Atmospheric pressure is the weight of a column of air over its cross section, and its height is equal to the thickness of the atmosphere. It consists of several gases (nitrogen 78% and oxygen 21%, in addition to other gases). Areas of lower atmospheric pressure have less atmospheric mass, while regions of higher atmospheric pressure have more atmospheric mass.
Low air pressure is formed when the temperature rises, as this causes air molecules to accelerate and move away from each other.
Higher atmospheric pressure is formed when the temperature is low, as this causes the air molecules to slow down and move closer together.
The atmospheric pressure varies at the surface of the earth, up to the mesosphere, and the atmospheric pressure changes according to the weather condition.
Atmospheric pressure decreases with altitude from the surface of the earth, and thus less oxygen in the atmosphere, which has an effect on living organisms that breathe the air, and need oxygen in their breathing. And the effect of height on humans is as follows:
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