A numerical method for determining the dry deposition of atmospheric trace gases

摘要: A diagnostic deposition model based on generally accepted micrometeorological ideas the transfer of momentum, sensible heat and matter near Earth's surface is presented. The parameterization fluxes flux-gradient relationships in turbulent region layer sublayer Stanton number as well Reynolds analogy between concentration, temperature wind velocity distributions underlying sublayer. requires only vertical profile data velocity, dry- wet-bulb temperatures trace gas concentrations from part layer.