Abstract
The datasets of two Ocean Model Intercomparison Project (OMIP) simulation experiments from the LASG/IAP Climate Ocean Model, version 3 (LICOM3), forced by two different sets of atmospheric surface data, are described in this paper. The experiment forced by CORE-II (Co-ordinated Ocean–Ice Reference Experiments, Phase II) data (1948–2009) is called OMIP1, and that forced by JRA55-do (surface dataset for driving ocean–sea-ice models based on Japanese 55-year atmospheric reanalysis) data (1958–2018) is called OMIP2. First, the improvement of LICOM from CMIP5 to CMIP6 and the configurations of the two experiments are described. Second, the basic performances of the two experiments are validated using the climatological-mean and interannual time scales from observation. We find that the mean states, interannual variabilities, and long-term linear trends can be reproduced well by the two experiments. The differences between the two datasets are also discussed. Finally, the usage of these data is described. These datasets are helpful toward understanding the origin system bias of the fully coupled model.
摘要
本文描述了中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室 (LASG/IAP) 气候系统海洋模式第三版 (LICOM3) 参与海洋模式比较计划 (OMIP) 的两个模拟试验数据集. 两个模拟试验采用不同大气表面强迫数据, 采用规范的海洋-海冰参考试验第二阶段 (Co-ordinated Ocean–Ice Reference Experiments, Phase II, CORE-II) 作为外强迫的试验称为 OMIP 第一阶段数据集 (OMIP1,1948-2009), 采用来自日本 55 年大气再分析表面数据驱动海洋-海冰模式 (JRA55-do) 强迫试验称为 OMIP 第二阶段数据集 (OMIP2, 1958-2018). 首先, 文章描述了 LICOM 从 CMIP5 到 CMIP6 的改进和试验基本设置. 其次, 利用来自观测气侯态和年际变化数据, 对两个试验的模拟性能进行检验. 结果表明模式的两个试验均很好再现了平均态、 年际变化和长期线性趋势. 同时, 讨论了两个模拟试验数据间的差异. 最后, 介绍了数据集的使用情况. 这两个数据集的提供有助于了解全耦合模式的系统偏差来源.
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Data availability statement
The data that support the findings of this study are available from https://esgf-nodes.llnl.gov/projects/cmip6/. The citation for OMIP1 is “CAS FGOALS-f3-L model output prepared for CMIP6 OMIP omip1. Earth System Grid Federation. https://doi.org/10.22033/ESGF/CMIP6.3413”. The citation for OMIP2 is “CAS FGOALS-f3-L model output prepared for CMIP6 OMIP omip2. Earth System Grid Federation. https://doi.org/10.22033/ESGF/CMIP6.3419”.
Change history
15 May 2020
In the original version of this article, the second author’s first name was misspelled as Zhipeng. The correct spelling is Zipeng. The sixth author’s first name was misspelled as Jirong. The correct spelling is Jinrong. The correct version is as follows:
LICOM Model Datasets for the CMIP6 Ocean Model Intercomparison Project
Pengfei LIN1,4, Zipeng YU1,4, Hailong LIU1,4, Yongqiang YU1,4, Yiwen LI1,4, Jinrong JIANG2, Wei XUE3, Kangjun CHEN1, Qian YANG1,4, Bowen ZHAO1,4, Jilin WEI1,4, Mengrong DING1,4, Zhikuo SUN1,4, Yaqi WANG1,4, Yao MENG1,4, Weipeng ZHENG1,4, and Jinfeng MA1
1 LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
2 Computer Network Information Center, Chinese Academy of Sciences, Beijing 100190, China
3 Department of Computer Science and Technology, Tsinghua University, Beijing 100084, China
4 College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
In the section “Data availability statement” on page 248 of the original version of this article, the URL of the data should be https://esgf-node.llnl.gov/projects/cmip6.
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Acknowledgements
This study was supported by the National Key R&D Program for Developing Basic Sciences (Grant Nos. 2016YFC1401401 and 2016YFC1401601), the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDC01000000), and the National Natural Science Foundation of China (Grants Nos. 41576026, 41576025, 41776030, 41931183 and 41976026).
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Article Highlights
• The OMIP1 and OMIP2 simulation datasets produced by LICOM3 are described.
• The mean states, interannual variabilities, and long-term linear trends can be reproduced well by the two experiments.
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Lin, P., Yu, Z., Liu, H. et al. LICOM Model Datasets for the CMIP6 Ocean Model Intercomparison Project. Adv. Atmos. Sci. 37, 239–249 (2020). https://doi.org/10.1007/s00376-019-9208-5
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DOI: https://doi.org/10.1007/s00376-019-9208-5