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Global patterns and controls of soil organic carbon dynamics as simulated by multiple terrestrial biosphere models: Current status and future directions
Soil is the largest organic carbon (C) pool of terrestrial ecosystems, and C loss from soil accounts for a large proportion of land‐atmosphere C exchange. Therefore, a small change in soil organic C (SOC) can affect atmospheric carbon dioxide (CO(2)) concentration and climate change. In the past dec...
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| Опубликовано в: : | Global Biogeochem Cycles |
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| Главные авторы: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
John Wiley and Sons Inc.
2015
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5008182/ https://ncbi.nlm.nih.gov/pubmed/27642229 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2014GB005021 |
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