College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
Department of Atmospheric Science, University of Wyoming, Laramie,
Wyoming, USA
College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
Department of Atmospheric and Oceanic Science & ESSIC, University
of Maryland, College Park, Maryland, USA
College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
Fang Wu
College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
College of Global Change and Earth System Science, State Key
Laboratory of Earth Surface Processes and Resource Ecology, and Joint Center
for Global Change and Green China Development, Beijing Normal University,
Beijing, China
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4,195
1,535
146
5,876
720
160
255
HTML: 4,195
PDF: 1,535
XML: 146
Total: 5,876
Supplement: 720
BibTeX: 160
EndNote: 255
Views and downloads (calculated since 28 Sep 2016)
Cumulative views and downloads
(calculated since 28 Sep 2016)
Total article views: 4,872 (including HTML, PDF, and XML)
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EndNote
3,632
1,143
97
4,872
484
132
203
HTML: 3,632
PDF: 1,143
XML: 97
Total: 4,872
Supplement: 484
BibTeX: 132
EndNote: 203
Views and downloads (calculated since 01 Feb 2018)
Cumulative views and downloads
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Total article views: 1,004 (including HTML, PDF, and XML)
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563
392
49
1,004
236
28
52
HTML: 563
PDF: 392
XML: 49
Total: 1,004
Supplement: 236
BibTeX: 28
EndNote: 52
Views and downloads (calculated since 28 Sep 2016)
Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 5,876 (including HTML, PDF, and XML)
Thereof 5,809 with geography defined
and 67 with unknown origin.
Total article views: 4,872 (including HTML, PDF, and XML)
Thereof 4,828 with geography defined
and 44 with unknown origin.
Total article views: 1,004 (including HTML, PDF, and XML)
Thereof 981 with geography defined
and 23 with unknown origin.
We found that 22–28 % of the low AOD bias in eastern China simulated by the Community Atmosphere Model version 5 can be improved by using a new emission inventory. The concentrations of primary aerosols are closely related to the emission, while the seasonal variations of secondary aerosols depend more on atmospheric processes. This study highlights the importance of improving both the emission and atmospheric processes in modeling the atmospheric aerosols and their radiative effects.
We found that 22–28 % of the low AOD bias in eastern China simulated by the Community Atmosphere...