Department of Meteorology, Stockholm University, Stockholm, Sweden
Thorsten Mauritsen
Department of Meteorology, Stockholm University, Stockholm, Sweden
Viewed
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: 5,676 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
3,912
308
1,456
5,676
107
163
HTML: 3,912
PDF: 308
XML: 1,456
Total: 5,676
BibTeX: 107
EndNote: 163
Views and downloads (calculated since 31 Jan 2024)
Cumulative views and downloads
(calculated since 31 Jan 2024)
Total article views: 3,233 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,648
308
277
3,233
107
163
HTML: 2,648
PDF: 308
XML: 277
Total: 3,233
BibTeX: 107
EndNote: 163
Views and downloads (calculated since 25 Sep 2024)
Cumulative views and downloads
(calculated since 25 Sep 2024)
Total article views: 2,443 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,264
0
1,179
2,443
0
0
HTML: 1,264
PDF: 0
XML: 1,179
Total: 2,443
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 31 Jan 2024)
Cumulative views and downloads
(calculated since 31 Jan 2024)
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: 5,676 (including HTML, PDF, and XML)
Thereof 5,580 with geography defined
and 96 with unknown origin.
Total article views: 3,233 (including HTML, PDF, and XML)
Thereof 3,142 with geography defined
and 91 with unknown origin.
Total article views: 2,443 (including HTML, PDF, and XML)
Thereof 2,438 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,...
