Atmospheric pressure Guide, Meaning , Facts, Information and Description
Atmospheric pressure is the pressure caused by the weight of air above any area in the Earth's atmosphere. Standard atmospheric pressure (atm) is discussed in the next section.Air masses are affected by the general atmospheric pressure within the mass, creating areas of high and low pressure.
As elevation increases, fewer air molecules are above. Therefore, atmospheric pressure decreases with increasing height. The following relationship is a first-order approximation:
- ,
A column of air, 1 square inch in cross section, measured from sea level to the top of the atmosphere would weigh approximately 14.7 lb. A 1 m2 column of air would weigh about 10 tonnes. See density of air.
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Standard atmospheric pressure
Standard atmospheric pressure or "the standard atmosphere" (1 atm) is defined as 101.325 kPa. (see also Standard temperature and pressure)
This can also be stated as:
- 29.92 inches of mercury
- 760 mm of mercury
- 760 torr
- 1013.25 millibars (mb)
- 14.7 psia or 0 psig
- 0.967838490064855 at (metric atmospheric pressure).
In a low atmospheric pressure system the atmospheric pressure of the air mass is lower than that of the surrounding air. Low atmospheric pressure systems are symbolized by an L on a weather map and are associated with areas of storminess and precipitation. Wind movement is cyclonic around a low pressure system and cold fronts and warm fronts are generally connected to them.
In a high atmospheric pressure system the atmospheric pressure of the air mass is higher than that of the surrounding air. High atmospheric pressure systems are symbolized by an H on a weather map and are associated with areas of clear weather.
It is possible to demonstrate atmospheric pressure in a classroom or home environment using the crushing can experiment. See Atmospheric pressure demo
This is an Article on Atmospheric pressure. Page Contains Information, Facts Details or Explanation Guide About Atmospheric pressure See also
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