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首页> 外文期刊>Estuarine Coastal and Shelf Science >Role of continental shelf on non-linear interaction of storm surges, tides and wind waves: An idealized study representing the west coast of India
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Role of continental shelf on non-linear interaction of storm surges, tides and wind waves: An idealized study representing the west coast of India

机译:大陆架在风暴潮,潮汐和风浪的非线性相互作用中的作用:代表印度西海岸的理想化研究

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The study reports role and dependence of continental shelf geometry on the non-linear interaction of storm surges, tides, and wind waves. As a case study, the shelf geometry representing the west coast of India is considered and numerical simulations are executed using the standard representation of a tropical cyclone. The idealized experiments assume the west coast of India as a straight coastline with varying continental shelf width ranging from 35 km in the south to 330 km in the north. For the experiments. ADCIRC model in standalone mode and coupled ADCIRC+SWAN are used by considering 13 idealized cyclone tracks covering the study domain. It is noticed that an amplification of peak storm surge of similar to 12 cm for every 10 km increase in the shelf width. During different phases of the tide, the surge-wave interaction modifies the water level elevation and its occurrence as the tidal range increases towards north. The interaction of tides on surges and wind waves is observed maximum at low-tide and minimum at flood tide over the wide shelf regions. In general, the non-linear interaction is found to be 15%-20% for any cyclone track or tidal phase. The wave setup caused by wind waves is marginally varies with change of amplitude and phase of the tide, however, its profile is significantly modified, particularly over the wider shelf widths. (C) 2017 Elsevier Ltd. All rights reserved.
机译:这项研究报告了大陆架几何形状对风暴潮,潮汐和风浪的非线性相互作用的作用和依赖性。作为案例研究,考虑了代表印度西海岸的层架几何形状,并使用热带气旋的标准表示法进行了数值模拟。理想化的实验假设印度西海岸为直线海岸线,大陆架宽度从南部的35公里到北部的330公里不等。对于实验。独立模式下的ADCIRC模型和耦合的ADCIRC + SWAN通过考虑涵盖研究领域的13条理想化的气旋轨道来使用。可以注意到,货架宽度每增加10 km,峰值风暴潮的放大幅度将接近12 cm。在潮汐的不同阶段,随着潮汐范围向北增加,浪涌波相互作用会改变水位升高及其发生。在宽阔的陆架区域,潮汐与潮汐和风浪的相互作用在低潮时观察到最大,而在洪潮时观察到最小。通常,对于任何旋风径迹或潮汐期,非线性相互作用为15%-20%。风浪引起的波浪形成随潮汐的幅度和相位的变化而略有变化,但是,其轮廓被显着改变,尤其是在较宽的层架宽度上。 (C)2017 Elsevier Ltd.保留所有权利。

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