Precipitation (meteorology)
In
meteorology, precipitation (also known as hydrometeor) is any product of the condensation of
atmospheric water vapor that is deposited on the earth's surface. It occurs when the atmosphere (being a large gaseous
solution) becomes saturated with
water vapour and the water condenses and falls out of solution (i.e., precipitates). Air becomes saturated via two processes, cooling and adding moisture.
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Hydrometeor
(n.)
A meteor or atmospheric phenomenon dependent upon the vapor of water; -- in the pl., a general term for the whole aqueous phenomena of the atmosphere, as rain, snow, hail, etc.
Webster's Revised Unabridged Dictionary (1913), edited by Noah Porter.
About
hydrometeor
hydrometeor
Eng: hydrometeor
Urdu: شہاب آبی ۔ ماجویہ ۔ ماجوی مظاہرہ ۔
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