Numerical Simulation of Cloud–Clear Air Interfacial Mixing: Homogeneous versus Inhomogeneous MixingSource: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 008::page 2493Author:Andrejczuk, Miroslaw
,
Grabowski, Wojciech W.
,
Malinowski, Szymon P.
,
Smolarkiewicz, Piotr K.
DOI: 10.1175/2009JAS2956.1Publisher: American Meteorological Society
Abstract: This note presents an analysis of several dozens of direct numerical simulations of the cloud?clear air mixing in a setup of decaying moist turbulence with bin microphysics. The goal is to assess the instantaneous relationship between the homogeneity of mixing and the ratio of the time scales of droplet evaporation and turbulent homogenization. Such a relationship is important for developing improved microphysical parameterizations for large-eddy simulation of clouds. The analysis suggests a robust relationship for the range of time scale ratios between 0.5 and 10. Outside this range, the scatter of numerical data is significant, with smaller and larger time scale ratios corresponding to mixing scenarios that approach the extremely inhomogeneous and homogeneous limits, respectively. This is consistent with the heuristic argument relating the homogeneity of mixing to the time scale ratio.
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contributor author | Andrejczuk, Miroslaw | |
contributor author | Grabowski, Wojciech W. | |
contributor author | Malinowski, Szymon P. | |
contributor author | Smolarkiewicz, Piotr K. | |
date accessioned | 2017-06-09T16:28:10Z | |
date available | 2017-06-09T16:28:10Z | |
date copyright | 2009/08/01 | |
date issued | 2009 | |
identifier issn | 0022-4928 | |
identifier other | ams-68423.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4209980 | |
description abstract | This note presents an analysis of several dozens of direct numerical simulations of the cloud?clear air mixing in a setup of decaying moist turbulence with bin microphysics. The goal is to assess the instantaneous relationship between the homogeneity of mixing and the ratio of the time scales of droplet evaporation and turbulent homogenization. Such a relationship is important for developing improved microphysical parameterizations for large-eddy simulation of clouds. The analysis suggests a robust relationship for the range of time scale ratios between 0.5 and 10. Outside this range, the scatter of numerical data is significant, with smaller and larger time scale ratios corresponding to mixing scenarios that approach the extremely inhomogeneous and homogeneous limits, respectively. This is consistent with the heuristic argument relating the homogeneity of mixing to the time scale ratio. | |
publisher | American Meteorological Society | |
title | Numerical Simulation of Cloud–Clear Air Interfacial Mixing: Homogeneous versus Inhomogeneous Mixing | |
type | Journal Paper | |
journal volume | 66 | |
journal issue | 8 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/2009JAS2956.1 | |
journal fristpage | 2493 | |
journal lastpage | 2500 | |
tree | Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 008 | |
contenttype | Fulltext |