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

作　　者：Qi Shu Zhenya Song Ying Bao Xiaodan Yang Yajuan Song Xinfang Li Meng Wei Fangli Qiao 

机构地区：[1]First Institute of Oceanography,and Key Laboratory of Marine Science and Numerical Modeling,Ministry of Natural Resources,Qingdao,266061,China [2]Laboratory for Regional Oceanography and Numerical Modeling,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao,266237,China [3]Shandong Key Laboratory of Marine Science and Numerical Modeling,Qingdao,266061,China

出　　处：《Acta Oceanologica Sinica》2022年第10期22-31,共10页海洋学报（英文版）

基　　金：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(Shu Xingbei Young Talent Program)under contract No.2019S06。

摘　　要：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.

关 键 词：FIO-ESM OMIP CMIP6 OGCM 

分 类 号：P714[天文地球—海洋科学]