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Density of air - Wikipedia
The density of air or atmospheric density, denoted ρ, is the mass per unit volume of Earth's atmosphere. Air density, like air pressure, decreases with increasing altitude. It also changes with variations in atmospheric pressure, temperature and humidity. At 101.325 kPa (abs) and 20 °C (68 °F), air has a density of … See more
Other things being equal (most notably the pressure and humidity), hotter air is less dense than cooler air and will thus rise while cooler air tends to fall. This can be seen by using the ideal gas law as an approximation. See more
Troposphere
To calculate the density of air as a function of altitude, one requires additional parameters. For the troposphere, the lowest part (~10 km) of the atmosphere, they are listed below, along with their values according to … See moreThe addition of water vapor to air (making the air humid) reduces the density of the air, which may at first appear counter-intuitive. This occurs … See more
Wikipedia text under CC-BY-SA license Air Density Calculator
Use this air density calculator to instantly find how tightly packed an object's molecules are, allowing you to estimate \rho ρ based on the local temperature and pressure conditions. This value is vital for many further calculations, such …
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Density of Air - Density of Dry and Humid Air, Factors …
The formula for density is d = m/v, where d is the density, m is the mass, and v is the volume. In this session, let us discuss the density of air, value of air density, and factors affecting the density of air.
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The density of air depends upon the atmospheric temperature, pressure and humidity. Dry air has a density of 1.29 gram per litre at 0 degree Celsius (32 degrees Fahrenheit) at average sea level. The density of air refers to the mass …
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Online calculator, figures and tables showing density, specific weight and thermal expansion coefficients of air at temperatures ranging -100 to 1600 °C (-140 to 2900 °F) at atmospheric and …
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Density - Wikipedia
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