Parameterization of dry deposition velocity in the atmospheric surface layer

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作者：
Kharchenko, A.I. [1 ]
机构：
[1] Russ. Fed. Nuclear Center - VNIIEF, Mira 37, Sarov 607190, Russia
来源：
Journal of Aerosol Science | 1997年 / 28卷 / SUPPL. 1期
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where x+ is the dimensionless slip factor. The equations(2-4) that are valid to calculate the particles deposition velocity to a thlly absorbing surface of zo< 10 cm roughness for friction wind velocities U; 10-200; cm/s; can be used to set boundary conditions for a semiempirical equation for turbulent diffusion at the upper edge of the atmospheric surface layer; which is where boundary conditions are generally specified for hydrothermodynamics equations. This work has been performed under ISTC Project # 47. REFERENCES Chamberlain A.C. (1967) Transport of lycopodium spores and other small particles to rough surfaces. Proc. of Royal Soc; A; 296; 45-70. Monin A.S; Yaglom AM. (1965) Statistical hydromechanics. V. 1. -M.: Nauka. Sehmel G.A. and Hodgson WH. (1978) A model for predicting dry deposition of particles and gases to environmental surfaces. PNL-SA-6721; Battelle; Pacific Northwest Laboratories; Richland; WA. Sehmel G.A. (1984) Deposition and resuspension. In Atmo; wheric science and power production (edited by Randerson D.); 533-583;
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