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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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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2018
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5943515/ https://ncbi.nlm.nih.gov/pubmed/29743649 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-25756-3 |
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