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Atmospheric pressure. Torricelli’s experiment and Pascal’s Principle.

28/03/2026

The online atmospheric pressure measurement simulations on this page will allow us to better understand what atmospheric pressure is, how we observe it and how we measure it. We will see what Torricelli’s experiment was about, which laid the foundation for modern atmospheric pressure measuring instruments. We will also learn what Pascal’s Principle is.

What is atmospheric pressure

Atmospheric pressure is the force per unit area exerted by the air that forms the atmosphere on the earth’s surface. It is a fundamental phenomenon in the atmosphere and plays a crucial role in various aspects of our daily lives and natural processes.

Atmospheric pressure measurement unit

The IS unit of pressure is the pascal (Pa), named after Blaise Pascal. One pascal is equal to a force of one newton per square meter (N/m²). Other units of measurement are the bar (bar, equivalent to 100,000 Pa), the millimeter of mercury (mmHg), which is based on the experiment performed by Evangelista Torricelli in the 17th century, or the atmosphere (equivalent to 760 mmHg or 1.013 bar).

Variation of atmospheric pressure with altitude

Atmospheric pressure varies with altitude, since the amount of air over a given area decreases as we move away from the earth’s surface. The higher the altitude, the lower the atmospheric pressure. Atmospheric pressure also influences climate and the formation of weather systems. Changes in atmospheric pressure can indicate the arrival of cold or warm fronts, and areas of high and low pressure are responsible for wind patterns and atmospheric currents.

Atmospheric pressure measuring instruments

Barometers are instruments used to measure atmospheric pressure. There are different types, such as the mercury barometer and the aneroid barometer. In addition, weather stations and satellites also collect atmospheric pressure data for weather analysis and prediction.

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Atmospheric pressure measurement simulations

Concept of Pressure


In the first of our online atmospheric pressure measurement simulations, it is possible to observe how the pressure that an object exerts on its base changes when the weight of the object or its contact surface changes.





Torricelli’s experiment


Torricelli’s experiment, performed in 1643, proved the existence of atmospheric pressure. Torricelli filled a glass tube about one meter high with mercury, sealed it and inverted it in a vessel also containing mercury. He observed that the mercury in the tube descended, leaving an empty space at the top, and stabilized at a height of about 76 cm. This phenomenon occurred because the atmospheric pressure pushed the mercury in the vessel upward, balancing the column of mercury in the tube. This experiment led to the invention of the first instrument for measuring atmospheric pressure, the mercury barometer.

Drag the mercury tube into the vessel and see what happens to its level depending on the atmospheric pressure of the planet.






Pascal’s principle


Pascal’s Principle states that a change in pressure applied to an incompressible fluid at equilibrium within a closed vessel is transmitted uniformly in all directions and to all points in the fluid. Pascal’s Principle has a multitude of practical applications in all kinds of hydraulic devices such as presses, brakes, elevators, etc.

In the last of our online atmospheric pressure measurement simulations, you can see how the equilibrium point varies in two connected columns of fluid when the radii of the tubes change.

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Atmospheric pressure is the force exerted by the air in the atmosphere on the Earth’s surface due to the weight of the air column above a given point. Although air seems light, it has mass and therefore exerts pressure in all directions. This pressure decreases with altitude because the amount of air above us becomes smaller as we ascend. Atmospheric pressure plays a key role in weather patterns, wind formation and the behavior of warm and cold fronts. It also affects biological and technological processes such as breathing, boiling point changes and the operation of measuring instruments. Its SI unit is the pascal (Pa), although units like the bar, millimeter of mercury (mmHg) and atmosphere (atm) are also widely used.
Torricelli’s experiment demonstrated that the atmosphere exerts pressure. By filling a glass tube with mercury, inverting it over a dish and observing that the mercury stabilized at 760 mm, Torricelli showed that atmospheric pressure was supporting the column of mercury. This experiment established the millimeter of mercury as a pressure unit. Pascal’s principle states that pressure applied to a confined fluid is transmitted equally in all directions. This explains the operation of hydraulic presses, braking systems and many industrial devices. Together, Torricelli’s experiment and Pascal’s principle provide a foundation for understanding how fluids behave and how pressure is measured in scientific and technological contexts.
Because the higher you go, the less air there is above you. Atmospheric pressure is the weight of the air pressing down, so if the air column is smaller, the pressure is lower. That’s why breathing becomes harder at high altitudes: there is less air and less oxygen.
It showed that the atmosphere has weight and exerts pressure. Torricelli filled a tube with mercury, inverted it and saw that the mercury stayed at about 760 mm instead of falling completely. The only thing holding it up was atmospheric pressure. This experiment led to the invention of the first barometer.
Because changes in pressure help predict the weather. Falling pressure often means storms or bad weather, while rising pressure indicates clear skies. Atmospheric pressure is also important in aviation, diving, cooking at high altitudes and many industrial processes. Barometers allow us to track these changes and understand how the atmosphere behaves.

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