Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Interannual sea surface salinity variations observed in the tropical North Pacific Ocean | |
Li, Yuanlong1,2; Wang, Fan2; Han, Weiqing1; Wang, F | |
2013-05-28 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
卷号 | 40期号:10页码:2194-2199 |
文章类型 | Article |
摘要 | Analysis of observational data sets reveals pronounced interannual variations of sea surface salinity (SSS) in the tropical North Pacific (7 degrees N-15 degrees N) during 2000-2012. SSS anomalies with maximum magnitudes >0.2 occur in the central Pacific and translate westward at a speed of 15-20 cm s(-1). The signals are weakened during their westward movement but reinforced in the Philippine Sea. Budget analysis for the mixed layer salinity suggests that in the central Pacific, El Nino-Southern Oscillation-related atmospheric freshwater forcing and ocean advection changes are both important in generating and maintaining these large SSS anomalies. In the advection term, the most contributing component is the meridional Ekman advection induced by trade winds. These SSS anomalies are subsequently carried westward by the North Equatorial Current, which is the primary cause of SSS variations in the Philippine Sea. Freshwater forcing is also at work in the Philippine Sea, but its role is generally secondary.; Analysis of observational data sets reveals pronounced interannual variations of sea surface salinity (SSS) in the tropical North Pacific (7 degrees N-15 degrees N) during 2000-2012. SSS anomalies with maximum magnitudes >0.2 occur in the central Pacific and translate westward at a speed of 15-20 cm s(-1). The signals are weakened during their westward movement but reinforced in the Philippine Sea. Budget analysis for the mixed layer salinity suggests that in the central Pacific, El Nino-Southern Oscillation-related atmospheric freshwater forcing and ocean advection changes are both important in generating and maintaining these large SSS anomalies. In the advection term, the most contributing component is the meridional Ekman advection induced by trade winds. These SSS anomalies are subsequently carried westward by the North Equatorial Current, which is the primary cause of SSS variations in the Philippine Sea. Freshwater forcing is also at work in the Philippine Sea, but its role is generally secondary. |
关键词 | Sea Surface Salinity Mixed Layer Enso |
学科领域 | Geology |
DOI | 10.1002/grl.50429 |
URL | 查看原文 |
收录类别 | SCI |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000328840200055 |
WOS关键词 | FRESH POOL ; EL-NINO ; VARIABILITY ; PERIOD ; LAYER ; ARGO |
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/337002/16415 |
专题 | 海洋环流与波动重点实验室 |
通讯作者 | Wang, F |
作者单位 | 1.Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA 2.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Shandong, Peoples R China |
第一作者单位 | 海洋环流与波动重点实验室 |
推荐引用方式 GB/T 7714 | Li, Yuanlong,Wang, Fan,Han, Weiqing,et al. Interannual sea surface salinity variations observed in the tropical North Pacific Ocean[J]. GEOPHYSICAL RESEARCH LETTERS,2013,40(10):2194-2199. |
APA | Li, Yuanlong,Wang, Fan,Han, Weiqing,&Wang, F.(2013).Interannual sea surface salinity variations observed in the tropical North Pacific Ocean.GEOPHYSICAL RESEARCH LETTERS,40(10),2194-2199. |
MLA | Li, Yuanlong,et al."Interannual sea surface salinity variations observed in the tropical North Pacific Ocean".GEOPHYSICAL RESEARCH LETTERS 40.10(2013):2194-2199. |
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