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...

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Detalles Bibliográficos
Autores principales: Hasekamp, Otto P., Gryspeerdt, Edward, Quaas, Johannes
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6881401/
https://www.ncbi.nlm.nih.gov/pubmed/31776336
http://dx.doi.org/10.1038/s41467-019-13372-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6881401/
https://www.ncbi.nlm.nih.gov/pubmed/31776336
http://dx.doi.org/10.1038/s41467-019-13372-2

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