Articles | Volume 15, issue 10
https://doi.org/10.5194/acp-15-5521-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-5521-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
AOD trends during 2001–2010 from observations and model simulations
Atmospheric Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
A. de Meij
Sustainable Development, NOVELTIS, rue du Lac, 31670 Labège, France
J. Yoon
Atmospheric Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
Institute for Physics of the Atmosphere, Johannes Gutenberg University Mainz, Germany
A. K. Georgoulias
Department of Meteorology and Climatology, School of Geology, Aristotle University of Thessaloniki, Greece
Multiphase Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
Energy, Environment and Water Research Center, The Cyprus Institute, Nicosia, Cyprus
M. Astitha
The Department of Civil and Environmental Engineering, University of Connecticut, Storrs, Connecticut, USA
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Short summary
Thanks to numerical simulations and satellite observations, it is shown that aerosol optical depth (AOD) trends (2000--2010 period) over the US and Europe are due to emission decrease, while over the Sahara Desert and the Middle East they are due to meteorological changes. Over Southeast Asia, both meteorology and emission changes are important for the AOD trends.
It is shown that soluble components strongly influence AOD, as their contribution is enhanced by the aerosol water content.
Thanks to numerical simulations and satellite observations, it is shown that aerosol optical...
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