Summary

by the National Weather Service Aviation Weather: For Pilots and Flight Operations Personnel… (1975)

Atmospheric Pressure and Altimetry When you understand pressure, its measurement, and effects of temperature and altitude on pressure, you can more readily grasp the significance of pressure and its application to altimetry.
Atmospheric Pressure Atmospheric pressure is the force per unit area exerted by the weight of the atmosphere. Since air is not solid, we cannot weigh it with conventional scales. Yet, Toricelli proved three centuries ago that he could weigh the atmosphere by balancing it against a column of mercury.
Source: Wikisource

by the National Weather Service Aviation Weather: For Pilots and Flight Operations Personnel… (1975)

Density Altitude What is density altitude? Density altitude simply is the altitude in the standard atmosphere where air density is the same as where you are. Pressure, temperature, and humidity determine air density. On a hot day, the air becomes "thinner" or lighter, and its density where you are is equivalent to a higher altitude in the standard atmosphere—thus the term "high density altitude". On a cold day, the air becomes heavy; its density is the same as that at an altitude in the standard atmosphere lower than your altitude—"low density altitude".
Source: Wikisource

by the National Weather Service Aviation Weather: For Pilots and Flight Operations Personnel… (1975)

Pressure Variation Pressure varies with altitude and temperature of the air as well as with other minor influences which we neglect here.
Altitude
As we move upward through the atmosphere, weight of the air above becomes less and less. If we carry a barometer with us, we can measure a decrease in pressure as weight of the air above decreases. Within the lower few thousand feet of the troposphere, pressure decreases roughly one inch for each 1,000 feet increase in altitude. The higher we go, the slower is the rate of decrease with height.
Source: Wikisource

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