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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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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