Vertical structure of tidal currents in the Xuliujing Section of Changjiang River Estuary

• Published in: Acta oceanologica Sinica 2023-02, Vol.42 (2), p.44-55
• Main Authors: Chen, Zhigao, Ban, Ya, Chen, Xiaoye, Li, Dajun, Wang, Shengping
• Format: Article
• Language: English
• Subjects: Climatology; Constituents; Diurnal; Diurnal tides; Doppler sonar; Earth and Environmental Science; Earth Sciences; Ecology; Ellipses; Engineering Fluid Dynamics; Environmental Chemistry; Estuaries; Estuarine dynamics; Marine & Freshwater Sciences; Ocean currents; Oceanography; Outflow; Profilers; River banks; River beds; River erosion; Riverbanks; Riverbeds; Rivers; Seasonal variation; Seasonal variations; Seasons; Semidiurnal tides; Stratification; Summer; Tidal currents; Velocity; Vertical profiles; Water circulation; Water column; Water outflow
• ISSN: 0253-505X; 1869-1099
• DOI: 10.1007/s13131-021-1976-y

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.