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Earth’s radiative imbalance from the Last Glacial Maximum to the present
The energy imbalance at the top of the atmosphere determines the temporal evolution of the global climate, and vice versa changes in the climate system can alter the planetary energy fluxes. This interplay is fundamental to our understanding of Earth’s heat budget and the climate system. However, ev...
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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
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6660766/ https://ncbi.nlm.nih.gov/pubmed/31285336 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1905447116 |
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