Atmospheric pressure
Atmospheric pressure (air pressure or barometric pressure - after the barometer) is the pressure within the Earth's atmosphere, i.e., the force per unit area exerted against a surface by the air column's weight above that surface within its atmosphere.
etm: Gr atmos ('vapor' or 'steam') + sphaira ('sphere') + Latin pressura ('action to press')
The standard reference of atmospheric pressure (1 atm) is 101,33 Pa = 101.33 kPa = 101.33kPa/100 = 1013.3 bar.
[2] A value of 29.92 inHg (inches of mercury) or 14.6 PSI is used to determine the average-day sea level pressures. Any value below 29.92 inHg would be considered low pressure and anything above would be high pressure.