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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2016-07-01
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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 |
work_keys_str_mv |
AT akorolev theoreticalstudyofmixinginliquidcloudspart1classicalconcepts AT akhain theoreticalstudyofmixinginliquidcloudspart1classicalconcepts AT mpinsky theoreticalstudyofmixinginliquidcloudspart1classicalconcepts AT jfrench theoreticalstudyofmixinginliquidcloudspart1classicalconcepts |
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