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Future climate forcing potentially without precedent in the last 420 million years
The evolution of Earth's climate on geological timescales is largely driven by variations in the magnitude of total solar irradiance (TSI) and changes in the greenhouse gas content of the atmosphere. Here we show that the slow ∼50 Wm(−2) increase in TSI over the last ∼420 million years (an incr...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5382278/ https://www.ncbi.nlm.nih.gov/pubmed/28375201 http://dx.doi.org/10.1038/ncomms14845 |