IOCAS-IR  > 海洋环流与波动重点实验室
Interbasin freshwater, heat and salt transport through the boundaries of the East and South China Seas from a variable-grid global ocean circulation model
Fang, GH; Wei, ZX; Choi, BH; Wang, H; Fang, Y; Li, W
2003-02-01
发表期刊SCIENCE IN CHINA SERIES D-EARTH SCIENCES
ISSN1006-9313
卷号46期号:2页码:149-161
文章类型Article
摘要The monthly and annual mean freshwater, heat and salt transport through the open boundaries of the South and East China Seas derived from a variable-grid global ocean circulation model is reported. The model has 1/6degrees resolution for the seas adjacent to China and 30 resolution for the global ocean. The model results are in fairly good agreement with the existing estimates based on measurements. The computation shows that the flows passing through the South China Sea contribute volume, heat and salt transport of 5.3 Sv, 0.57 PW and 184 Ggs(-1), respectively (about 1/4) to the Indonesian Throughflow, indicating that the South China Sea is an important pathway of the Pacific to Indian Ocean throughflow. The volume, heat and salt transport of the Kuroshio in the East China Sea is 25.6 Sv, 2.32 PW and 894 Ggs(-1), respectively. Less than 1/4 of this transport passes through the passage between Iriomote and Okinawa. The calculation of heat balance indicates that the South China Sea absorbs net heat flux from the sun and atmosphere with a rate of 0.08 PW, while the atmosphere gains net heat flux from the Baohai, Yellow and East China Seas with a rate of 0.05 PW.; The monthly and annual mean freshwater, heat and salt transport through the open boundaries of the South and East China Seas derived from a variable-grid global ocean circulation model is reported. The model has 1/6degrees resolution for the seas adjacent to China and 30 resolution for the global ocean. The model results are in fairly good agreement with the existing estimates based on measurements. The computation shows that the flows passing through the South China Sea contribute volume, heat and salt transport of 5.3 Sv, 0.57 PW and 184 Ggs(-1), respectively (about 1/4) to the Indonesian Throughflow, indicating that the South China Sea is an important pathway of the Pacific to Indian Ocean throughflow. The volume, heat and salt transport of the Kuroshio in the East China Sea is 25.6 Sv, 2.32 PW and 894 Ggs(-1), respectively. Less than 1/4 of this transport passes through the passage between Iriomote and Okinawa. The calculation of heat balance indicates that the South China Sea absorbs net heat flux from the sun and atmosphere with a rate of 0.08 PW, while the atmosphere gains net heat flux from the Baohai, Yellow and East China Seas with a rate of 0.05 PW.
关键词South China Sea East China Sea Volume Transport Heat Transport Salt Transport Heat Balance Indonesian Throughflow
学科领域Geosciences, Multidisciplinary
收录类别SCI
语种英语
WOS记录号WOS:000181268700006
引用统计
被引频次:70[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/2510
专题海洋环流与波动重点实验室
作者单位1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
2.State Ocean Adm, Key Lab Marine Sci & Numer Modelling, Qingdao 266061, Peoples R China
3.Sungkyunkwan Univ, Dept Civil & Environm Engn, Suwon 440746, South Korea
4.Texas A&M Univ, Dept Oceanog, College Stn, TX 77843 USA
5.Chinese Acad Sci, Inst Atmospher Phys, LASG, Beijing 100029, Peoples R China
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GB/T 7714
Fang, GH,Wei, ZX,Choi, BH,et al. Interbasin freshwater, heat and salt transport through the boundaries of the East and South China Seas from a variable-grid global ocean circulation model[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2003,46(2):149-161.
APA Fang, GH,Wei, ZX,Choi, BH,Wang, H,Fang, Y,&Li, W.(2003).Interbasin freshwater, heat and salt transport through the boundaries of the East and South China Seas from a variable-grid global ocean circulation model.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,46(2),149-161.
MLA Fang, GH,et al."Interbasin freshwater, heat and salt transport through the boundaries of the East and South China Seas from a variable-grid global ocean circulation model".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 46.2(2003):149-161.
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