Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Revisit the interannual variability of the North Equatorial Current transport with ECMWF ORA-S3 | |
Zhai, Fangguo1,2,3; Hu, Dunxin1,2; Hu, DX | |
2013-03-01 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS |
ISSN | 2169-9275 |
卷号 | 118期号:3页码:1349-1366 |
文章类型 | Article |
摘要 | The interannual variability of the North Equatorial Current (NEC) transport in the tropical northwestern Pacific Ocean is investigated with the output from ECMWF Ocean Analysis/Reanalysis System 3 (ORA-S3). The results show that the amplitude and root mean square (RMS) of interannual NEC transport anomalies increase from about 3.0-4.0 Sv and 2.0 Sv at 170 degrees E to above 5.0 and 3.4 Sv at 135 degrees E, respectively. The NEC transport variation agrees well with the variation of the sea surface height (SSH) anomaly difference between the southern and northern boundaries of the NEC region. Further analysis near the Philippine coast suggests that their good agreement mainly comes from the agreement of the NEC transport and SSH variations south of the gyre boundary. Around the bifurcation point off the Philippine coast, the southern branch of the NEC transport is highly related to El Nino-Southern Oscillation (ENSO) events. During El Nino/La Nina years, westerly/easterly wind anomalies and positive/negative wind stress curl anomalies develop in the tropical northwestern Pacific Ocean south of 20 degrees N before the mature phase. The wind forcing center moves eastward with time and reaches the easternmost position around 170 degrees E several months before the mature phase. This wind forcing generates upwelling/downwelling Rossby waves, which propagate westward to result in negative/positive SSH anomalies, hence inducing a cyclonic/anticyclonic gyre anomaly, which is responsible for the increase/decrease of the NEC transport. The northern branch of the NEC transport near the Philippine coast has no significant simultaneous relation with ENSO events.; The interannual variability of the North Equatorial Current (NEC) transport in the tropical northwestern Pacific Ocean is investigated with the output from ECMWF Ocean Analysis/Reanalysis System 3 (ORA-S3). The results show that the amplitude and root mean square (RMS) of interannual NEC transport anomalies increase from about 3.0-4.0 Sv and 2.0 Sv at 170 degrees E to above 5.0 and 3.4 Sv at 135 degrees E, respectively. The NEC transport variation agrees well with the variation of the sea surface height (SSH) anomaly difference between the southern and northern boundaries of the NEC region. Further analysis near the Philippine coast suggests that their good agreement mainly comes from the agreement of the NEC transport and SSH variations south of the gyre boundary. Around the bifurcation point off the Philippine coast, the southern branch of the NEC transport is highly related to El Nino-Southern Oscillation (ENSO) events. During El Nino/La Nina years, westerly/easterly wind anomalies and positive/negative wind stress curl anomalies develop in the tropical northwestern Pacific Ocean south of 20 degrees N before the mature phase. The wind forcing center moves eastward with time and reaches the easternmost position around 170 degrees E several months before the mature phase. This wind forcing generates upwelling/downwelling Rossby waves, which propagate westward to result in negative/positive SSH anomalies, hence inducing a cyclonic/anticyclonic gyre anomaly, which is responsible for the increase/decrease of the NEC transport. The northern branch of the NEC transport near the Philippine coast has no significant simultaneous relation with ENSO events. |
学科领域 | Oceanography |
DOI | 10.1002/jgrc.20093 |
URL | 查看原文 |
收录类别 | SCI |
语种 | 英语 |
WOS研究方向 | Oceanography |
WOS类目 | Oceanography |
WOS记录号 | WOS:000320323200021 |
WOS关键词 | NINO-SOUTHERN-OSCILLATION ; BAROCLINIC ROSSBY WAVES ; PACIFIC-OCEAN ; CURRENT BIFURCATION ; TROPICAL PACIFIC ; WESTERN BOUNDARY ; MINDANAO CURRENT ; CIRCULATION ; PHILIPPINES ; KUROSHIO |
WOS标题词 | Science & Technology ; Physical Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/16429 |
专题 | 海洋环流与波动重点实验室 |
通讯作者 | Hu, DX |
作者单位 | 1.Chinese Acad Sci, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 3.State Ocean Adm, Inst Oceanog 3, Xiamen, Peoples R China |
第一作者单位 | 海洋环流与波动重点实验室; 中国科学院海洋研究所 |
推荐引用方式 GB/T 7714 | Zhai, Fangguo,Hu, Dunxin,Hu, DX. Revisit the interannual variability of the North Equatorial Current transport with ECMWF ORA-S3[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2013,118(3):1349-1366. |
APA | Zhai, Fangguo,Hu, Dunxin,&Hu, DX.(2013).Revisit the interannual variability of the North Equatorial Current transport with ECMWF ORA-S3.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,118(3),1349-1366. |
MLA | Zhai, Fangguo,et al."Revisit the interannual variability of the North Equatorial Current transport with ECMWF ORA-S3".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 118.3(2013):1349-1366. |
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