Theoretical study of mixing in liquid clouds – Part 1: Classical concepts

The present study considers final stages of in-cloud mixing in the framework of classical concept of homogeneous and extreme inhomogeneous mixing. Simple analytical relationships between basic microphysical parameters were obtained for homogeneous and extreme inhomogeneous mixing based on the adi...

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Main Authors: A. Korolev, A. Khain, M. Pinsky, J. French
Format: Article
Language:English
Published: Copernicus Publications 2016-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/9235/2016/acp-16-9235-2016.pdf
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spelling doaj-c61bf8e9a4a84a88a10b5bdb6c495a882020-11-24T22:33:45ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-07-01169235925410.5194/acp-16-9235-2016Theoretical study of mixing in liquid clouds – Part 1: Classical conceptsA. Korolev0A. Khain1M. Pinsky2J. French3Environment and Climate Change Canada, Cloud Physics and Severe Weather Section, Toronto, CanadaDepartment of Atmospheric Sciences, the Hebrew University of Jerusalem, Jerusalem, IsraelDepartment of Atmospheric Sciences, the Hebrew University of Jerusalem, Jerusalem, IsraelUniversity of Wyoming, Laramie, WY, USAThe present study considers final stages of in-cloud mixing in the framework of classical concept of homogeneous and extreme inhomogeneous mixing. Simple analytical relationships between basic microphysical parameters were obtained for homogeneous and extreme inhomogeneous mixing based on the adiabatic consideration. It was demonstrated that during homogeneous mixing the functional relationships between the moments of the droplets size distribution hold only during the primary stage of mixing. Subsequent random mixing between already mixed parcels and undiluted cloud parcels breaks these relationships. However, during extreme inhomogeneous mixing the functional relationships between the microphysical parameters hold both for primary and subsequent mixing. The obtained relationships can be used to identify the type of mixing from in situ observations. The effectiveness of the developed method was demonstrated using in situ data collected in convective clouds. It was found that for the specific set of in situ measurements the interaction between cloudy and entrained environments was dominated by extreme inhomogeneous mixing.https://www.atmos-chem-phys.net/16/9235/2016/acp-16-9235-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Korolev
A. Khain
M. Pinsky
J. French
spellingShingle A. Korolev
A. Khain
M. Pinsky
J. French
Theoretical study of mixing in liquid clouds – Part 1: Classical concepts
Atmospheric Chemistry and Physics
author_facet A. Korolev
A. Khain
M. Pinsky
J. French
author_sort A. Korolev
title Theoretical study of mixing in liquid clouds – Part 1: Classical concepts
title_short Theoretical study of mixing in liquid clouds – Part 1: Classical concepts
title_full Theoretical study of mixing in liquid clouds – Part 1: Classical concepts
title_fullStr Theoretical study of mixing in liquid clouds – Part 1: Classical concepts
title_full_unstemmed Theoretical study of mixing in liquid clouds – Part 1: Classical concepts
title_sort theoretical study of mixing in liquid clouds – part 1: classical concepts
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2016-07-01
description The present study considers final stages of in-cloud mixing in the framework of classical concept of homogeneous and extreme inhomogeneous mixing. Simple analytical relationships between basic microphysical parameters were obtained for homogeneous and extreme inhomogeneous mixing based on the adiabatic consideration. It was demonstrated that during homogeneous mixing the functional relationships between the moments of the droplets size distribution hold only during the primary stage of mixing. Subsequent random mixing between already mixed parcels and undiluted cloud parcels breaks these relationships. However, during extreme inhomogeneous mixing the functional relationships between the microphysical parameters hold both for primary and subsequent mixing. The obtained relationships can be used to identify the type of mixing from in situ observations. The effectiveness of the developed method was demonstrated using in situ data collected in convective clouds. It was found that for the specific set of in situ measurements the interaction between cloudy and entrained environments was dominated by extreme inhomogeneous mixing.
url https://www.atmos-chem-phys.net/16/9235/2016/acp-16-9235-2016.pdf
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AT akhain theoreticalstudyofmixinginliquidcloudspart1classicalconcepts
AT mpinsky theoreticalstudyofmixinginliquidcloudspart1classicalconcepts
AT jfrench theoreticalstudyofmixinginliquidcloudspart1classicalconcepts
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