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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محفوظ في:
التفاصيل البيبلوغرافية
الحاوية / القاعدة:Global Biogeochem Cycles
المؤلفون الرئيسيون: Tian, Hanqin, Lu, Chaoqun, Yang, Jia, Banger, Kamaljit, Huntzinger, Deborah N., Schwalm, Christopher R., Michalak, Anna M., Cook, Robert, Ciais, Philippe, Hayes, Daniel, Huang, Maoyi, Ito, Akihiko, Jain, Atul K., Lei, Huimin, Mao, Jiafu, Pan, Shufen, Post, Wilfred M., Peng, Shushi, Poulter, Benjamin, Ren, Wei, Ricciuto, Daniel, Schaefer, Kevin, Shi, Xiaoying, Tao, Bo, Wang, Weile, Wei, Yaxing, Yang, Qichun, Zhang, Bowen, Zeng, Ning
التنسيق: Artigo
اللغة:Inglês
منشور في: John Wiley and Sons Inc. 2015
الموضوعات:
Research Articles
الوصول للمادة أونلاين: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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