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Air Class 7 Social Science Geography Chapter 4 CBSE Notes - 2025-26

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Social Science Geography Notes for Chapter 4 Air Class 7 - FREE PDF Download

CBSE Class 7 Geography Chapter 4 is an important chapter of this syllabus that explains the different aspects, facts, and concepts of air. Students will need comprehensive notes to study this chapter well. To make it easier, the subject experts of Vedantu have compiled the ideal notes to follow and take your preparation to the next level. Understand these concepts well from these notes and learn how to formulate answers by using them.


Air is the standard term for a mixture of gases that constitute the Earth’s atmosphere. The gas is chiefly nitrogen, mixed with argon, water vapour, oxygen, trace gases, and carbon dioxide. Air contributes to a significant factor for the survival of living creatures. In this chapter, students will learn the significance of air and how it is essential for our survival. Students can refer to the Class 7 Geography Chapter 4 Notes to understand elaborate explanations on the structure of the atmosphere, composition of the atmosphere, climate, weather, and so on.

Access Class 7 Geography Chapter 4 - Air

In CBSE Class 7 Social Science geography Chapter 4, you come to learn about air. As we all know, the earth is surrounded by an atmosphere that acts as a blanket of air. It is vital for the survival of living beings on earth. We breathe the air provided by the atmosphere.


Harmful sun rays are protected because of it. Without an atmosphere, the temperatures on the earth would have been extreme and unsuitable for living. Without the atmosphere in the morning, the temperatures would be highly high, while at night, it would be freezing. We would be baked alive in the day without the atmosphere. 

 

The Atmosphere and Its Composition:

  • Air is a mixture of gases. Nitrogen and oxygen contribute to the bulk of the atmosphere. Other gases present in low quantities are carbon dioxide, hydrogen, ozone, helium, and argon. In the atmosphere tiny dust particles are present.

  • Nitrogen: forms 78% of the atmosphere. The plants need it for their survival. Nitrogen cannot be directly taken in from the air by plants. Hence, bacteria living in soil and roots of the plants take nitrogen from the atmosphere and change it into usable forms for the plant. 

  • Oxygen: is the second most abundant in the atmosphere. It is essential for humans and animals as it is used for breathing and respiration. Plants produce oxygen by the method of photosynthesis. Oxygen content in the air hence remains stable. Imbalance occurs when there is cutting down of trees. 

  • Carbon Dioxide: is another vital gas in the atmosphere. Green plants use it for photosynthesis, in which food is produced. Oxygen is released in the process. Human beings and animals release carbon dioxide. The carbon dioxide released from respiration and taken in for photosynthesis by plants create a perfect balance. The imbalance occurs when fossil fuels are burned. They are responsible for adding tons of carbon dioxide to the atmosphere.

 

Structure of the Atmosphere: 

  • It is divided into five layers: Troposphere, Stratosphere, Mesosphere, Thermosphere, and Exosphere.

  • With an average height of 13 kilometres, the troposphere is the most vital layer of the atmosphere. It has all the gases, including oxygen which is used for breathing. Weather phenomena like rainfall, fog, and hail storms occur in this region.

  • The stratosphere has a height of 50 kilometres and is free from weather phenomena and clouds. Conditions here are ideal for flying aeroplanes. It contains a layer of ozone that protects us from the harmful UV rays of the sun.

  • The mesosphere is above the stratosphere and extends up to a height of 80 kilometres. When meteorites enter this layer from space, they burn up.

  • The thermosphere extends between 80 kilometres to 400 kilometres. Herewith increasing height temperature rises rapidly. One of the parts of the thermosphere is the ionosphere. This layer is responsible for radio transmission. Radio waves transmitted are reflected by this layer. 

  • The exosphere forms the uppermost layer of the atmosphere. It has gases like helium and hydrogen.

 

Weather and Climate: 

Weather is the condo of the atmosphere at a particular time at a specific place. Weather changes occur within a day, and these changes can be dramatic. Average weather conditions calculated in an area over a long period are termed as the climate of that place. There are various components of the weather and climate. These parameters are the same for both. Some of these parameters or features are:

 

Temperature:

  • The temperature of the atmosphere can be defined as the degree of hotness or coldness of the air.

  • Temperature varies from day to night, from season to season. During summers, temperatures are higher than in winters. 

  • Insolation or the incoming solar energy intercepted by the earth acts as an essential factor in influencing temperatures on earth.

  • The insulation amount decreases from equator to pole, and so does the temperature. Poles are covered with ice for the same reason.

  • Cities have a higher temperature than villages since cities have buildings made of concrete and metal, which gets highly heated up during the day and releases heat at night. High-rise crowded buildings in cities trap warm air, and this raises the temperature in the region.

 

Air Pressure:

  • Air pressure is because of the pressure exerted by the air column. 

  • As we go up in the atmosphere, air pressure decreases rapidly. It is higher at sea level and decreases with height.

  • The temperature of a given place influences the horizontal distribution of air pressure.

  • Where temperatures are high, the air gets heated and becomes light. This air rises, thus creating a low-pressure trough. Low-pressure areas are associated with cloudy skies and wet weather. 

