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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >The influence of tidal currents on the asymmetry of tide-dominated ebb-tidal deltas
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The influence of tidal currents on the asymmetry of tide-dominated ebb-tidal deltas

机译:潮流对潮汐主导的潮汐三角洲不对称性的影响

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An idealized numerical model is developed to study the spatial asymmetry of ebb-tidal deltas under influence of large-scale alongshore tidal currents. It is shown that the asymmetry of the delta depends on the magnitude of the cross-shore and large scale alongshore tidal currents, their phase difference, and on the width of the inlet. Model results are compared with observations of ebb-tidal deltas of the tidal inlet systems of the Dutch Wadden Sea and with the ebb-tidal delta of the Eastern Scheldt, located in the southwestern part of the Netherlands. The modeled current and residual sediment transport patterns agree well with observed ones. The modeled asymmetry of the ebb tidal delta also agree with observed ones. Furthermore, bottom patterns are consistent with those found with a previous version of the idealized model which focused on the modeling of symmetric ebb tidal deltas. However, the model is not able to reproduce the observed ebb-dominated channel. The underlying physical processes are explained in terms of vorticity dynamics. The convergence of the mean vorticity flux generates mean vorticity and thereby residual circulation. An analysis shows there is competition between two contributions to the convergence of the mean vorticity flux. This competition explains the sensitivity of the results to the model parameters. (c) 2008 Elsevier Ltd. All rights reserved.
机译:建立了一个理想的数值模型来研究在大规模沿海潮汐流的影响下潮汐三角洲的空间不对称性。结果表明,三角洲的不对称性取决于跨岸和大规模沿岸潮流的大小,它们的相位差以及入口的宽度。将模型结果与荷兰瓦登海潮汐入口系统的潮汐三角洲观测值以及位于荷兰西南部的东部谢尔德的潮汐三角洲观测结果进行了比较。模拟的当前和剩余泥沙运移模式与观测到的相吻合。潮汐退潮三角洲的模型不对称性也与观测到的一致。此外,底部模式与理想化模型先前版本中发现的模式一致,后者侧重于对称潮汐潮汐三角洲的建模。但是,该模型无法重现观察到的退潮控制通道。潜在的物理过程是根据涡度动力学来解释的。平均涡度通量的收敛产生平均涡度,从而产生残余循环。分析表明,在平均涡度通量收敛的两个贡献之间存在竞争。这次比赛解释了结果对模型参数的敏感性。 (c)2008 Elsevier Ltd.保留所有权利。

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