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GEO - LESSON 4: AIR
What is a Atmosphere ?
* Our Earth is surrounded by a huge blanket of air called
atmosphere
* It provides us the air we breathe and protects us from
the harmful effects of the sun’s rays
Composition Of The Atmosphere
Do you know that the Air we take in while breathing is actullay a
mixture of many gases ?
•Nitrogen and oxyen are two gases which make up the bulk of the atmosphere.
•Carbon dioxide, helium, ozone, argon and hydrogen are found in lesser quantities.
•Apart from these gases, tiny dust particles are also present in the air.
Yes !
Nitrogen (78%)
Oxygen (21%)
Carbon dioxide
(0.03%)
Argon
(0.93%)
All others
(0.04%)
Pie Chart
Do You Know ?
When air is heated, it expands,
becomes lighter and goes up. Cold air is
denser and heavy. That is why it tends
to sink down. When hot air rises, cold
air from surrounding area rushes there
to fill in the gap. That is how air
circulation takes place
Do You Know ?
Structure Of The Atmosphere
Our atmosphere is divided into
five layers starting from the
earth’s sur face. These are
Troposphere, Stratosphere,
Mesosphere, Thermosphere and
Exosphere
Troposphere: This layer is the most
important layer of the atmosphere. Its
average height is 13 km. The air we
breathe exists here. Almost all the
weather phenomena like rainfall, fog and
hailstorm occur in this layer.
Stratosphere: Above the troposphere lies the
stratosphere. It extends up to a height of 50
km. This layer is almost free from clouds and
associated weather phenomenon, making
conditions most ideal for flying aeroplanes.
One important feature of stratosphere is that it
contains a layer of ozone gas. We have just
learnt how it protects us from the harmful
effect of the sun rays.
Mesosphere: This is the third layer of the
atmosphere. It lies above the stratosphere. It
extends up to the height of 80 km. Meteorites
burn up in this layer on entering from the
space.
Thermosphere: In thermosphere temperature
rises very rapidly with increasing height.
Ionosphere is a part of this layer. It extends
between Fig. 4.2: Layers of the Atmosphere
2020-21 AIR 23 Do you know? You will be
surprised to know that the earth receives only
1 in 2,000,000,000 parts of the sun’s energy.
80-400 km. This layer helps in radio
transmission. In fact, radio waves transmitted
from the earth are reflected back to the earth
by this layer.
Exosphere: The upper
most layer of the
atmosphere is known as
exosphere. This layer has
very thin air. Light gases
like helium and hydrogen
float into the space from
here.
WEATHER AND CLIMATE
Weather is this hour-to-hour, day to day
condition of the atmosphere. A hot or humid
weather may make one irritable
The average weather condition of a place for a
longer period of time represents the climate of a
place.
“Is it going to rain today?” “Will it be bright and sunny today?” How
many times have we heard this from anxious cricket fans speculating the
fate of a One Day match? If we imagine our body to be a radio and the
mind its speaker, weather is something that fiddles with its control
knobs. Weather is this hour-to-hour, day to day condition of the
atmosphere. A hot or humid weather may make one irritable. A
pleasant, breezy weather may make one cheerful and even plan for an
outing. Weather can change dramatically from day to day. However, the
average weather condition of a place for a longer period of time
represents the climate of a place. Now do you understand why we have
daily weather forecasts.
WEATHER AND CLIMATE
The temperature you feel
everyday is the temperataure
of the atmosphere. The
degree of hotness and
coldness of the air is known
as temperature.
Temperature
Air Pressure
*Air above us presses us with a great force on our
bodies.
*Air pressure is defined as the pressure exerted by
the weight of air on the earth’s surface.
*The air always moves from high pressure areas
to low pressure areas.
Air Pressure
On the moon there is no air and hence no air
pressure. Astronauts have to wear special
protective space suits filled with air when they
go to the moon. If they did not wear these
space suits, the counter pressure exerted by the
body of the astronauts would make the blood
vessels burst. The astronauts would bleed.
Do You Know ?
Wind
*The movement of air from high pressure
area to low pressure areas is called wind.
*Sometimes when the wind blows gently you can
even see it blowing away smoke or fine dust.
*Winds can be broadly divided into three types.
Permanent winds, seasonal winds, local winds
Wind
1. Permanent winds – The trade winds,
westerlies and easterlies are the
permanent winds. These blow constantly
throughout the year in a particular
direction.
2. Seasonal winds – These winds change
their direction in different seasons. For
example monsoons in India.
3. Local winds – These blow only during a
particular period of the day or year in a
small area. For example, land and sea
breeze. Do you recall the hot and dry local
wind of northern planes of India? It is
called loo.
