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contributor authorBott, A.
contributor authorSievers, U.
contributor authorZdunkowski, W.
date accessioned2017-06-09T14:29:54Z
date available2017-06-09T14:29:54Z
date copyright1990/09/01
date issued1989
identifier issn0022-4928
identifier otherams-20386.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156608
description abstractA one-dimensional radiation fog model is presented which includes a detailed description of the interaction between atmospheric radiative transfer and the microphysical structure of the fog. Aerosol particles and activated cloud droplets are treated using a two-dimensional joint size distribution whereby the activation process of aerosols is explicitly modeled. For this purpose a new positive definite semi-Lagrangian advection scheme is developed that produces only small numerical diffusion and is numerically very efficient. For the radiative calculations, time dependent attenuation parameters are determined from the actual particle size distributions. The diffusional growth of the particles is calculated by considering radiative effects in the droplet growth equation. Numerical results elucidate that the strong interaction between the radiatively induced droplet growth and their gravitational settling is responsible for a distinct reduction of the liquid water content which also shows quasi-periodic oscillations with periods of 15?20 min. Application of the model to a measured fog episode demonstrates its ability to predict reasonably well the main features of a fog event. This is also true for the oscillations of the liquid water content which are calculated with timescales similar to the observations.
publisherAmerican Meteorological Society
titleA Radiation Fog Model with a Detailed Treatment of the Interaction between Radiative Transfer and Fog Microphysics
typeJournal Paper
journal volume47
journal issue18
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1990)047<2153:ARFMWA>2.0.CO;2
journal fristpage2153
journal lastpage2166
treeJournal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 018
contenttypeFulltext


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