基于HYCOM设计了3组数值试验,分别采用KPP(K-Profile Parameterization),KT(Kraus and Turner),MY(Mellor and Yamada)2.5三种垂向混合方案,比较分析了这3种混合方案对全球大洋的模拟能力。结果表明:KPP方案和MY2.5方案模拟的温度场十...基于HYCOM设计了3组数值试验,分别采用KPP(K-Profile Parameterization),KT(Kraus and Turner),MY(Mellor and Yamada)2.5三种垂向混合方案,比较分析了这3种混合方案对全球大洋的模拟能力。结果表明:KPP方案和MY2.5方案模拟的温度场十分类似,在中高纬度几乎一致,在赤道断面上MY2.5方案的最大误差小于KPP方案,对于暖池区SST的模拟MY2.5方案的误差也稍小于KPP方案,但二者的差别并不明显。在模拟赤道潜流时,MY2.5方案暴露出明显不足,其模拟效果要明显差于KPP方案和KT方案。KT方案模拟效果的好坏依赖于混合层底的确定是否准确,其在中高纬度海域的模拟效果要明显优于热带海域。总之,在热带海域,KPP方案的模拟整体效果最好,在中高纬度海域,KPP方案和MY2.5方案差别不大,而KT方案则更适用于中高纬度。展开更多
基于HYCOM(Hybrid Coordinate Oceanic Circulation Model),以OFES(OGCM for the Earth Simulator)资料为参考,分析了KPP、MY2.5、KT三种不同混合方案对北太平洋西边界流系的模拟结果的影响。结果表明:三种不同混合方案模拟的上层海洋...基于HYCOM(Hybrid Coordinate Oceanic Circulation Model),以OFES(OGCM for the Earth Simulator)资料为参考,分析了KPP、MY2.5、KT三种不同混合方案对北太平洋西边界流系的模拟结果的影响。结果表明:三种不同混合方案模拟的上层海洋平均流场与OFES资料相似,但在流向和流幅上略有差异,其中KPP方案模拟的流速与OFES资料最为接近,MY2.5方案次之,KT方案与其差别最大。通过代表性断面上流速的对比分析,对模式就北赤道流、棉兰老流、棉兰老潜流、黑潮的模拟效果进行比较,KPP方案模拟的效果同前人的观测和研究最为接近。分析了北赤道流,棉兰老流,棉兰老潜流,黑潮的流量的季节变化特征,其中KPP方案与OFES资料计算的棉兰老流和棉兰老潜流的季节变化特征与前人描述比较一致,表现为春强秋弱。KPP方案和OFES资料的计算结果表明,北赤道流和棉兰老流大致上是同向变化的,而在冬季棉兰老流同黑潮的变化基本上是一致的。展开更多
The origin of the Ryukyu Current(RC)and the formation of its subsurface velocity core were investigated using a 23-year(1993–2015)global Hybrid Coordinate Ocean Model(HYCOM)dataset.The volume transport of the RC come...The origin of the Ryukyu Current(RC)and the formation of its subsurface velocity core were investigated using a 23-year(1993–2015)global Hybrid Coordinate Ocean Model(HYCOM)dataset.The volume transport of the RC comes from the Kuroshio eastward branch(KEB)east of Taiwan and part of the North Pacific Subtropical Gyre(p-NPSG).From the surface to 2000m depth,the KEB(p-NPSG)transport contributes 41.5%(58.5%)to the mean total RC transport.The KEB originally forms the subsurface velocity core of the RC east of Taiwan due to blockage of the subsurface Kuroshio by the Ilan Ridge(sill depth:700 m).Above 700m,the Kuroshio can enter the East China Sea(ECS)over the Ilan Ridge,meanwhile,the blocked Kuroshio below 700m turns to the right and flows along the Ryukyu Islands.With the RC flowing northeastward,the p-NPSG contribution strengthens the subsurface maximum structure of the RC owing to the blockage of the Ryukyu Ridge.In the surface layer,the p-NPSG cannot form a stable northeastward current due to frequent disturbance by mesoscale eddies and water exchange through the gaps(with net volume transport into ECS)between the Ryukyu Islands.展开更多
