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>...
Main Authors: | , , , , |
---|---|
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 |
id |
doaj-9c7accdc9ce243529f4ef85fcb410210 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT ejung precipitationsusceptibilityinmarinestratocumulusandshallowcumulusfromairbornemeasurements AT ejung precipitationsusceptibilityinmarinestratocumulusandshallowcumulusfromairbornemeasurements AT baalbrecht precipitationsusceptibilityinmarinestratocumulusandshallowcumulusfromairbornemeasurements AT asorooshian precipitationsusceptibilityinmarinestratocumulusandshallowcumulusfromairbornemeasurements AT asorooshian precipitationsusceptibilityinmarinestratocumulusandshallowcumulusfromairbornemeasurements AT pzuidema precipitationsusceptibilityinmarinestratocumulusandshallowcumulusfromairbornemeasurements AT hhjonsson precipitationsusceptibilityinmarinestratocumulusandshallowcumulusfromairbornemeasurements |
_version_ |
1725473805466337280 |