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Recent improvements to the physical model of the Bohai Sea,the Yellow Sea and the East China Sea Operational Oceanography Forecasting System

Recent improvements to the physical model of the Bohai Sea,the Yellow Sea and the East China Sea Operational Oceanography Forecasting System

作     者:Ang Li Xueming Zhu Yunfei Zhang Shihe Ren Miaoyin Zhang Ziqing Zu Hui Wang Ang Li;Xueming Zhu;Yunfei Zhang;Shihe Ren;Miaoyin Zhang;Ziqing Zu;Hui Wang

作者机构:Key Laboratory of Marine Hazards ForecastingNational Marine Environmental Forecasting CenterMinistry of Natural ResourcesBeijing 100081China Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai)Zhuhai 519000China 

出 版 物:《Acta Oceanologica Sinica》 (海洋学报(英文版))

年 卷 期:2021年第40卷第11期

页      面:87-103页

核心收录:

学科分类:07[理学] 0707[理学-海洋科学] 

基  金:The National Key Research and Development Program of China under contract No.2017YFA0604203 the National Natural Science Foundation of China under contract Nos 42176029 and 41806003。 

主  题:Operational Oceanography Forecasting System East China Sea SST Yellow Sea Warm Current 

摘      要:In order to satisfy the increasing demand for the marine forecasting capacity,the Bohai Sea,the Yellow Sea and the East China Sea Operational Oceanography Forecasting System(BYEOFS)has been upgraded and improved to Version 2.0.Based on the Regional Ocean Modeling System(ROMS),a series of comparative experiments were conducted during the improvement process,including correcting topography,changing sea surface atmospheric forcing mode,adjusting open boundary conditions,and considering atmospheric pressure correction.(1)After the topography correction,the volume transport and meridional velocity maximum of Yellow Sea Warm Current increase obviously and the unreasonable bending of its axis around 36.1°N,123.5°E disappears.(2)After the change of sea surface forcing mode,an effective negative feedback mechanism is formed between predicted sea surface temperature(SST)by the ocean model and sea surface radiation fluxes fields.The simulation errors of SST decreased significantly,and the annual average of root-mean-square error(RMSE)decreased by about 18%.(3)The change of the eastern lateral boundary condition of baroclinic velocity from mixed Radiation-Nudging to Clamped makes the unreasonable westward current in Tsushima Strait disappear.(4)The adding of mean sea level pressure correction option which forms the mean sea level gradient from the Bohai Sea and the Yellow Sea to the western Pacific in winter and autumn is helpful to increasing the fluctuation of SLA and outflow of the Yellow Sea when the cold high air pressure system controls the Yellow Sea area.

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