Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms
<p>Aerosol and cloud properties over southern China during the 10-year period 2006–2015 are analysed based on observations from passive and active satellite sensors and emission data. The results show a strong decrease in aerosol optical depth (AOD) over the study area, accompanied by an incre...
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doaj-ead8c7e9f3aa4da8bcdadfb705ec26462020-11-25T01:46:43ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242020-01-012045747410.5194/acp-20-457-2020Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanismsN. Benas0J. F. Meirink1K.-G. Karlsson2M. Stengel3P. Stammes4R&D Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), De Bilt, the NetherlandsR&D Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), De Bilt, the NetherlandsSwedish Meteorological and Hydrological Institute (SMHI), Norrköping, SwedenDeutscher Wetterdienst (DWD), Offenbach, GermanyR&D Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), De Bilt, the Netherlands<p>Aerosol and cloud properties over southern China during the 10-year period 2006–2015 are analysed based on observations from passive and active satellite sensors and emission data. The results show a strong decrease in aerosol optical depth (AOD) over the study area, accompanied by an increase in liquid cloud cover and cloud liquid water path (LWP). The most significant changes occurred mainly in late autumn and early winter: AOD decreased by about 35 %, coinciding with an increase in liquid cloud fraction by 40 % and a near doubling of LWP in November and December. Analysis of emissions suggests that decreases in carbonaceous aerosol emissions from biomass burning activities were responsible for part of the AOD decrease, while inventories of other, anthropogenic emissions mainly showed increases. Analysis of precipitation changes suggests that an increase in precipitation also contributed to the overall aerosol reduction. Possible explanatory mechanisms for these changes were examined, including changes in circulation patterns and aerosol–cloud interactions (ACIs). Further analysis of changes in aerosol vertical profiles demonstrates a consistency of the observed aerosol and cloud changes with the aerosol semi-direct effect, which depends on relative heights of the aerosol and cloud layers: fewer absorbing aerosols in the cloud layer would lead to an overall decrease in the evaporation of cloud droplets, thus increasing cloud LWP and cover. While this mechanism cannot be proven based on the present observation-based analysis, these are indeed the signs of the reported changes.</p>https://www.atmos-chem-phys.net/20/457/2020/acp-20-457-2020.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
N. Benas J. F. Meirink K.-G. Karlsson M. Stengel P. Stammes |
spellingShingle |
N. Benas J. F. Meirink K.-G. Karlsson M. Stengel P. Stammes Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms Atmospheric Chemistry and Physics |
author_facet |
N. Benas J. F. Meirink K.-G. Karlsson M. Stengel P. Stammes |
author_sort |
N. Benas |
title |
Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms |
title_short |
Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms |
title_full |
Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms |
title_fullStr |
Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms |
title_full_unstemmed |
Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms |
title_sort |
satellite observations of aerosols and clouds over southern china from 2006 to 2015: analysis of changes and possible interaction mechanisms |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2020-01-01 |
description |
<p>Aerosol and cloud properties over southern China during
the 10-year period 2006–2015 are analysed based on observations from passive
and active satellite sensors and emission data. The results show a strong
decrease in aerosol optical depth (AOD) over the study area, accompanied by
an increase in liquid cloud cover and cloud liquid water path (LWP). The
most significant changes occurred mainly in late autumn and early winter: AOD decreased by about 35 %, coinciding with an increase in liquid
cloud fraction by 40 % and a near doubling of LWP in November and
December. Analysis of emissions suggests that decreases in carbonaceous
aerosol emissions from biomass burning activities were responsible for part
of the AOD decrease, while inventories of other, anthropogenic emissions
mainly showed increases. Analysis of precipitation changes suggests that an
increase in precipitation also contributed to the overall aerosol reduction.
Possible explanatory mechanisms for these changes were examined, including
changes in circulation patterns and aerosol–cloud interactions (ACIs). Further
analysis of changes in aerosol vertical profiles demonstrates a consistency
of the observed aerosol and cloud changes with the aerosol semi-direct
effect, which depends on relative heights of the aerosol and cloud layers: fewer absorbing aerosols in
the cloud layer would lead to an overall decrease in the evaporation of cloud
droplets, thus increasing cloud LWP and cover. While this mechanism cannot
be proven based on the present observation-based analysis, these are indeed
the signs of the reported changes.</p> |
url |
https://www.atmos-chem-phys.net/20/457/2020/acp-20-457-2020.pdf |
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