Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements

Precipitation tends to decrease as aerosol concentration increases in warm marine boundary layer clouds at fixed liquid water path (LWP). The quantitative nature of this relationship is captured using the precipitation susceptibility (<i>S</i><sub><i>o</i></sub>...

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Main Authors: E. Jung, B. A. Albrecht, A. Sorooshian, P. Zuidema, H. H. Jonsson
Format: Article
Language:English
Published: Copernicus Publications 2016-09-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/11395/2016/acp-16-11395-2016.pdf
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spelling doaj-9c7accdc9ce243529f4ef85fcb4102102020-11-24T23:52:18ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-09-0116113951141310.5194/acp-16-11395-2016Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurementsE. Jung0E. Jung1B. A. Albrecht2A. Sorooshian3A. Sorooshian4P. Zuidema5H. H. Jonsson6Department of Atmospheric Sciences, University of Miami, Miami, FL, 33149, USAnow at: National Institute of Meteorological Sciences, Jeju, 63568, South KoreaDepartment of Atmospheric Sciences, University of Miami, Miami, FL, 33149, USADepartment of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ, 85721, USADepartment of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ, 85721, USADepartment of Atmospheric Sciences, University of Miami, Miami, FL, 33149, USANaval Postgraduate School, Monterey, CA, 93943, USAPrecipitation tends to decrease as aerosol concentration increases in warm marine boundary layer clouds at fixed liquid water path (LWP). The quantitative nature of this relationship is captured using the precipitation susceptibility (<i>S</i><sub><i>o</i></sub>) metric. Previously published works disagree on the qualitative behavior of <i>S</i><sub><i>o</i></sub> in marine low clouds: <i>S</i><sub><i>o</i></sub> decreases monotonically with increasing LWP or cloud depth (<i>H</i>) in stratocumulus clouds (Sc), while it increases and then decreases in shallow cumulus clouds (Cu). This study uses airborne measurements from four field campaigns on Cu and Sc with similar instrument packages and flight maneuvers to examine if and why <i>S</i><sub><i>o</i></sub> behavior varies as a function of cloud type. The findings show that <i>S</i><sub><i>o</i></sub> increases with <i>H</i> and then decreases in both Sc and Cu. Possible reasons for why these results differ from those in previous studies of Sc are discussed.https://www.atmos-chem-phys.net/16/11395/2016/acp-16-11395-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Jung
E. Jung
B. A. Albrecht
A. Sorooshian
A. Sorooshian
P. Zuidema
H. H. Jonsson
spellingShingle E. Jung
E. Jung
B. A. Albrecht
A. Sorooshian
A. Sorooshian
P. Zuidema
H. H. Jonsson
Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
Atmospheric Chemistry and Physics
author_facet E. Jung
E. Jung
B. A. Albrecht
A. Sorooshian
A. Sorooshian
P. Zuidema
H. H. Jonsson
author_sort E. Jung
title Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
title_short Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
title_full Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
title_fullStr Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
title_full_unstemmed Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
title_sort precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2016-09-01
description Precipitation tends to decrease as aerosol concentration increases in warm marine boundary layer clouds at fixed liquid water path (LWP). The quantitative nature of this relationship is captured using the precipitation susceptibility (<i>S</i><sub><i>o</i></sub>) metric. Previously published works disagree on the qualitative behavior of <i>S</i><sub><i>o</i></sub> in marine low clouds: <i>S</i><sub><i>o</i></sub> decreases monotonically with increasing LWP or cloud depth (<i>H</i>) in stratocumulus clouds (Sc), while it increases and then decreases in shallow cumulus clouds (Cu). This study uses airborne measurements from four field campaigns on Cu and Sc with similar instrument packages and flight maneuvers to examine if and why <i>S</i><sub><i>o</i></sub> behavior varies as a function of cloud type. The findings show that <i>S</i><sub><i>o</i></sub> increases with <i>H</i> and then decreases in both Sc and Cu. Possible reasons for why these results differ from those in previous studies of Sc are discussed.
url https://www.atmos-chem-phys.net/16/11395/2016/acp-16-11395-2016.pdf
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