文摘基于HYCOM设计了3组数值试验,分别采用KPP(K-Profile Parameterization),KT(Kraus and Turner),MY(Mellor and Yamada)2.5三种垂向混合方案,比较分析了这3种混合方案对全球大洋的模拟能力。结果表明:KPP方案和MY2.5方案模拟的温度场十分类似,在中高纬度几乎一致,在赤道断面上MY2.5方案的最大误差小于KPP方案,对于暖池区SST的模拟MY2.5方案的误差也稍小于KPP方案,但二者的差别并不明显。在模拟赤道潜流时,MY2.5方案暴露出明显不足,其模拟效果要明显差于KPP方案和KT方案。KT方案模拟效果的好坏依赖于混合层底的确定是否准确,其在中高纬度海域的模拟效果要明显优于热带海域。总之,在热带海域,KPP方案的模拟整体效果最好,在中高纬度海域,KPP方案和MY2.5方案差别不大,而KT方案则更适用于中高纬度。
文摘基于HYCOM(Hybrid Coordinate Oceanic Circulation Model),以OFES(OGCM for the Earth Simulator)资料为参考,分析了KPP、MY2.5、KT三种不同混合方案对北太平洋西边界流系的模拟结果的影响。结果表明:三种不同混合方案模拟的上层海洋平均流场与OFES资料相似,但在流向和流幅上略有差异,其中KPP方案模拟的流速与OFES资料最为接近,MY2.5方案次之,KT方案与其差别最大。通过代表性断面上流速的对比分析,对模式就北赤道流、棉兰老流、棉兰老潜流、黑潮的模拟效果进行比较,KPP方案模拟的效果同前人的观测和研究最为接近。分析了北赤道流,棉兰老流,棉兰老潜流,黑潮的流量的季节变化特征,其中KPP方案与OFES资料计算的棉兰老流和棉兰老潜流的季节变化特征与前人描述比较一致,表现为春强秋弱。KPP方案和OFES资料的计算结果表明,北赤道流和棉兰老流大致上是同向变化的,而在冬季棉兰老流同黑潮的变化基本上是一致的。
基金The National Natural Science Foundation of China under contract Nos 41576001,41920104006,41776107,41906023,41621064,41476020 and 41606113the Scientific Research Fund of SIO under contract Nos JG1626,JG1621 and JT1604+2 种基金the Project of State Key Laboratory of Satellite Ocean Environment Dynamics,SIO under contract Nos SOEDZZ1901,SOEDZZ1804 and SOEDZZ1806the National Programme on Global Change and Air-sea Interaction under contract No.GASI-IPOVAI-01-02the Zhejiang Provincial Natural Science Foundation of China under contract No.LQ17D060003
文摘The origin of the Ryukyu Current(RC)and the formation of its subsurface velocity core were investigated using a 23-year(1993–2015)global Hybrid Coordinate Ocean Model(HYCOM)dataset.The volume transport of the RC comes from the Kuroshio eastward branch(KEB)east of Taiwan and part of the North Pacific Subtropical Gyre(p-NPSG).From the surface to 2000m depth,the KEB(p-NPSG)transport contributes 41.5%(58.5%)to the mean total RC transport.The KEB originally forms the subsurface velocity core of the RC east of Taiwan due to blockage of the subsurface Kuroshio by the Ilan Ridge(sill depth:700 m).Above 700m,the Kuroshio can enter the East China Sea(ECS)over the Ilan Ridge,meanwhile,the blocked Kuroshio below 700m turns to the right and flows along the Ryukyu Islands.With the RC flowing northeastward,the p-NPSG contribution strengthens the subsurface maximum structure of the RC owing to the blockage of the Ryukyu Ridge.In the surface layer,the p-NPSG cannot form a stable northeastward current due to frequent disturbance by mesoscale eddies and water exchange through the gaps(with net volume transport into ECS)between the Ryukyu Islands.
