The subsurface water in the North Pacific tropical gyre
文献类型：期刊论文
| 作者 | Wang, Fan ; Li, Yuanlong; Zhang, Yanhui; Hu, Dunxin; Wang, F
|
| 刊名 | DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
 |
| 出版日期 | 2013-05-01 |
| 卷号 | 75页码:78-92 |
| 关键词 | Water mass North Pacific tropical gyre North Pacific Tropical water Subsurface salinity maximum Ventilated thermocline |
| ISSN号 | 0967-0637 |
| 通讯作者 | Wang, F |
| 中文摘要 | The subsurface water (22.5-25.5 sigma(0)) in the North Pacific tropical gyre (NPTG; 130 degrees E-150 degrees W, 5 degrees-10 degrees N), addressed as the North Pacific tropical subsurface water (TSSW), features a lateral salinity minimum and vertical salinity maximum in the western and central Pacific Ocean. In this study this water body is investigated using Argo float profiles and Word Ocean Atlas 2009 (WOA09) dataset. Comparing with the North Pacific Tropical water (NPTW), the TSSW is of lower salinity, lower oxygen, higher nutrient concentration, and denser vertical salinity maximum S-max. Subtropical ventilation and local ocean dynamics are both important in setting up its unique characteristics. Our analysis shows that its properties, structure, and seasonal variations are diverse at different longitudes. In the western Pacific, the TSSW is mainly of North Pacific water origin. Its high salinity core is formed by the southward intrusion of the NPTW. Diapycnal mixing with the surface-layer fresh water reduces its salinity and lowers its S-max to denser isopycnals. The TSSW in the western Pacific can be regarded as a diluted portion of the NPTW. In the central Pacific, advection of salty water masses from both hemispheres and westward invasion of the eastern Pacific fresh water are all important in regulating its characteristics. The TSSW in the central Pacific is a mixture of various water sources formed under highly variable flow pattern and intensive mixing. The TSSW should be regarded as an important subsurface water body connecting North/South Pacific thermocline water, although it might not be a water mass by traditional definition. (C) 2013 Elsevier Ltd. All rights reserved. |
| 英文摘要 | The subsurface water (22.5-25.5 sigma(0)) in the North Pacific tropical gyre (NPTG; 130 degrees E-150 degrees W, 5 degrees-10 degrees N), addressed as the North Pacific tropical subsurface water (TSSW), features a lateral salinity minimum and vertical salinity maximum in the western and central Pacific Ocean. In this study this water body is investigated using Argo float profiles and Word Ocean Atlas 2009 (WOA09) dataset. Comparing with the North Pacific Tropical water (NPTW), the TSSW is of lower salinity, lower oxygen, higher nutrient concentration, and denser vertical salinity maximum S-max. Subtropical ventilation and local ocean dynamics are both important in setting up its unique characteristics. Our analysis shows that its properties, structure, and seasonal variations are diverse at different longitudes. In the western Pacific, the TSSW is mainly of North Pacific water origin. Its high salinity core is formed by the southward intrusion of the NPTW. Diapycnal mixing with the surface-layer fresh water reduces its salinity and lowers its S-max to denser isopycnals. The TSSW in the western Pacific can be regarded as a diluted portion of the NPTW. In the central Pacific, advection of salty water masses from both hemispheres and westward invasion of the eastern Pacific fresh water are all important in regulating its characteristics. The TSSW in the central Pacific is a mixture of various water sources formed under highly variable flow pattern and intensive mixing. The TSSW should be regarded as an important subsurface water body connecting North/South Pacific thermocline water, although it might not be a water mass by traditional definition. (C) 2013 Elsevier Ltd. All rights reserved. |
| WOS标题词 | Science & Technology ; Physical Sciences |
| 学科主题 | Oceanography |
| 类目[WOS] | Oceanography |
| 研究领域[WOS] | Oceanography |
| 关键词[WOS] | SEA-SURFACE SALINITY ; MERIDIONAL OVERTURNING CIRCULATION ; WESTERN EQUATORIAL PACIFIC ; PHILIPPINE SEA ; INTERANNUAL VARIABILITY ; THERMOCLINE WATER ; BARRIER LAYER ; ROSSBY WAVES ; OCEAN ; PRECIPITATION |
| 收录类别 | SCI |
| 原文出处 | 10.1016/j.dsr.2013.01.002 |
| 语种 | 英语 |
| WOS记录号 | WOS:000317888800007 |
| 公开日期 | 2014-07-17 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/16444]  |
| 专题 | 海洋研究所_海洋环流与波动重点实验室 |
| 通讯作者 | Wang, F |
| 作者单位 | Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Fan,Li, Yuanlong,Zhang, Yanhui,et al. The subsurface water in the North Pacific tropical gyre[J]. DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,2013,75:78-92. |
| APA | Wang, Fan,Li, Yuanlong,Zhang, Yanhui,Hu, Dunxin,&Wang, F.(2013).The subsurface water in the North Pacific tropical gyre.DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,75,78-92. |
| MLA | Wang, Fan,et al."The subsurface water in the North Pacific tropical gyre".DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS 75(2013):78-92. |
入库方式： OAI收割
来源：海洋研究所
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