Department of Meteorology, Stockholm University, Stockholm, Sweden
Thorsten Mauritsen
Department of Meteorology, Stockholm University, Stockholm, Sweden
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Total article views: 6,214 (including HTML, PDF, and XML)
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4,136
464
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6,214
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HTML: 4,136
PDF: 464
XML: 1,614
Total: 6,214
BibTeX: 324
EndNote: 315
Views and downloads (calculated since 31 Jan 2024)
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Total article views: 3,711 (including HTML, PDF, and XML)
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2,813
464
434
3,711
324
315
HTML: 2,813
PDF: 464
XML: 434
Total: 3,711
BibTeX: 324
EndNote: 315
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Cumulative views and downloads
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Total article views: 2,503 (including HTML, PDF, and XML)
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1,323
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1,180
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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: 6,214 (including HTML, PDF, and XML)
Thereof 6,118 with geography defined
and 96 with unknown origin.
Total article views: 3,711 (including HTML, PDF, and XML)
Thereof 3,620 with geography defined
and 91 with unknown origin.
Total article views: 2,503 (including HTML, PDF, and XML)
Thereof 2,498 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,...