Moisture
THANK YOU

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Geography class 7 lesson air

  • 2. GEO - LESSON 4: AIR
  • 3. What is a Atmosphere ? * Our Earth is surrounded by a huge blanket of air called atmosphere * It provides us the air we breathe and protects us from the harmful effects of the sun’s rays
  • 4. Composition Of The Atmosphere Do you know that the Air we take in while breathing is actullay a mixture of many gases ? •Nitrogen and oxyen are two gases which make up the bulk of the atmosphere. •Carbon dioxide, helium, ozone, argon and hydrogen are found in lesser quantities. •Apart from these gases, tiny dust particles are also present in the air. Yes !
  • 5. Nitrogen (78%) Oxygen (21%) Carbon dioxide (0.03%) Argon (0.93%) All others (0.04%) Pie Chart
  • 6.
  • 8.
  • 9.
  • 10. When air is heated, it expands, becomes lighter and goes up. Cold air is denser and heavy. That is why it tends to sink down. When hot air rises, cold air from surrounding area rushes there to fill in the gap. That is how air circulation takes place Do You Know ?
  • 11. Structure Of The Atmosphere Our atmosphere is divided into five layers starting from the earth’s sur face. These are Troposphere, Stratosphere, Mesosphere, Thermosphere and Exosphere
  • 12. Troposphere: This layer is the most important layer of the atmosphere. Its average height is 13 km. The air we breathe exists here. Almost all the weather phenomena like rainfall, fog and hailstorm occur in this layer. Stratosphere: Above the troposphere lies the stratosphere. It extends up to a height of 50 km. This layer is almost free from clouds and associated weather phenomenon, making conditions most ideal for flying aeroplanes. One important feature of stratosphere is that it contains a layer of ozone gas. We have just learnt how it protects us from the harmful effect of the sun rays.
  • 13. Mesosphere: This is the third layer of the atmosphere. It lies above the stratosphere. It extends up to the height of 80 km. Meteorites burn up in this layer on entering from the space. Thermosphere: In thermosphere temperature rises very rapidly with increasing height. Ionosphere is a part of this layer. It extends between Fig. 4.2: Layers of the Atmosphere 2020-21 AIR 23 Do you know? You will be surprised to know that the earth receives only 1 in 2,000,000,000 parts of the sun’s energy. 80-400 km. This layer helps in radio transmission. In fact, radio waves transmitted from the earth are reflected back to the earth by this layer.
  • 14. Exosphere: The upper most layer of the atmosphere is known as exosphere. This layer has very thin air. Light gases like helium and hydrogen float into the space from here.
  • 15.
  • 16. WEATHER AND CLIMATE Weather is this hour-to-hour, day to day condition of the atmosphere. A hot or humid weather may make one irritable The average weather condition of a place for a longer period of time represents the climate of a place.
  • 17. “Is it going to rain today?” “Will it be bright and sunny today?” How many times have we heard this from anxious cricket fans speculating the fate of a One Day match? If we imagine our body to be a radio and the mind its speaker, weather is something that fiddles with its control knobs. Weather is this hour-to-hour, day to day condition of the atmosphere. A hot or humid weather may make one irritable. A pleasant, breezy weather may make one cheerful and even plan for an outing. Weather can change dramatically from day to day. However, the average weather condition of a place for a longer period of time represents the climate of a place. Now do you understand why we have daily weather forecasts. WEATHER AND CLIMATE
  • 18.
  • 19. The temperature you feel everyday is the temperataure of the atmosphere. The degree of hotness and coldness of the air is known as temperature. Temperature
  • 20.
  • 21.
  • 22. Air Pressure *Air above us presses us with a great force on our bodies. *Air pressure is defined as the pressure exerted by the weight of air on the earth’s surface. *The air always moves from high pressure areas to low pressure areas.
  • 24. On the moon there is no air and hence no air pressure. Astronauts have to wear special protective space suits filled with air when they go to the moon. If they did not wear these space suits, the counter pressure exerted by the body of the astronauts would make the blood vessels burst. The astronauts would bleed. Do You Know ?
  • 25. Wind *The movement of air from high pressure area to low pressure areas is called wind. *Sometimes when the wind blows gently you can even see it blowing away smoke or fine dust. *Winds can be broadly divided into three types. Permanent winds, seasonal winds, local winds
  • 26. Wind
  • 27. 1. Permanent winds – The trade winds, westerlies and easterlies are the permanent winds. These blow constantly throughout the year in a particular direction. 2. Seasonal winds – These winds change their direction in different seasons. For example monsoons in India. 3. Local winds – These blow only during a particular period of the day or year in a small area. For example, land and sea breeze. Do you recall the hot and dry local wind of northern planes of India? It is called loo.
  • 28.
  • 29.
  • 31.
  • 32.
  • 33.
  • 34.
  • 35.
  • 36.