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Atmospheric Pressure: Causes, Variations, Pressure Belts & More | UPSC Notes

Last Updated on Feb 08, 2025
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Atmospheric pressure is a fundamental concept in meteorology and the study of Earth's atmosphere. It refers to the force exerted by the weight of the air above a specific area. It plays a crucial role in weather patterns, air circulation, and climate dynamics. Understanding atmospheric pressure is essential for comprehending various atmospheric phenomena and predicting weather conditions.

Questions related to pressure systems, weather patterns, global circulation, and climate dynamics regularly appear in the UPSC Civil Services Examination. The topic atmospheric pressure UPSC is specifically relevant for the General Studies paper, particularly in the section covering Environmental Science, Climate Change, and Geography.

This article will cover key factors influencing atmospheric pressure, including altitude, temperature, air masses, rotation of the Earth, and solar heating.

Check the article on the Types of Rainfall – NCERT Notes for UPSC here!

GS Paper

General Studies Paper I

Topics for UPSC Prelims

Atmospheric Pressure, High and Low-Pressure Systems, Barometer, Pressure Gradients, Weather Patterns, Influence on Climate, Cyclones

Topics for UPSC Mains

Role of High and Low-Pressure Systems in Weather Formation, Pressure Gradients and Their Effects on Wind Patterns, Impact on Cyclone and Anticyclone Development, Influence on Climate and Weather Variability

What is Atmospheric Pressure?

Atmospheric pressure is also known as barometric pressure. It is expressed as the force per unit area exerted by an atmospheric column. Atmospheric column is defined as the air above the per unit area of the surface. And there is change in the atmospheric column with an increase in height or altitude. Because of this pressure is maximum at sea level and minimum at the end of the troposphere. Every second we are surrounded by atmospheric pressure like the air we inhale has weight. The device which measures atmospheric pressure is called a barometer. The reading of barometric pressure is done either in centimeters or inches and the pressure in the barometer is determined by the movement of the mercury column. One of the major causes of change in atmospheric pressure is air motion i.e., wind which moves from high pressure area to low pressure area.

Causes of Atmospheric Pressure

The atmospheric pressure is primarily caused by the weight of the air above a given location and is influenced by several factors. Here are the key causes of atmospheric pressure:

  • Gravity: The force of gravity pulls the Earth's atmosphere towards its center, resulting in the weight of the air exerting pressure on the surface below. The higher the column of air above a location, the greater the atmospheric pressure.
  • Altitude: Atmospheric pressure decreases with increasing altitude. As one moves higher in the atmosphere, there are fewer air molecules above, leading to lower atmospheric pressure. This is because the weight of the air decreases with altitude.

  • Temperature: Temperature variations affect atmospheric pressure. Warmer air tends to expand and become less dense, leading to lower pressure. Conversely, cooler air contracts and becomes denser, resulting in higher pressure.
  • Air Masses: Differences in temperature and moisture content between air masses contribute to variations in atmospheric pressure. When warm air rises and forms a low-pressure area, surrounding air flows towards it, causing a drop in pressure. Conversely, when cool air sinks and forms a high-pressure area, surrounding air diverges and results in increased pressure.
  • Rotation of the Earth: The rotation of the Earth induces the Coriolis effect, which influences wind patterns. The Coriolis effect causes air to deflect from its original path, creating areas of low and high pressure.
  • Solar Heating: Unequal heating of the Earth's surface by the Sun leads to variations in temperature. This, in turn, affects atmospheric pressure. The equatorial regions receive more direct sunlight, resulting in warmer air and lower pressure. The polar regions receive less sunlight and have cooler air, leading to higher pressure.

Read the article on Heating and Cooling of the Atmosphere!

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Vertical Variation of Atmospheric Pressure

In the lower atmosphere there is a decrease in pressure rapidly with height. For example: at the Mt. Everest, the pressure of air is two-thirds less than what it is at sea level. The level of decrease in pressure with altitude is not the same everywhere. Since there are changes in factors like temperature, amount of water vapour, gravity which control air density. Because of this variability in different factors, there is no simple relationship between altitude and pressure. Decrease in atmospheric pressure is seen on an average at the rate of about 34 millibars every 300 metres of height.

Gradient force of vertical pressure is much larger than that of gradient force of horizontal pressure. But is balanced by approximately equal but opposite gravitational force. Because of this strong upward wind is not experienced. Because of the presence of gravity air is denser at the surface and has high pressure. As pressure is inversely proportional to density and temperature. So, change in either temperature or density will lead to change in pressure. Increasing pressure indicates fine, settled weather whereas decreasing pressure indicates unstable and cloudy weather.

