Temperature inversion in the Huanghai Sea bottom cold water in summer
文献类型：期刊论文
| 作者 | Yuan Dongliang1,2 ; Li Yao1,2,3; Qiao Fangli4; Zhao Wei4; Yuan, DL
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| 刊名 | ACTA OCEANOLOGICA SINICA
 |
| 出版日期 | 2013-03-01 |
| 卷号 | 32期号:3页码:42-47 |
| 关键词 | temperature inversion Huanghai Sea bottom cold water Huanghai Sea cold water mass summer |
| ISSN号 | 0253-505X |
| 通讯作者 | Yuan, DL |
| 中文摘要 | Using conductivity-Temperature-depth data of a recent cruise during July 22-28, 2008 and historical data, it is found that temperature inversions occur from time to time in the Huanghai Sea(Yellow Sea) cold water mass (HSCWM) in summer. The temperature inversions are produced by the movement of the fresh and cold HSCWM masses above the warm and saline Huanghai Sea Warm Current water at the central bottom of the Huanghai Sea Trough. The non-homogeneous profiles of the temperature and the salinity suggest that vertical mixing in the HSCWM, which is of great importance to the circulation in the Huanghai Sea in summer, is weak. Trajectories of satellite-tracked surface drifters suggest that waters in the northern reach of the Huanghai Sea move southward along the 40-50 m isobaths and descend into the southern Huanghai Sea to form the western core of the HSCWM. |
| 英文摘要 | Using conductivity-Temperature-depth data of a recent cruise during July 22-28, 2008 and historical data, it is found that temperature inversions occur from time to time in the Huanghai Sea(Yellow Sea) cold water mass (HSCWM) in summer. The temperature inversions are produced by the movement of the fresh and cold HSCWM masses above the warm and saline Huanghai Sea Warm Current water at the central bottom of the Huanghai Sea Trough. The non-homogeneous profiles of the temperature and the salinity suggest that vertical mixing in the HSCWM, which is of great importance to the circulation in the Huanghai Sea in summer, is weak. Trajectories of satellite-tracked surface drifters suggest that waters in the northern reach of the Huanghai Sea move southward along the 40-50 m isobaths and descend into the southern Huanghai Sea to form the western core of the HSCWM. |
| 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] | YELLOW SEA ; CIRCULATION |
| 收录类别 | SCI |
| 原文出处 | 10.1007/s13131-013-0287-3 |
| 语种 | 英语 |
| WOS记录号 | WOS:000316239100006 |
| 公开日期 | 2014-07-17 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/16438]  |
| 专题 | 海洋研究所_海洋环流与波动重点实验室 |
| 通讯作者 | Yuan, DL |
| 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.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 4.State Ocean Adm, Inst Oceanog 1, Qingdao 266061, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yuan Dongliang,Li Yao,Qiao Fangli,et al. Temperature inversion in the Huanghai Sea bottom cold water in summer[J]. ACTA OCEANOLOGICA SINICA,2013,32(3):42-47. |
| APA | Yuan Dongliang,Li Yao,Qiao Fangli,Zhao Wei,&Yuan, DL.(2013).Temperature inversion in the Huanghai Sea bottom cold water in summer.ACTA OCEANOLOGICA SINICA,32(3),42-47. |
| MLA | Yuan Dongliang,et al."Temperature inversion in the Huanghai Sea bottom cold water in summer".ACTA OCEANOLOGICA SINICA 32.3(2013):42-47. |
入库方式： OAI收割
来源：海洋研究所
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