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Analysis of polarimetric satellite measurements suggests stronger cooling due to aerosol-cloud interactions
Anthropogenic aerosol emissions lead to an increase in the amount of cloud condensation nuclei and consequently an increase in cloud droplet number concentration and cloud albedo. The corresponding negative radiative forcing due to aerosol cloud interactions (RF[Formula: see text] ) is one of the mo...
Gorde:
| Argitaratua izan da: | Nat Commun |
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| Egile Nagusiak: | , , |
| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Nature Publishing Group UK
2019
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| Gaiak: | |
| Sarrera elektronikoa: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6881401/ https://ncbi.nlm.nih.gov/pubmed/31776336 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-13372-2 |
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