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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. 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. 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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  • In this study, 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. Evaluation of model drift, temperature, salinity, mixed layer depth, and the Atlantic Meridional Overturning Circulation shows 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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      沈阳化工大学材料科学与工程学院 沈阳 110142

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