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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.
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