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On the developments of spectral wave models: numerics and parameterizations for the coastal ocean

机译:关于谱波模型的发展:沿海海洋的数值和参数化

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摘要

The development of numerical wave models for coastal applications, including coupling with ocean circulation models, has spurred an ongoing effort on theoretical foundations, numerical techniques, and physical parameterizations. Some important aspects of this effort are reviewed here, and results are shown in the case of the French Atlantic and Channel coast using version 4.18 of the WAVEWATCH Ⅲ~R model. Compared to previous results, the model errors have been strongly reduced thanks to, among other things, the introduction of currents, coastal reflection, and bottom sediment types. This last item is described here for the first time, allowing unprecedented accuracy at some sites along the French Atlantic Coast. The adequate resolution, necessary to represent strong gradients in tidal currents, was made possible by the efficiency brought by unstructured grids. A further increase in resolution, necessary to resolve surf zones and still cover vast regions,will require further developments in numerical methods.
机译:沿海应用的数值波浪模型的发展,包括与海洋环流模型的耦合,促使人们在理论基础,数值技术和物理参数化方面进行了不懈的努力。本文对这项工作的一些重要方面进行了回顾,并使用WAVEWATCHⅢ〜R模型的4.18版在法国大西洋和海峡沿岸的情况下显示了结果。与以前的结果相比,由于引入了水流,海岸反射和底部沉积物类型等因素,大大减少了模型误差。这是最后一次在此进行描述,从而使法国大西洋沿岸的某些地点获得了空前的准确性。非结构化网格带来的效率使得代表潮流中的强梯度所必需的足够分辨率成为可能。解决海浪区并仍然覆盖广大地区所必需的分辨率的进一步提高将要求数值方法的进一步发展。

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