Scale height

In physics, a scale height, usually denoted by the capital letter H, is a distance (vertical or radial) over which a physical quantity decreases by a factor of e (the base of natural logarithms, approximately 2.718). == Scale height used in a simple atmospheric pressure model == For planetary atmospheres, scale height is the increase in altitude for which the atmospheric pressure decreases by a factor of e.

Source: Wikipedia — Scale height (CC BY-SA 4.0)

Scale height

In physics, a scale height, usually denoted by the capital letter H, is a distance (vertical or radial) over which a physical quantity decreases by a factor of e (the base of natural logarithms, approximately 2.718). == Scale height used in a simple atmospheric pressure model == For planetary atmospheres, scale height is the increase in altitude for which the atmospheric pressure decreases by a factor of e.

Source: Wikipedia "Scale height" · CC BY-SA 4.0

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