Observational and model studies of synoptic current fluctuations in the Bohai Strait on the Chinese continental shelf

被引:36
作者
Ding, Yang [1 ,2 ]
Bao, Xianwen [1 ,2 ,3 ]
Yao, Zhigang [3 ]
Bi, Congcong [1 ,2 ,3 ]
Wan, Kai [4 ]
Bao, Min [5 ]
Jiang, Zhipeng [1 ,2 ,3 ]
Song, Jun [6 ]
Gao, Jia [7 ]
机构
[1] Ocean Univ China, Key Lab Phys Oceanog, Minist Educ, Qingdao, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Qingdao, Peoples R China
[3] Ocean Univ China, Coll Ocean & Atmospher Sci, Qingdao 266100, Peoples R China
[4] State Ocean Adm, North China Sea Marine Engn Prospecting Inst, Qingdao, Peoples R China
[5] State Ocean Adm, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou, Zhejiang, Peoples R China
[6] Dalian Ocean Univ, Sch Marine Sci & Environm Engn, Dalian, Peoples R China
[7] Natl Marine Data & Informat Serv, Tianjin, Peoples R China
基金
中国国家自然科学基金;
关键词
Bohai Strait; Synoptic fluctuation; Inflow and outflow; Winter storm; Water exchange; Coastal-trapped wave; COASTAL-TRAPPED WAVES; SUSPENDED-SEDIMENT; SEA; TRANSPORT; YELLOW; OCEAN;
D O I
10.1007/s10236-019-01247-5
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Three winter storms struck the Bohai and Yellow seas in succession during February 16-25, 2017. Periodic fluctuations of sea level, currents, temperature, and salinity were recorded at a moored station deployed in the Bohai Strait. Observations also captured significant synoptic fluctuations of inflow and outflow through the Bohai Strait with maximum magnitude exceeding 50cms(-1). The sea level dropped by >1m and the bottom temperature decreased by 2.5 degrees C in <30h during these winter storms. A regional ocean model was used to investigate the prominent fluctuations of synoptic exchange flow through the Bohai Strait. The model results indicated that the Bohai and Yellow seas in their entirety responded strongly to the storm bursts and subsequent relaxation at the synoptic scale. The periodic winter storm bursts and relaxation excited the cyclonic propagation of coastal-trapped waves around the Bohai and Yellow seas. Strong periodic inflow and outflow during the passage of the three successive storms promoted water exchange between the Bohai Sea and the northern Yellow Sea. Successive winter storms might also affect the mean current structure through the Bohai Strait. The mean currents through the Bohai Strait during the studied storm period were characterized by inflow in both northern and southern parts of the strait and outflow through the middle of the strait. This arrangement is different from the traditional view of inflow via the northern channel and outflow through the southern channel.
引用
收藏
页码:323 / 351
页数:29
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