The relative dispersion of cloud droplets: its robustness with respect to key cloud properties

Flight data measured in warm convective clouds near Istanbul in June 2008 were used to investigate the relative dispersion of cloud droplet size distribution. The relative dispersion (ϵ), defined as the ratio between the standard deviation (σ) of the cloud droplet size distr...

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Main Authors: E. Tas, A. Teller, O. Altaratz, D. Axisa, R. Bruintjes, Z. Levin, I. Koren
Format: Article
Language:English
Published: Copernicus Publications 2015-02-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/2009/2015/acp-15-2009-2015.pdf
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spelling doaj-4fbba32c049a46768f084bd3d9e77fc32020-11-24T23:46:01ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-02-011542009201710.5194/acp-15-2009-2015The relative dispersion of cloud droplets: its robustness with respect to key cloud propertiesE. Tas0A. Teller1O. Altaratz2D. Axisa3R. Bruintjes4Z. Levin5I. Koren6Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot, IsraelDepartment of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot, IsraelDepartment of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot, IsraelResearch Applications Laboratory, National Center for Atmospheric Research, Boulder, CO, USAResearch Applications Laboratory, National Center for Atmospheric Research, Boulder, CO, USADepartment of Geophysics and Planetary Science, Tel Aviv University, IsraelDepartment of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot, IsraelFlight data measured in warm convective clouds near Istanbul in June 2008 were used to investigate the relative dispersion of cloud droplet size distribution. The relative dispersion (ϵ), defined as the ratio between the standard deviation (σ) of the cloud droplet size distribution and cloud droplet average radius (⟨r⟩), is a key factor in regional and global models. The relationship between ε and the clouds' microphysical and thermodynamic characteristics is examined. The results show that ε is constrained with average values in the range of ~0.25–0.35. ε is shown not to be correlated with cloud droplet concentration or liquid water content (LWC). However, ε variance is shown to be sensitive to droplet concentration and LWC, suggesting smaller variability of ϵ in the clouds' most adiabatic regions. A criterion for use of in situ airborne measurement data for calculations of statistical moments (used in bulk microphysical schemes), based on the evaluation of ϵ, is suggested.http://www.atmos-chem-phys.net/15/2009/2015/acp-15-2009-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Tas
A. Teller
O. Altaratz
D. Axisa
R. Bruintjes
Z. Levin
I. Koren
spellingShingle E. Tas
A. Teller
O. Altaratz
D. Axisa
R. Bruintjes
Z. Levin
I. Koren
The relative dispersion of cloud droplets: its robustness with respect to key cloud properties
Atmospheric Chemistry and Physics
author_facet E. Tas
A. Teller
O. Altaratz
D. Axisa
R. Bruintjes
Z. Levin
I. Koren
author_sort E. Tas
title The relative dispersion of cloud droplets: its robustness with respect to key cloud properties
title_short The relative dispersion of cloud droplets: its robustness with respect to key cloud properties
title_full The relative dispersion of cloud droplets: its robustness with respect to key cloud properties
title_fullStr The relative dispersion of cloud droplets: its robustness with respect to key cloud properties
title_full_unstemmed The relative dispersion of cloud droplets: its robustness with respect to key cloud properties
title_sort relative dispersion of cloud droplets: its robustness with respect to key cloud properties
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2015-02-01
description Flight data measured in warm convective clouds near Istanbul in June 2008 were used to investigate the relative dispersion of cloud droplet size distribution. The relative dispersion (ϵ), defined as the ratio between the standard deviation (σ) of the cloud droplet size distribution and cloud droplet average radius (⟨r⟩), is a key factor in regional and global models. The relationship between ε and the clouds' microphysical and thermodynamic characteristics is examined. The results show that ε is constrained with average values in the range of ~0.25–0.35. ε is shown not to be correlated with cloud droplet concentration or liquid water content (LWC). However, ε variance is shown to be sensitive to droplet concentration and LWC, suggesting smaller variability of ϵ in the clouds' most adiabatic regions. A criterion for use of in situ airborne measurement data for calculations of statistical moments (used in bulk microphysical schemes), based on the evaluation of ϵ, is suggested.
url http://www.atmos-chem-phys.net/15/2009/2015/acp-15-2009-2015.pdf
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