Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6

Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6
复制标题

DOI:
10.1007/s40641-020-00160-0
复制
发表时间:
2020-08
影响因子:
9.5
通讯作者:
R. Séférian;S. Berthet;A. Yool;J. Palmiéri;L. Bopp;A. Tagliabue;L. Kwiatkowski;O. Aumont;J. Christian;J. Dunne;M. Gehlen;T. Ilyina;J. John;Hongmei Li;M. Long;Jessica Y. Luo;H. Nakano;A. Romanou;J. Schwinger;C. Stock;Yeray Santana-Falcón;Y. Takano;J. Tjiputra;H. Tsujino;Michio Watanabe;Tongwen Wu;Fanghua Wu;A. Yamamoto
R. Séférian;S. Berthet;A. Yool;J. Palmiéri;L. Bopp;A. Tagliabue;L. Kwiatkowski;O. Aumont;J. Christian;J. Dunne;M. Gehlen;T. Ilyina;J. John;Hongmei Li;M. Long;Jessica Y. Luo;H. Nakano;A. Romanou;J. Schwinger;C. Stock;Yeray Santana-Falcón;Y. Takano;J. Tjiputra;H. Tsujino;Michio Watanabe;Tongwen Wu;Fanghua Wu;A. Yamamoto
中科院分区:
地球科学1区
文献类型:
--
作者:
R. Séférian;S. Berthet;A. Yool;J. Palmiéri;L. Bopp;A. Tagliabue;L. Kwiatkowski;O. Aumont;J. Christian;J. Dunne;M. Gehlen;T. Ilyina;J. John;Hongmei Li;M. Long;Jessica Y. Luo;H. Nakano;A. Romanou;J. Schwinger;C. Stock;Yeray Santana-Falcón;Y. Takano;J. Tjiputra;H. Tsujino;Michio Watanabe;Tongwen Wu;Fanghua Wu;A. Yamamoto

文献摘要

被引文献

相似文献

审查的目的海洋地球化学成分的变化或更新已被映射CMIP 5和CMIP 6模式版本之间,并作出评估,在多大程度上,这些已导致改进的模拟平均状态的海洋地球化学模型在当前一代的地球系统models(ESMs.Recent FindingsThe表示海洋地球化学已在当前一代的地球系统models的进展。然而,仍然很难确定哪些模型更新负责给定的改进。此外,在当前一代的地球系统模型中,海洋生物地球化学在地球系统相互作用和气候反馈方面的全部潜力仍然没有得到充分的研究。总结海洋生物地球化学数据的可用性不断增加,以及对潜在过程的更好理解,使得当前一代ESM的海洋生物地球化学成分取得了进展。本研究审查的程度,海洋生态地球化学成分的ESM之间的第5和第6阶段的耦合模式相互比较项目(CMIP)的进展。
Purpose of ReviewThe changes or updates in ocean biogeochemistry component have been mapped between CMIP5 and CMIP6 model versions, and an assessment made of how far these have led to improvements in the simulated mean state of marine biogeochemical models within the current generation of Earth system models (ESMs).Recent FindingsThe representation of marine biogeochemistry has progressed within the current generation of Earth system models. However, it remains difficult to identify which model updates are responsible for a given improvement. In addition, the full potential of marine biogeochemistry in terms of Earth system interactions and climate feedback remains poorly examined in the current generation of Earth system models.SummaryIncreasing availability of ocean biogeochemical data, as well as an improved understanding of the underlying processes, allows advances in the marine biogeochemical components of the current generation of ESMs. The present study scrutinizes the extent to which marine biogeochemistry components of ESMs have progressed between the 5th and the 6th phases of the Coupled Model Intercomparison Project (CMIP).