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Composition and Structure of the Atmosphere, Layers, Diagram

Structure of the Atmosphere

The atmosphere is the air surrounding our planet consisting of layers of gases that are essential for life like oxygen for humans and carbon dioxide for plants. These layers are held by gravity, it protects us from harmful UV rays and maintains a suitable temperature for living things. While it extends up to about 1600 kilometers above Earth, 99 percent of its mass is within just 32 kilometers from the surface.

The atmosphere is structured in distinct layers, each with unique properties, such as temperature and composition. You can think of it like a multi-layered cake, where each layer serves a specific function. Earth’s atmosphere consists of five main layers: the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Each layer varies in its composition, temperature, and altitude. Let us take a closer look at these layers along with a diagram.

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Composition of the Atmosphere

Earth’s atmosphere is made up of about 78% nitrogen, 21% oxygen, and 1% other gases. Nitrogen (N2) is the most abundant gas and is essential for the survival of all living organisms. Oxygen (O2) is vital for humans and animals, who breathe it in, while green plants produce it during photosynthesis, helping to keep oxygen levels stable. Carbon dioxide (CO2) is another important gas it acts as a greenhouse gas, primarily coming from the burning of fossil fuels. These gases are distributed in atmospheric layers, each characterized by different temperature and pressure conditions.

Carbon Dioxide

  • Carbon dioxide is very important in meteorology.
  • It is transparent to incoming sunlight but blocks some of the Earth’s emitted radiation.
  • It reflects some of this radiation back to Earth’s surface.
  • Carbon dioxide is a major cause of the greenhouse effect.
  • Its levels have been rising due to the burning of fossil fuels. This increase in carbon dioxide is the main cause of global warming.
  • Carbon dioxide is a colorless and odorless gas. It is soluble in water, ethanol, acetone and has the following properties:
  1.  Melting Point: -55.6 deg
  2. Boiling Point: -78.5 Degree
  3. Density: 1.977

Ozone Gas

  • Ozone is an important part of the atmosphere, contains high concentrations of Ozone(O3)
  • Ozone is a very reactive gas and attacks other molecules in the air, often regenerating oxygen in the process
  •  It is mostly found 10 to 50 kilometers above Earth’s surface.
  • Bluish Gas that harmful to breathe
  •  Ozone acts like a shield, absorbing the Sun’s harmful ultraviolet (UV) rays and preventing them from reaching the ground.
  •  The small amount of ozone in the atmosphere is in the stratosphere’s ozone layer.
  • Although it represent only a tiny fraction of the atmosphere, Ozone is essential for life on Earth

Water Vapour

  • Water vapor is the gas form of water in the atmosphere.
  • Responsible for all types of precipitation.
  • Less water vapor at higher altitudes, decreases from the poles to the equator.
  • Can make up to 4% of the atmosphere in warm, humid areas.
  • Enters the air mainly through evaporation from oceans, rivers, lakes, and transpiration from plants.
  • Water vapor is the most common greenhouse gas on Earth.
  • Accounts for about half of the greenhouse effect, trapping the Sun’s heat in the atmosphere.
  • Greenhouse gases keep Earth warm enough for life; without them, Earth would be about 59°F (33°C) colder.
  • Important part of the water cycle, changing between liquid, ice, and gas as it moves through the air, land, and oceans.

Layered Structure of the Atmosphere

Depending upon temperature there are five layers in the Structure of the atmosphere. These are:

  • Troposphere
  • Stratosphere
  • Mesosphere
  • Thermosphere
  • Exosphere

structure of atmosphere

Troposphere

Troposphere
  • It is considered the lowest layer of Earth’s atmosphere.
  • Starts from the surface of the earth and goes up to the height of 8 Kms to 18 Km
  • All kinds of weather changes happen in this layer
  • Temperature decreases with increasing height of the atmosphere at the rate of 1 degree Celsius for every 165 m of the height
  • Tropopause, the transitional zone, separates the Troposphere and the Stratosphere.

Stratosphere

Stratosphere
  • The second layer of the atmosphere above the troposphere.
  • Extends up to 50 kilometers above Earth’s surface.
  • Extremely dry due to low water vapor content.
  • Located above stormy weather, with strong, consistent horizontal winds.
  • Contains the ozone layer, which absorbs UV rays and protects Earth from harmful radiation.
  • The Stratopause separates the Stratosphere from the Mesosphere.

Mesosphere

Mesosphere
  • The Mesosphere is above the Stratosphere.
  • It is the coldest layer of the atmosphere.
  • Starts at 50 km and extends up to 80 km above Earth’s surface.
  • Temperature decreases with height, reaching -100°C at 80 km.
  • Meteors burn up in this layer.
  • The Mesopause is the boundary between the Mesosphere and the Thermosphere.

Thermosphere

Thermosphere
  • Located between 80 and 400 km above the Mesopause.
  • Reflects radio waves emitted from Earth.
  • Temperature increases with height in this layer.
  • Contains satellites and the aurora.

Ionosphere

Ionosphere
  • The lower thermosphere is called the Ionosphere.
  • Composed of ions, which are electrically charged particles.
  • Ionized by cosmic and solar radiation.
  • Located 80 to 400 kilometers above the Mesopause.

Exosphere

Exosphere
  • The Exosphere is the topmost layer of the atmosphere.
  • Atoms and molecules can escape into space from this region.
  • Extends up to 10,000 kilometres from the top of the thermosphere.
  • Gases are very sparse due to the lack of gravitational force.
  • Air density is very low in this layer.

Structure of the Atmosphere UPSC Facts

  • From lowest to highest, the major layers are the troposphere, stratosphere, mesosphere, thermosphere and exosphere.
  • About 78% of the gases in the Earth’s atmosphere are nitrogen, 21% are oxygen, 0.9 % are argon, and 0.1 % are other gases.
  • The remaining 0.1 per cent of gases includes trace amounts of neon, water vapour, methane, carbon dioxide, and methane.
  • The thermosphere is the hottest layer.

 

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Indus River System
Climate of India
Rivers of India
Tributaries of Ganga
National Parks in India
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Wildlife Sanctuaries of India
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FAQs

What is the atmosphere made of?

About 78% of the gases in the Earth's atmosphere are nitrogen, 21% are oxygen, 0.9 % are argon, and 0.1 % are other gases. The remaining 0.1 per cent of gases includes trace amounts of neon, water vapour, methane, carbon dioxide, and methane.

How does the composition and structure of the atmosphere insulate the earth?

The atmosphere acts as a thick layer of insulation, shielding the planet. The Greenhouse Effect is what happens when heat from the Sun is absorbed and kept inside the atmosphere, keeping the Earth warm.

What is the best definition of atmosphere?

The gaseous envelope of a celestial body (such as a planet): the whole mass of air surrounding the earth.

What are the main 5 layers of the atmosphere?

From lowest to highest, the major layers are the troposphere, stratosphere, mesosphere, thermosphere and exosphere.

Which layer is the hottest?

The Thermosphere.

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