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Reduction in global area burned and wildfire emissions since 1930s enhances carbon uptake by land
The terrestrial biosphere currently absorbs about 30% of anthropogenic CO(2) emissions. This carbon uptake over land results primarily from vegetation’s response to increasing atmospheric CO(2) but other factors also play a role. Here we show that since the 1930s increasing population densities and...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5904128/ https://www.ncbi.nlm.nih.gov/pubmed/29666366 http://dx.doi.org/10.1038/s41467-018-03838-0 |