  • In regions with lower temperatures, the air is cold and heavy, shrinking and creating a high-pressure space. This area is associated with clear skies and sunny weather.

  • Air always tends to move from the high-pressure region to a low-pressure part. 

 

Wind: 

  • Movement of air is defined as air, from an area of high pressure to a place of low pressure. 

  • Winds are of three types- permanent winds, local winds, and seasonal winds. 

  • Permanent winds are the trade winds, easterlies, and westerlies. These winds constantly blow in a particular direction throughout the year.

  • Seasonal winds are winds that change the rules with changing seasons. The monsoon winds in India are seasonal.

  • Local winds are which blow only at a particular time of the day or year in a restricted area. Land breeze and sea breeze in the coastal regions are local winds, loo in the northern plains is also a local wind. 

 

Moisture:

  • The moisture content in the air at a given time and place is called the humidity at that place. 

  • Water evaporates from the body of water to form water vapour. When there is an excess of water vapour in the air, we call it a humid day.

  • With rising temperatures, the water holding capacity of the air increases. On humid days clothes take a longer time to dry, we feel sweaty and uncomfortable 

  • Rising water vapours aggregate to form clouds. When clouds cannot further hold moisture, they pour down in the form of precipitation.

  • Jet planes leave behind white trails of moisture that have been condensed in their engines. These white trails are visible till air disturbances dissolve them. 

  • Rain forms due to precipitation. Groundwater is primarily stored rainwater. Plants are instrumental in water preservation. If trees on hill slopes are cut down, rainwater flows down and floods the low-lying areas. 

  • Rainfalls are three types: convectional rainfall, orographic rainfall, and cyclonic rainfall. Rainfall is significant for the survival of living beings on the earth as it gets freshwater to the surface water. Scarcity and drought occur in the absence of rainfall, but if there is an excess of rainfall, floods take place. 

  • Cyclones are rotating storms with a low-pressure centre termed as the eye of the hurricane. Cyclones are associated with large-scale destruction and damage to life and property. 

  • Odisha is on the east coast of India and is a central cyclone-prone area. 

  • Storms originating in the Bay of Bengal hit this state and caused widespread destruction.

 

Important Questions and Answers

1. What are the three types of rainfall? Name one place which experiences each type of rainfall.

Ans: The three types of rainfall are:

  • Convectional Rainfall: This type of rain is not prominent in India. It occurs in equatorial regions where the temperature is exceptionally high, and water from water bodies evaporates due to extreme heat and after condensation comes down as precipitation. 

  • Orographic Rainfall: This rainfall is experienced on the windward side of the Western Ghats in India. The Western Ghats forces the moisture-laden winds from the Arabian Sea to rise and cause rain.

  • Cyclonic Rainfall: Cyclonic Rainfall is experienced in parts of Odisha when the cyclones originating over the Bay of Bengal hit Odisha.

 

2. Define the atmosphere. Why is it important for us?

Ans: The atmosphere can be defined as a blanket of air surrounding the Earth. 

Atmosphere saves us from the harmful UV rays of the sun. It protects us from incoming meteorites. It provides air that every living being breathes in.

 

3. What is the greenhouse effect and which gas is associated with it?

Ans: The incoming solar radiations of the sun are trapped inside the earth, which results in Its warming up. This causes the temperatures of the planet to rise. 

The primary greenhouse gas is carbon dioxide. Methane, chlorofluorocarbons are few greenhouse gases. 

 

4. What do you understand by the term weather?

Ans: Weather can be defined as the condition of the weather at a particular time and place. The weather of an area may change over a day drastically. 

The parameters associated with air are temperature, air pressure, humidity, etc.

 

5. What is air pressure?

Ans: Air pressure can be defined as the pressure exerted by the column of air of the earth on the planet's surface. 

Air pressure decreases with increasing altitude. The highest air pressure is measured at sea level.

 

6. What is insolation?

Ans: Insolation is the amount of solar radiation intercepted by the atmosphere of the earth. It quantifies the solar energy incident on a specific area on land over a given period. 

 

There are two units of insolation: a. kilowatt hours per square metre per day (kWh/sq.)/day - of solar energy hitting an area on a day b watts per square metre (W/sq.)- the average amount of solar energy (or power) intercepting an area annually, i.e., over one year. Insolation decreases with the distance from the equator to the poles.

 

7. Give a reason why wet clothes take longer to dry in humid weather.

Ans: On a humid day, the moisture content of the air is already high. So, it cannot accommodate further moisture and takes longer to absorb moisture from the clothes. Hence, it takes very long to dry clothes on a humid day.


Importance of CBSE Class 7 Geography Chapter 4 Air Notes

CBSE Class 7 Geography Chapter 4 Air Notes is a crucial chapter that has been included in the Class 7 Geography syllabus to develop a conceptual foundation among the students. They will learn what air is and how the atmosphere is formed from this chapter. Hence, they will need the support of the comprehensive study material to grab hold of the concepts.

