1. Effect of Freshwater Discharge From Estuary Dam on Residual Circulation in Bifurcated Channel.
- Author
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Kim, J. W., Song, J. I., Yoon, B. I., and Woo, S.‐B.
- Subjects
FRESH water ,WATER quality ,HARMONIC analysis (Mathematics) ,ESTUARIES ,DAMS ,ADVECTION ,FRICTION - Abstract
The residual structure of the inner part of the Yeongsan River estuary has been reported to be a multi‐layer vertical structure, unlike the two‐layer vertical structure of a typical estuary, due to irregular freshwater discharge. The inner estuary has a main channel connected to the open sea, and a bifurcated channel system (sub‐channel) in its central part, which can affect the residual current. In this study, field observations of three‐dimensional velocity and salinity were conducted to understand the discharge effects on the residual current at bifurcated channels. The residual flows were estimated using least‐squares harmonic analysis. The relative contributions of advection acceleration and friction terms to nonlinear effects were evaluated using along‐channel momentum balance. In the absence of freshwater discharge, the flow patterns were dominated by tidal dynamics in the sub‐channel rather than the main channel, whereas most flow patterns during freshwater discharge were dominated by near‐surface strong velocity in the main channel. A multi‐layer vertical residual structure was observed during the non‐discharge period in the main channel, which was caused by the insertion of upstream residual flow from the sub‐channel. Nonlinear effects occurred at the bifurcation point of the two channels. During the non‐discharge period, the advection term was most dominant, whereas the vertical friction term was dominant during the discharge period. Moreover, the magnitude of the horizontal friction term was larger than that of the advection term. Therefore, freshwater discharge can lead to an increase in the friction term, which in turn can markedly affect the residual circulation. Plain Language Summary: Residual circulation is a common and influential process in the major estuaries and coastal regions of the world, and understanding this is of great significance with respect to marine material transport, water quality, and ecological processes. The tidal propagation and residual flow patterns through the bifurcated narrow channel of the inner part of the Yeongsan River estuary are connected to the center of the main channel, which can significantly contribute to the formation of a vertical residual flow structure. Residual circulation shows a noticeable change due to the strong flow caused by the freshwater discharge from the estuary dam. Nonlinear effects occurred largely at the bifurcation point of the two channels, and in this regard, the major mechanisms of residual circulation differed between the two channels. Channel bifurcations are artificially or naturally formed along various coasts, and our research results provide a good example of identifying the causes of environmental changes. Key Points: Multi‐layer vertical residual structure is due to induction of upstream residual flow from a narrow bifurcated channelNonlinear effects occur at the bifurcation point of the channelsThe advection term dominated during non‐discharge periods, whereas the vertical friction term dominated during discharge periods [ABSTRACT FROM AUTHOR]
- Published
- 2023
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