Check the article on the Types of Clouds: Geography NCERT Notes for UPSC here

Horizontal Variation of Atmospheric Pressure

Minute difference in pressure is also considered very important in terms of direction of winds and velocity. Distribution of pressure horizontally is studied by drawing isobars at a constant level. Line which connects places having equal pressure is called isobars. But for reducing the effect of altitude on pressure, it is measured at any station after being reduced to sea level for purposes of comparison.

Rate and direction of pressure changes which is called as pressure gradient is expressed by spacing present in isobar. By this we can define pressure gradient as the decrease in pressure per unit distance in the direction in which the pressure decreases most rapidly. There are several distinct identifiable zones of homogeneous horizontal pressure regimes or ‘pressure belts’. There are seven pressure belts on the Earth surface, they are:

  • equatorial low,
  • the subtropical highs,
  • the subpolar lows, and
  • the polar highs.

Also study the topic: Forces Affecting Velocity And Direction Of Wind!

Pressure Belts of the Earth

Pressure belts of the Earth refer to zones or bands of atmospheric pressure that encircle the planet. These pressure belts are created by the unequal heating of the Earth's surface by the Sun, which leads to variations in air density and pressure. The main pressure belts are the Equatorial Low Pressure Belt (also known as the Intertropical Convergence Zone or ITCZ), the Subtropical High Pressure Belts (North and South), the Subpolar Low Pressure Belts, and the Polar High Pressure Belts. These pressure belts play a crucial role in shaping global wind patterns and weather systems.

Equatorial Low Pressure Belt or ‘Doldrums’

This belt lies between 10°N and 10°S latitudes. The width of this pressure belt may vary between 5°N and 5°S and 20°N and 20°S. This belt is known as Doldrums because of the extremely calm air movements. There is variation in the position of this belt based on the movement of the Sun.

Subtropical High Pressure Belt or Horse Latitudes

The height of this belt extends from near the tropics to about 35°N and S. In this belt subsiding air is warm and dry and that’s why most of the deserts are present along this belt, in both hemispheres.

Sub-Polar Low Pressure Belt

This belt is located between 45°N and S latitudes along with the Arctic and the Antarctic circles (66.5° N and S latitudes). As temperature is low in these latitudes the sub polar low pressure belts are not very well pronounced year long. In the southern hemisphere such belts surround the periphery of Antarctica and are not as well differentiated.

Polar High Pressure Belt

This belt is small in areas and extends around the poles. This belt is situated around poles between 80 – 90° N and S latitudes. In this belt the lowest temperature is found over the poles.

Key Takeaways for UPSC Aspirants

  • Definition: The force exerted by the weight of air above a given point on Earth's surface.
  • Measurement: Measured by a barometer, units are millibars (mb) or inches of mercury (inHg).
  • Sea Level Pressure: Standard atmospheric pressure at sea level is 1013.25 mb.
  • Altitude Effect: Atmospheric pressure decreases as altitude increases because there is less air above the measurement point.
  • Weather Patterns: In general, high pressure means fine and still weather, while low pressure is associated with cloudiness and rain.
  • Pressure Systems: Anticyclones, otherwise known as high pressure systems, and cyclones, otherwise known as low-pressure systems, are of the main elements in meteorology.
  • Isobars: Lines appearing on a weather map joining all places of equal pressure; close spacing indicates a strong wind, and wide spacing, a light breeze.
  • Pressure Belts: The Earth has a number of major pressure belts, including the equatorial low-pressure belt and the subtropical high-pressure belts, that determine global climate and weather patterns.

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Atmospheric Pressure UPSC FAQs

Atmospheric pressure can be expressed in bar by dividing the pressure value in pascals by 100,000, as 1 bar is equal to 100,000 pascals.

1 atmospheric pressure, or 1 atm, is approximately equal to 101.3 kilopascals (kPa) or 1,013 millibars (mbar).

Atmospheric pressure refers to the force exerted by the weight of the Earth's atmosphere on a given area.

Atmospheric pressure is measured by an instrument called a barometer.

Yes, 1 atm (atmosphere) is a unit commonly used to represent average atmospheric pressure value at sea level.

Atmospheric pressure at sea level is approximately 101.3 kilopascals (kPa) or 1,013 millibars (mbar).

The unit of atmospheric pressure is often expressed in pascals (Pa), but other common units include kilopascals (kPa) and millibars (mbar).

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