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SEASONAL VARIABILITY OF THE INDONESIAN THROUGHFLOW FROM A VARIABLE-GRID GLOBAL OCEAN MODEL
Wang Yong-gang1,2,3; Fang Guo-hong2; Wei Ze-xun2; Chen Hai-ying2; Wang Xin-yi2
2004
发表期刊JOURNAL OF HYDRODYNAMICS
卷号16期号:5页码:525-532
文章类型Article
摘要The objective of this study is to model the mean and seasonal mass transport of the Pacific to Indian Ocean throughflow using variable-grid global Ocean General Circulation Model (OGCM) with fine grid (1 degrees/6) covering the area from 20 S to 60 degrees N and from 98 E to 156 E. The computations show that Indonesian Throughflow (ITF) mass transport, computed as a sum of through-strait transport, has maximum transport in Sept. (17. 5Sv) and minimum transport in Jan. (9. 5Sv). The annual mean ITF transport amounts to 14. 5Sv. Twenty-two percent of this transport passes through Lombok Strait. Sixty-five percent of this transport passes through Timor Passage. Semi-annual variability is apparent in Lombok and Ombai Straits while annual variability is apparent in Timor Passage.
关键词Indonesian Throughflow Seasonal Variability Global Ocean Circulation Model
收录类别SCI
语种英语
WOS记录号WOS:000208261100003
引用统计
被引频次:3[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/337002/32508
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, Inst Oceanog 1, Key Lab Marine Sci & Numer Modeling, Qingdao 266061, Peoples R China
3.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China
第一作者单位中国科学院海洋研究所
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GB/T 7714
Wang Yong-gang,Fang Guo-hong,Wei Ze-xun,et al. SEASONAL VARIABILITY OF THE INDONESIAN THROUGHFLOW FROM A VARIABLE-GRID GLOBAL OCEAN MODEL[J]. JOURNAL OF HYDRODYNAMICS,2004,16(5):525-532.
APA Wang Yong-gang,Fang Guo-hong,Wei Ze-xun,Chen Hai-ying,&Wang Xin-yi.(2004).SEASONAL VARIABILITY OF THE INDONESIAN THROUGHFLOW FROM A VARIABLE-GRID GLOBAL OCEAN MODEL.JOURNAL OF HYDRODYNAMICS,16(5),525-532.
MLA Wang Yong-gang,et al."SEASONAL VARIABILITY OF THE INDONESIAN THROUGHFLOW FROM A VARIABLE-GRID GLOBAL OCEAN MODEL".JOURNAL OF HYDRODYNAMICS 16.5(2004):525-532.
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