quantity

atmospheric pressure

The pressure exerted by the weight of the Earth's atmosphere, approximately 101.325 kilopascals at sea level.
16 related articles

Description

Atmospheric pressure is the force per unit area exerted by the weight of the air column above a given point. At sea level, this pressure averages about 101.325 kilopascals (or 1 atmosphere). It decreases exponentially with altitude, roughly halving every 5.6 kilometers. This pressure is not just a static weight—it drives weather systems, affects boiling points, and is essential for life as we know it.

History

Evangelista Torricelli invented the mercury barometer in 1643, providing the first reliable measurement of atmospheric pressure. Blaise Pascal later demonstrated that pressure decreases with altitude, confirming the concept of an air 'ocean'.

How it works

Air molecules are constantly in motion, colliding with surfaces and each other. The cumulative effect of countless molecular collisions on a surface creates pressure. Gravity pulls air molecules toward Earth, creating a gradient: more molecules near the surface, fewer higher up. The pressure at any height is simply the total weight of air above that point. Variations in temperature and humidity cause air to expand or contract, creating high- and low-pressure systems that drive winds and weather.

In practice

Atmospheric pressure is fundamental to meteorology (weather forecasting), aviation (altimeters), and medicine (hyperbaric chambers). It also determines the boiling point of water, which is why cooking times change at high altitudes.

Fun fact

The pressure at the bottom of the Mariana Trench is over 1,000 times greater than at sea level—equivalent to having about 50 jumbo jets stacked on your big toe.

Concept graph →

Related articles · 16

Cosmology2026-07-223 minarXiv:2607.19938
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General Relativity2026-07-082 minarXiv:2607.07741express
Cosmic Mirage: How the Solar Bubble Is Reshaping the Map of the Universe
The cosmological debate is like two craftsmen measuring the same wall but getting different lengths. One uses a tape measure, applying it to nearby landmarks — Cepheids (pulsating beacon stars) and Type Ia supernovae (flashes of dying stars). He finds the wall is stretching at 73.5 arbitrary units.
Storm Mosaic: AI Model STRATA Pieces Together Global Weather
For decades, global atmospheric models resembled artists forced to paint planetary storms with coarse brushstrokes: a resolution of 25–100 km forced them to 'guess' convection through approximate schemes, introducing systematic errors in rainfall and climate forecasts.
Instrumentation2026-06-082 minarXiv:2606.09116express
How Stratospheric Weather Alters Particle Counters Deep Underground
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Freo Doctor: How Wind Governs the Fate of Meteorites
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Plasma Physics2026-05-242 minarXiv:2605.25060express
Invisible Fire: How Plasma Cools by Emitting Light
Imagine a powerful hair dryer that blows not warm air but white-hot plasma, such devices are called plasma wind tunnels. They are used to test on Earth how a spacecraft will enter the atmosphere.
Fluid Dynamics2026-04-192 minarXiv:2604.17636express
Bubbles vs. Friction: How Air Makes Ships Faster
A ship gliding through water constantly rubs against it, like a palm against a rough surface. This friction eats fuel and slows progress. One way to reduce it is to blow air under the hull: water stops sticking to the hull, and drag drops. But air is finicky: sometimes it helps, sometimes it hurts.
Water Under Pressure: Why It Flows Faster
Water deep within the Earth is compressed more than a thousandfold compared to the surface. Even there, it continues to flow, but its internal structure changes. Researchers measured how water resists flow and compression as pressure rises from zero to 1.6 gigapascals — equivalent to placing a 16-ton weight on every square centimeter.
Machine Learning2026-02-261 minarXiv:2602.23146express
Weather in Every Backyard
The weather on the next street can differ from yours: cooler by the river, hotter over asphalt, windier between buildings. A regular forecast misses this: its grid cell is the size of a city, not a backyard.
q-bio.TO2026-02-191 minarXiv:2602.17265express
Lungs Like a City: How Air Flows Through Bronchial Streets
A lung scan reveals a tree: the trunk is the trachea, branches are the bronchi, and leaves are the alveoli. But how does air spread through these branches? Scientists built a computer model that replicates the lung's shape from images obtained via computed tomography.
Applied Physics2026-01-302 minarXiv:2601.23117express
A Tuning-Fork Membrane for Vacuum
A thin film of silicon nitride is stretched over a frame like the skin of a drum. The slightest nudge from gas molecules makes it tremble. A laser beam delivered through a glass fiber picks up that trembling and turns it into a pressure reading. The whole setup fits in a pocket, not on an optical table.
Muons as a Thermometer for Cyclones
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Why the Planet Hit the Brakes on Warming for a Quarter Century
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nlin.AO2021-07-023 minarXiv:2107.00843
Ozone Sings in Many Voices: How Climate Stratifies by Altitude
In the vast concert hall of the atmosphere, ozone plays a part that changes from tier to tier. Near the surface, its notes sound alarming, for there it is a pollutant that irritates lungs and leaves. At 25 kilometers up, the same gas becomes a protective shield that absorbs harsh ultraviolet radiation.
A Thermometer That Hears India's Pulse
The thermometer at a weather station in Delhi doesn't know it's part of a giant ear. Every day it records the temperature, and after forty years of such records, you can hear the breathing of an entire subcontinent. The India Meteorological Department divided the country's land into one-degree squares and took readings from 1970 to 2009.
How Ripples on Water Steer the Planet's Winds
The planet's winds are not free-flowing currents but rather obedient jets that can be nudged from an unexpected direction. The ocean surface, covered with waves, acts like a tuning knob: change its roughness, and giant air rivers shift by hundreds of kilometers.