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Vertical structure of tidal currents in the Xuliujing Section of Changjiang River Estuary
被引:0
作者:
Chen, Zhigao
[1
,2
,3
,4
]
Ban, Ya
[2
]
Chen, Xiaoye
[1
]
Li, Dajun
[1
]
Wang, Shengping
[1
,4
]
机构:
[1] East China Univ Technol, Fac Geomat, Nanchang 330013, Peoples R China
[2] Chongqing Acad Metrol & Qual Inspect, Chongqing 401120, Peoples R China
[3] Nanjing White Shark Surveying & Mapping Technol Co, Nanjing 210038, Peoples R China
[4] Minist Nat Resources, Key Lab Marine Environm Survey Technol & Applicat, Guangzhou 510300, Peoples R China
基金:
中国国家自然科学基金;
关键词:
vertical structure;
seasonal variations;
tidal current;
mean current;
acoustic Doppler current profiler;
Changjiang River Estuary;
YANGTZE-RIVER;
SHELF;
CHINA;
VARIABILITY;
DISCHARGE;
STRAIT;
D O I:
10.1007/s13131-021-1976-y
中图分类号:
P7 [海洋学];
学科分类号:
0707 ;
摘要:
Three long-term fixed acoustic Doppler current profilers were first used for investigating the vertical structure of tidal currents in Xuliujing Section of Changjiang River Estuary. Moreover, three different periods (spring, summer and fall) were also considered for investigating seasonal variations. The semi-diurnal tides were the most energetic, with along-channel speed of up to 80 cm/s for M-2 constituent, which dominates at all stations with percent energy up to 65%-75% during seasons. The shape of tidal ellipses of the most energetic semi-diurnal constituent M-2 showed obvious polarization of the flow paralleling to the riverbank, with the minor semi-axis being generally less than 20% of the major one. The maximum velocity of mean current is appeared in top layers at all the three stations, and the velocity decreased with the depth. The seasonal variations of direction are also observed, which is probably caused by complex local topography since the erosion and deposition in riverbed. Observed vertical variation of four parameters of M-2 ellipses, agreed well with the optimally fit frictional solutions in top and middle layers. However, there was an obvious difference between frictional model and observed data in the lower water column. Discrepancies are probably on account of stratification, which strengthens in summer and fall due to the freshening influence of the Changjiang River Estuary outflow.
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页码:44 / 55
页数:12
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