vertical flux

vertical flux

In dry deposition this refers to the rate at which a gas particle is deposited onto another surface without the aid of precipitation. Vertical flux equals concentration of the species multiplied by the deposition velocity.

[International Journal of Heat and Mass Transfer; v31n11; 2291; 1988.] [Journal of Atmospheric Sciences; v48n11; 1909; 1991.]

Source: Atmospheric Chemistry Glossary

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