Temperature inversion in China seas
Hao, Jiajia1; Chen, Yongli2; Wang, Fan2
刊名JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
2010-12-10
卷号115期号:.页码:C12025-
关键词Warm Current Yellow Water
通讯作者Hao, JJ, Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
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
文献子类Article
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.
学科主题Oceanography
WOS关键词WARM CURRENT ; YELLOW ; WATER
WOS研究方向Oceanography
语种英语
WOS记录号WOS:000285260000001
资助机构Chinese Academy of Sciences [KZCX1-YW-12, KZCX2-YW-Q11-02]
内容类型期刊论文
源URL[http://ir.yic.ac.cn/handle/133337/4420]  
专题烟台海岸带研究所_海岸带信息集成与综合管理实验室
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
推荐引用方式
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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