barometric law قانون ِ فشارسنجی، ~ فشارسنجیک qânun-e fešârsanji, ~ fešârsanjik Fr.: loi barométrique A law which describes the vertical pressure distribution in the
lower parts of Earth’s atmosphere.
The atmospheric pressure decreases exponentially from any reference
surface as the altitude increases. See also: → barometer; → law. |