. Because of this, the temperature
may be high. The effectiveness of this temperature is not that great. Its exposure to
astronaut, if they are coming out from the capsule, is not affecting at all.
The Aurora is conspicuous phenomena observed in this layer. It is a striking display of
light and are maximum between 10pm to 2am in the magnetic polar region of
northern and southern hemispheres. It is known as Aurora Borealis (Figure 10) in the
northern and Aurora Australis in southern hemisphere. They are referred as northern
and southern lights. Charged particles coming from the solar flare reaches to the
earth’s upper atmosphere. These charged particles collide with nitrogen and oxygen
molecules present there in rarity. The collusion results into innumerable little surges of
lights. The scattering of these lights seen is very beautiful and magnificent.

Exosphere: Exo means external. Therefore,
exosphere the external or the outer most layer of
the atmosphere. Its lower boundary starts from the
thermopause (650 km) to the limit from where the
void space begins. This limit is estimated to be
about 10000 km. This much distance is little less
than the diameter of the earth. It is really a very big
size of the limit of the atmosphere. In exosphere,
very light gases are traced and they are hydrogen
and helium. Their molecules are spaced very widely.
Beyond the upper limit of exosphere, the space is
considered to be void.

Importance of the Atmosphere
Atmosphere is very crucial for every types of lives surviving on the earth. Without atmosphere, there is
least possibility of survival of living organisms. In very brief, following are the importance of
atmosphere.
Atmosphere is made up of several gases. These gases are important for the living world. Oxygen
available in the atmosphere is the life of all animals including human beings for breathe. Carbon
dioxide gas helps in photosynthesis by plants which is food for many animals. Without food, they are
unable to live. Photosynthesis is not possible without the humidity of the air and soils. Hence,
availability of water is also very important and it is partly also found in the air in the form of vapour.
The atmospheric vapour is distributed and redistributed all through the globe by hydrological cycle but
not uniformly. Nitrogen is equally very vital for making proteins through nitrogen fixation to plants and
to all animals. It is the building blocks for the growth of the body of all animals.
Ozone is a protective layer of the atmosphere which traps harmful ultra-violet rays coming from the
solar radiations. Its trapping in the ozonosphere ensures good health of all flora and fauna of the earth
particularly in the higher latitudes. Carbon dioxide, methane, nitrous oxide, fluorinated gases, water
vapour etc. are responsible for keeping the earth warm. Solar energy is reaching to the ground directly
from the sun by short wave radiations. But when the earth radiates back the received energy to space,
it is being trapped by greenhouse gases. They keep the earth liveable and maintain proper
temperature. Without greenhouse effect, the average temperature would fall to minus 18C whereas at
present the average temperature of the earth is 15C. The difference between the two is of 33C.
We are able to hear any sound because of the presence of air in the atmosphere. It behaves like a
medium to transport the sound waves. Flying of aeroplane is possible because of air as it helps in
floatation and marching forward the plane.

Composition, structure and importance of the atmosphere

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Composition, structure and importance of the atmosphere