The revision notes prepared by the experts will become an integral part of this study material students use to prepare for this chapter. These notes are designed by following the latest CBSE Class 7 syllabus to cover all the topics included in the chapter. The precise version of all these topics is simple enough to understand and to focus on the preparation.

The notes can be perfectly used as revision material before an exam. Students will not have to go through the entire chapter. They can perfectly use these notes to memorise the concepts and recall them faster. The easier version of these concepts will aid in compiling the right answers to all the exam questions.


Benefits of CBSE Class 7 Geography Chapter 4 Air Notes

  • The notes will offer a concise format of the chapter to make your revision faster and better.

  • You will be able to recall what you have studied precisely to formulate the right answers.

  • Save your precious time by downloading these notes and following them during your study sessions.

Download CBSE Class 7 Geography Chapter 4 Air Notes PDF

Get the free PDF version of these notes and prepare this chapter exceptionally. Develop your concepts for this chapter by using these notes and learn the concepts properly. Revise and recall the concepts better during an exam and score well to stay ahead of the competition.


Conclusion 

Vedantu's free PDF notes on CBSE Class 7 Geography Chapter 4, "Air," provide a valuable educational resource for students. These notes comprehensively cover the diverse aspects of Earth's atmosphere, from its composition to its role in supporting life and the challenges it faces. Tailored to the CBSE curriculum, they ensure students have access to high-quality study materials.


Vedantu's commitment to offering free, accessible educational content is commendable, empowering students to explore the intricacies of our planet's air. These notes facilitate a deeper understanding of this essential component of our environment, fostering an appreciation for its significance and the importance of preserving its quality. By utilizing these resources, students can enhance their geographical knowledge, critical thinking skills, and overall academic performance, making them an indispensable asset for geography enthusiasts and educators alike.


Related Study Materials for Class 7 Geography Chapter 4 Air

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Study Materials for Geography Class 7 Chapter 4 Air

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Class 7 Chapter 4 Air NCERT Solutions

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Class 7 Chapter 4 Air Important Questions


Chapter-wise Class 7 Geography Notes PDF - FREE Download


Other Bookwise Revision Notes Links for Class 7 Social Science


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FAQs on Air Class 7 Social Science Geography Chapter 4 CBSE Notes - 2025-26

1. What are the key concepts to summarise about the composition of the atmosphere from Chapter 4?

For a quick revision, remember that our atmosphere is primarily a mixture of gases. The main components are Nitrogen (78%), essential for plant life, and Oxygen (21%), which we breathe. The remaining 1% includes gases like Carbon Dioxide (used by plants for photosynthesis), Argon, and others, along with dust particles and water vapour.

2. How can I quickly revise the five layers of the atmosphere and their main function?

The atmosphere's structure is divided into five layers based on temperature. For revision, focus on their key roles:

  • Troposphere: The lowest layer where all weather events, like rain and clouds, happen.
  • Stratosphere: Contains the vital ozone layer, which protects us from the sun's harmful ultraviolet rays.
  • Mesosphere: This is where meteorites burn up as they enter the atmosphere.
  • Thermosphere: In this layer, temperature rises drastically. It also contains the ionosphere, which helps in radio transmission.
  • Exosphere: The final frontier, this uppermost layer is very thin and gradually merges with outer space.

3. What is the fundamental difference between weather and climate?

The core difference is the timescale. Weather refers to the short-term, hour-to-hour or day-to-day condition of the atmosphere at a specific place. For example, 'It is sunny today.' In contrast, climate is the average weather condition of a place over a very long period, usually more than 25 years. For example, 'The climate of Rajasthan is hot and dry.'

4. Why is the atmosphere essential for life beyond just providing air to breathe?

The atmosphere acts as a crucial protective blanket for Earth. It moderates our planet's temperature by trapping heat through the greenhouse effect, preventing extreme differences between day and night. Furthermore, the ozone layer within the stratosphere shields all living things from the sun's harmful and dangerous ultraviolet (UV) radiation.

5. How does air pressure create wind?

Wind is simply the movement of air caused by differences in air pressure. Air always flows from an area of high pressure to an area of low pressure. This movement is nature's way of balancing the pressure difference. The greater the difference in pressure between two locations, the faster the wind will blow.

6. What are the three main types of rainfall to remember for this chapter?

As per the NCERT syllabus for Class 7, there are three main mechanisms or types of rainfall:

  • Convectional Rainfall: Occurs when the land heats up, causing the air above it to warm and rise. As it rises, it cools, condenses, and forms clouds, leading to rainfall.
  • Orographic Rainfall: Happens when moist air is forced to rise over a mountain or a high relief barrier. The air cools as it ascends, leading to precipitation on the windward side of the mountain.
  • Cyclonic Rainfall: This type of rainfall is associated with cyclones or depressions, where warm and cold air masses meet, and the warmer, lighter air is forced to rise over the colder, denser air.

7. What is the significance of moisture in the atmosphere?

Moisture in the atmosphere, known as humidity, is crucial for the water cycle and weather patterns. When this water vapour rises, it cools and condenses to form clouds. When these droplets become too heavy to stay suspended in the air, they fall to the Earth as precipitation (rain, snow, or sleet), which is essential for all forms of life.