Temperature inversion in China seas
Hao, Jiajia1; Chen, Yongli2; Wang, Fan2
发表期刊JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
2010-12-10
卷号115期号:.页码:C12025-
关键词Warm Current Yellow Water
产权排序[Hao, Jiajia] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China; [Chen, Yongli; Wang, Fan] Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
通讯作者Hao, JJ, Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
作者部门信息集成与应用实验室
英文摘要Temperature inversion was reported as a common phenomenon in the areas near the southeastern Chinese coast (region A), west and south of the Korean Peninsula (region B), and north and east of the Shandong Peninsula (region C) during October-May in the present study, based on hydrographic data archived from 1930 through 2001 (319,029 profiles). The inversion was found to be remarkable with obvious temporal and spatial variabilities in both magnitude and coverage, with higher probabilities in region A (up to about 60%) and region C (40%-50%) than in region B (15%-20%). The analysis shows that seasonal variation of the net air-sea heat flux is closely related to the occurrence time of the inversion in the three areas, while the Yangtze and Yellow river freshwater plumes in the surface layer and ocean origin saline water in the subsurface layer maintain stable stratification. It seems that the evaporation/excessive precipitation flux makes little contribution to maintaining the stable inversion. Advection of surface fresh water by the wind-driven coastal currents results in the expansion of inversion in regions A and C. The inversion lasts for the longest period in region A (October-May) sustained by the Taiwan Warm Current carrying the subsurface saline water, while evolution of the inversion in region B is mainly controlled by the Yellow Sea Warm Current.; Temperature inversion was reported as a common phenomenon in the areas near the southeastern Chinese coast (region A), west and south of the Korean Peninsula (region B), and north and east of the Shandong Peninsula (region C) during October-May in the present study, based on hydrographic data archived from 1930 through 2001 (319,029 profiles). The inversion was found to be remarkable with obvious temporal and spatial variabilities in both magnitude and coverage, with higher probabilities in region A (up to about 60%) and region C (40%-50%) than in region B (15%-20%). The analysis shows that seasonal variation of the net air-sea heat flux is closely related to the occurrence time of the inversion in the three areas, while the Yangtze and Yellow river freshwater plumes in the surface layer and ocean origin saline water in the subsurface layer maintain stable stratification. It seems that the evaporation/excessive precipitation flux makes little contribution to maintaining the stable inversion. Advection of surface fresh water by the wind-driven coastal currents results in the expansion of inversion in regions A and C. The inversion lasts for the longest period in region A (October-May) sustained by the Taiwan Warm Current carrying the subsurface saline water, while evolution of the inversion in region B is mainly controlled by the Yellow Sea Warm Current.
文章类型Article
资助机构Chinese Academy of Sciences [KZCX1-YW-12, KZCX2-YW-Q11-02]
收录类别SCI
语种英语
关键词[WOS]WARM CURRENT ; YELLOW ; WATER
研究领域[WOS]Oceanography
WOS记录号WOS:000285260000001
引用统计
被引频次:29[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cn/handle/133337/4419
专题中国科学院海岸带环境过程与生态修复重点实验室_海岸带信息集成与战略规划研究中心
作者单位1.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
2.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China
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GB/T 7714
Hao, Jiajia,Chen, Yongli,Wang, Fan. Temperature inversion in China seas[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2010,115(.):C12025-.
APA Hao, Jiajia,Chen, Yongli,&Wang, Fan.(2010).Temperature inversion in China seas.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,115(.),C12025-.
MLA Hao, Jiajia,et al."Temperature inversion in China seas".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 115..(2010):C12025-.
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