Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixing

An idealized diffusion–evaporation model of time-dependent mixing between a cloud volume and a droplet-free volume is analyzed. The initial droplet size distribution (DSD) in the cloud volume is assumed to be monodisperse. It is shown that evolution of the microphysical variables and the final eq...

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Main Authors: M. Pinsky, A. Khain, A. Korolev
Format: Article
Language:English
Published: Copernicus Publications 2016-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/9273/2016/acp-16-9273-2016.pdf
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spelling doaj-55af3164a16d43318fadd55f208fbf6f2020-11-24T22:32:24ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-07-01169273929710.5194/acp-16-9273-2016Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixingM. Pinsky0A. Khain1A. Korolev2Department of Atmospheric Sciences, The Hebrew University of Jerusalem, Jerusalem, IsraelDepartment of Atmospheric Sciences, The Hebrew University of Jerusalem, Jerusalem, IsraelEnvironment Canada, Cloud Physics and Severe Weather Section, Toronto, CanadaAn idealized diffusion–evaporation model of time-dependent mixing between a cloud volume and a droplet-free volume is analyzed. The initial droplet size distribution (DSD) in the cloud volume is assumed to be monodisperse. It is shown that evolution of the microphysical variables and the final equilibrium state are unambiguously determined by two non-dimensional parameters. The first one is the potential evaporation parameter <i>R</i>, proportional to the ratio of the saturation deficit to the liquid water content in the cloud volume, that determines whether the equilibrium state is reached at 100 % relative humidity, or is characterized by a complete evaporation of cloud droplets. The second parameter <i>Da</i> is the Damkölher number equal to the ratio of the characteristic mixing time to the phase relaxation time. Parameters <i>R</i> and <i>Da</i> determine the type of mixing.<br><br>The results are analyzed within a wide range of values of <i>R</i> and <i>Da</i>. It is shown that there is no pure homogeneous mixing, since the first mixing stage is always inhomogeneous. The mixing type can change during the mixing process. Any mixing type leads to formation of a tail of small droplets in DSD and, therefore, to DSD broadening that depends on <i>Da</i>. At large <i>Da</i>, the final DSD dispersion can be as large as 0.2. The total duration of mixing varies from several to 100 phase relaxation time periods, depending on <i>R</i> and <i>Da</i>.<br><br>The definitions of homogeneous and inhomogeneous types of mixing are reconsidered and clarified, enabling a more precise delimitation between them. The paper also compares the results obtained with those based on the classic mixing concepts. >https://www.atmos-chem-phys.net/16/9273/2016/acp-16-9273-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Pinsky
A. Khain
A. Korolev
spellingShingle M. Pinsky
A. Khain
A. Korolev
Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixing
Atmospheric Chemistry and Physics
author_facet M. Pinsky
A. Khain
A. Korolev
author_sort M. Pinsky
title Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixing
title_short Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixing
title_full Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixing
title_fullStr Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixing
title_full_unstemmed Theoretical analysis of mixing in liquid clouds – Part 3: Inhomogeneous mixing
title_sort theoretical analysis of mixing in liquid clouds – part 3: inhomogeneous mixing
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2016-07-01
description An idealized diffusion–evaporation model of time-dependent mixing between a cloud volume and a droplet-free volume is analyzed. The initial droplet size distribution (DSD) in the cloud volume is assumed to be monodisperse. It is shown that evolution of the microphysical variables and the final equilibrium state are unambiguously determined by two non-dimensional parameters. The first one is the potential evaporation parameter <i>R</i>, proportional to the ratio of the saturation deficit to the liquid water content in the cloud volume, that determines whether the equilibrium state is reached at 100 % relative humidity, or is characterized by a complete evaporation of cloud droplets. The second parameter <i>Da</i> is the Damkölher number equal to the ratio of the characteristic mixing time to the phase relaxation time. Parameters <i>R</i> and <i>Da</i> determine the type of mixing.<br><br>The results are analyzed within a wide range of values of <i>R</i> and <i>Da</i>. It is shown that there is no pure homogeneous mixing, since the first mixing stage is always inhomogeneous. The mixing type can change during the mixing process. Any mixing type leads to formation of a tail of small droplets in DSD and, therefore, to DSD broadening that depends on <i>Da</i>. At large <i>Da</i>, the final DSD dispersion can be as large as 0.2. The total duration of mixing varies from several to 100 phase relaxation time periods, depending on <i>R</i> and <i>Da</i>.<br><br>The definitions of homogeneous and inhomogeneous types of mixing are reconsidered and clarified, enabling a more precise delimitation between them. The paper also compares the results obtained with those based on the classic mixing concepts. >
url https://www.atmos-chem-phys.net/16/9273/2016/acp-16-9273-2016.pdf
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