Department of Atmospheric and Oceanic Sciences & Shanghai Key Laboratory of Ocean-Land-Atmosphere Boundary Dynamics and Climate Change, Fudan University, Shanghai, 200438, China
Institute of Eco-Chongming (IEC), Shanghai, 202151, China
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Total article views: 3,687 (including HTML, PDF, and XML)
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2,987
559
141
3,687
112
111
167
HTML: 2,987
PDF: 559
XML: 141
Total: 3,687
Supplement: 112
BibTeX: 111
EndNote: 167
Views and downloads (calculated since 05 Mar 2025)
Cumulative views and downloads
(calculated since 05 Mar 2025)
Total article views: 1,216 (including HTML, PDF, and XML)
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EndNote
864
289
63
1,216
112
47
47
HTML: 864
PDF: 289
XML: 63
Total: 1,216
Supplement: 112
BibTeX: 47
EndNote: 47
Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
(calculated since 04 Nov 2025)
Total article views: 2,471 (including HTML, PDF, and XML)
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BibTeX
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2,123
270
78
2,471
64
120
HTML: 2,123
PDF: 270
XML: 78
Total: 2,471
BibTeX: 64
EndNote: 120
Views and downloads (calculated since 05 Mar 2025)
Cumulative views and downloads
(calculated since 05 Mar 2025)
Viewed (geographical distribution)
Total article views: 3,687 (including HTML, PDF, and XML)
Thereof 3,655 with geography defined
and 32 with unknown origin.
Total article views: 1,216 (including HTML, PDF, and XML)
Thereof 1,190 with geography defined
and 26 with unknown origin.
Total article views: 2,471 (including HTML, PDF, and XML)
Thereof 2,465 with geography defined
and 6 with unknown origin.
We note that the CESM2-WACCM and GFDL-ESM4 models would not simulate the tropospheric O3 forcing due to precursor gases from natural sources. Furthermore, the ozone simulated by them are also obviously less sensitive to natural precursors than to anthropogenic sources.
We note that the CESM2-WACCM and GFDL-ESM4 models would not simulate the tropospheric O3 forcing...