Volume 41 Issue 10
Oct.  2022
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Qi Shu, Zhenya Song, Ying Bao, Xiaodan Yang, Yajuan Song, Xinfang Li, Meng Wei, Fangli Qiao. FIO-ESM v2.0 CORE2-forced experiment for the CMIP6 Ocean Model Intercomparison Project[J]. Acta Oceanologica Sinica, 2022, 41(10): 22-31. doi: 10.1007/s13131-022-2000-x
Citation: Qi Shu, Zhenya Song, Ying Bao, Xiaodan Yang, Yajuan Song, Xinfang Li, Meng Wei, Fangli Qiao. FIO-ESM v2.0 CORE2-forced experiment for the CMIP6 Ocean Model Intercomparison Project[J]. Acta Oceanologica Sinica, 2022, 41(10): 22-31. doi: 10.1007/s13131-022-2000-x

FIO-ESM v2.0 CORE2-forced experiment for the CMIP6 Ocean Model Intercomparison Project

doi: 10.1007/s13131-022-2000-x
Funds:  The National Key R&D Program of China under contract Nos 2018YFA0605701 and 2016YFB0201100; the National Natural Science Foundation of China under contract Nos 41941012 and 41821004; the Basic Scientific Fund for National Public Research Institute of China (ShuXingbei Young Talent Program) under contract No. 2019S06.
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  • Corresponding author: E-mail: qiaofl@fio.org.cn
  • Received Date: 2021-09-16
  • Accepted Date: 2021-11-29
  • Available Online: 2022-05-11
  • Publish Date: 2022-10-27
  • We introduced the Coupled Model Intercomparison Project Phase 6 (CMIP6) Ocean Model Intercomparison Project CORE2-forced (OMIP-1) experiment by using the First Institute of Oceanography Earth System Model version 2.0 (FIO-ESM v2.0), and comprehensively evaluated the simulation results. Unlike other OMIP models, FIO-ESM v2.0 includes a coupled ocean surface wave component model that takes into account non-breaking surface wave-induced vertical mixing in the ocean and effect of surface wave Stokes drift on air-sea momentum and heat fluxes in the climate system. A sub-layer sea surface temperature (SST) diurnal cycle parameterization was also employed to take into account effect of SST diurnal cycle on air-sea heat fluxes to improve simulations of air-sea interactions. Evaluations show that mean values and long-term trends of significant wave height were adequately reproduced in the FIO-ESM v2.0 OMIP-1 simulations, and there is a reasonable fit between the SST diurnal cycle obtained from in situ observations and that parameterized by FIO-ESM v2.0. Evaluations of model drift, temperature, salinity, mixed layer depth, and the Atlantic Meridional Overturning Circulation show that the model performs well in the FIO-ESM v2.0 OMIP-1 simulation. However, the summer sea ice extent of the Arctic and Antarctic is underestimated.
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