Department of Meteorology, Stockholm University, Stockholm, Sweden
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Linnea Huusko
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: 803 (including HTML, PDF, and XML)
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Total article views: 525 (including HTML, PDF, and XML)
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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: 803 (including HTML, PDF, and XML)
Thereof 813 with geography defined
and -10 with unknown origin.
Total article views: 525 (including HTML, PDF, and XML)
Thereof 535 with geography defined
and -10 with unknown origin.
Total article views: 278 (including HTML, PDF, and XML)
Thereof 278 with geography defined
and 0 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,...