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On transient climate change at the Cretaceous−Paleogene boundary due to atmospheric soot injections
Climate simulations that consider injection into the atmosphere of 15,000 Tg of soot, the amount estimated to be present at the Cretaceous−Paleogene boundary, produce what might have been one of the largest episodes of transient climate change in Earth history. The observed soot is believed to origi...
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| Publicado no: | Proc Natl Acad Sci U S A |
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| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5594694/ https://ncbi.nlm.nih.gov/pubmed/28827324 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1708980114 |
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