Radiative forcing by light-absorbing aerosols of pyrogenetic iron oxides

Iron (Fe) oxides in aerosols are known to absorb sun light and heat the atmosphere. However, the radiative forcing (RF) of light-absorbing aerosols of pyrogenetic Fe oxides is ignored in climate models. For the first time, we use a global chemical transport model and a radiative transfer model to es...

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Detalles Bibliográficos
Autores principales: Ito, Akinori, Lin, Guangxing, Penner, Joyce E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5943515/
https://www.ncbi.nlm.nih.gov/pubmed/29743649
http://dx.doi.org/10.1038/s41598-018-25756-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5943515/
https://www.ncbi.nlm.nih.gov/pubmed/29743649
http://dx.doi.org/10.1038/s41598-018-25756-3

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