Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Circulation in the western tropical Pacific Ocean and its seasonal variation | |
Wang, F; Chang, P; Hu, DX; Seidel, H | |
2002-04-01 | |
发表期刊 | CHINESE SCIENCE BULLETIN |
ISSN | 1001-6538 |
卷号 | 47期号:7页码:591-595 |
文章类型 | Article |
摘要 | An assimilation data set based on the GFDL MOM3 model and the NODC XBT data set is used to examine the circulation in the western tropical Pacific and its seasonal variations. The assimilated and observed velocities and transports of the mean circulation agree well. Transports of the North Equatorial Current (NEC), Mindanao Current (MC), North Equatorial Countercurrent (NECC) west of 140degreesE and Kuroshio origin estimated with the assimilation data display the seasonal cycles, roughly strong in boreal spring and weak in autumn, with a little phase difference. The NECC transport also has a semi-annual fluctuation resulting from the phase lag between seasonal cycles of two tropical gyres' recirculations. Strong in summer during the southeast monsoon period, the seasonal cycle of the Indonesian throughflow (ITF) is somewhat different from those of its upstreams, the MC and New Guinea Coastal Current (NGCC), implying the monsoon's impact on it.; An assimilation data set based on the GFDL MOM3 model and the NODC XBT data set is used to examine the circulation in the western tropical Pacific and its seasonal variations. The assimilated and observed velocities and transports of the mean circulation agree well. Transports of the North Equatorial Current (NEC), Mindanao Current (MC), North Equatorial Countercurrent (NECC) west of 140degreesE and Kuroshio origin estimated with the assimilation data display the seasonal cycles, roughly strong in boreal spring and weak in autumn, with a little phase difference. The NECC transport also has a semi-annual fluctuation resulting from the phase lag between seasonal cycles of two tropical gyres' recirculations. Strong in summer during the southeast monsoon period, the seasonal cycle of the Indonesian throughflow (ITF) is somewhat different from those of its upstreams, the MC and New Guinea Coastal Current (NGCC), implying the monsoon's impact on it. |
关键词 | Seasonal Circulations Equatorial Currents Low-latitude Western Boundary Currents Western Tropical Pacific Ocean Assimilation Data |
学科领域 | Multidisciplinary Sciences |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000175219200016 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/2534 |
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.Texas A&M Univ, Dept Oceanog, College Stn, TX 77843 USA |
推荐引用方式 GB/T 7714 | Wang, F,Chang, P,Hu, DX,et al. Circulation in the western tropical Pacific Ocean and its seasonal variation[J]. CHINESE SCIENCE BULLETIN,2002,47(7):591-595. |
APA | Wang, F,Chang, P,Hu, DX,&Seidel, H.(2002).Circulation in the western tropical Pacific Ocean and its seasonal variation.CHINESE SCIENCE BULLETIN,47(7),591-595. |
MLA | Wang, F,et al."Circulation in the western tropical Pacific Ocean and its seasonal variation".CHINESE SCIENCE BULLETIN 47.7(2002):591-595. |
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