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The effect of a barrier on tidally forced flow in a density-stratified estuary

机译:屏障对密度分层河口潮汐强迫流动的影响

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Numerical simulations of a two-layer set of shallow water equations are used to study the effect of density stratification on tidally forced flow over a barrier in large estuaries. Previous work has shown that for a homogeneous fluid, the blocking effect of the barrier is strongly affected by the quadratic bottom stress. In particular, it was found that there was a nonlinear response to the tidal forcing, in that as the tidal forcing amplitude increased, so did the effect of the barrier in reducing the tidal range on the landward side of the barrier, but the magnitude of this blocking effect was greater than would be predicted by a linear relationship with the tidal forcing amplitude. Here, we find a similar phenomenon for a two-layer fluid model, which has both a free-surface displacement and an interface displacement. We find that the density stratification tends to enhance the blocking effect of the barrier when compared to a homogeneous fluid. Further, we find that the barrier induces significant internal tides, and also can cause a mean set-up of both layers on the landward side of the barrier. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 11]
机译:使用两层浅水方程组的数值模拟来研究密度分层对大河口屏障上的潮汐强迫作用的影响。先前的工作表明,对于均质流体,势垒的阻挡作用会受到二次底应力的强烈影响。特别是,发现对潮汐强迫存在非线性响应,因为随着潮汐强迫幅度的增加,障碍物的作用也减小了障碍物着陆侧的潮汐范围,但减小了这种阻挡作用大于与潮汐强迫幅度呈线性关系所预期的作用。在这里,对于两层流体模型,我们发现了类似的现象,该模型同时具有自由表面位移和界面位移。我们发现,与均匀流体相比,密度分层趋于增强屏障的阻挡效果。此外,我们发现障碍物引起了明显的内部潮汐,并且还可能导致障碍物着陆侧的两层平均沉降。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:11]

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