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: 5,514 (including HTML, PDF, and XML)
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3,817
272
1,425
5,514
78
144
HTML: 3,817
PDF: 272
XML: 1,425
Total: 5,514
BibTeX: 78
EndNote: 144
Views and downloads (calculated since 31 Jan 2024)
Cumulative views and downloads
(calculated since 31 Jan 2024)
Total article views: 3,087 (including HTML, PDF, and XML)
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XML
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BibTeX
EndNote
2,569
272
246
3,087
78
144
HTML: 2,569
PDF: 272
XML: 246
Total: 3,087
BibTeX: 78
EndNote: 144
Views and downloads (calculated since 25 Sep 2024)
Cumulative views and downloads
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Total article views: 2,427 (including HTML, PDF, and XML)
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1,248
0
1,179
2,427
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HTML: 1,248
PDF: 0
XML: 1,179
Total: 2,427
BibTeX: 0
EndNote: 0
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: 5,514 (including HTML, PDF, and XML)
Thereof 5,438 with geography defined
and 76 with unknown origin.
Total article views: 3,087 (including HTML, PDF, and XML)
Thereof 3,014 with geography defined
and 73 with unknown origin.
Total article views: 2,427 (including HTML, PDF, and XML)
Thereof 2,424 with geography defined
and 3 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,...
