Temperature inversion in the Huanghai Sea bottom cold water in summer

doi:10.1007/s13131-013-0287-3

IOCAS-IR > 海洋环流与波动重点实验室

	Temperature inversion in the Huanghai Sea bottom cold water in summer
	Yuan Dongliang1,2 ; Li Yao 1,2,3; Qiao Fangli 4; Zhao Wei 4; Yuan, DL
	2013-03-01
发表期刊	ACTA OCEANOLOGICA SINICA
ISSN	0253-505X
卷号	32 期号:3 页码:42-47
文章类型	Article
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.; 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.
关键词	Temperature Inversion Huanghai Sea Bottom Cold Water Huanghai Sea Cold Water Mass Summer
学科领域	Oceanography
DOI	10.1007/s13131-013-0287-3
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:000316239100006
WOS关键词	YELLOW SEA ; CIRCULATION
WOS标题词	Science & Technology ; Physical Sciences
引用统计	被引频次：13[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/16438
专题	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
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	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.

条目包含的文件
文件名称/大小	文献类型	版本类型	开放类型	使用许可
Temperature inversio（1066KB）			限制开放	CC BY-NC-SA	浏览