Department of Meteorology, Stockholm University, Stockholm, Sweden
Thorsten Mauritsen
Department of Meteorology, Stockholm University, Stockholm, Sweden
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Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 5,606 (including HTML, PDF, and XML)
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3,878
286
1,442
5,606
91
155
HTML: 3,878
PDF: 286
XML: 1,442
Total: 5,606
BibTeX: 91
EndNote: 155
Views and downloads (calculated since 31 Jan 2024)
Cumulative views and downloads
(calculated since 31 Jan 2024)
Total article views: 3,172 (including HTML, PDF, and XML)
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BibTeX
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2,623
286
263
3,172
91
155
HTML: 2,623
PDF: 286
XML: 263
Total: 3,172
BibTeX: 91
EndNote: 155
Views and downloads (calculated since 25 Sep 2024)
Cumulative views and downloads
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Total article views: 2,434 (including HTML, PDF, and XML)
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1,255
0
1,179
2,434
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PDF: 0
XML: 1,179
Total: 2,434
BibTeX: 0
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Views and downloads (calculated since 31 Jan 2024)
Cumulative views and downloads
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Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 5,606 (including HTML, PDF, and XML)
Thereof 5,510 with geography defined
and 96 with unknown origin.
Total article views: 3,172 (including HTML, PDF, and XML)
Thereof 3,081 with geography defined
and 91 with unknown origin.
Total article views: 2,434 (including HTML, PDF, and XML)
Thereof 2,429 with geography defined
and 5 with unknown origin.
Aerosol particles, from natural and human sources, have a cooling effect on the climate, partially offsetting global warming. They do this through direct (sunlight reflection) and indirect (cloud property alteration) mechanisms. Using a global climate model, we found that, despite declining emissions, the direct effect of human aerosols has increased while the indirect effect has decreased, which is attributed to the shift in emissions from North America and Europe to Southeast Asia.
Aerosol particles, from natural and human sources, have a cooling effect on the climate,...
