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首页> 外文期刊>Estuarine Coastal and Shelf Science >Nearshore hydrodynamics at pocket beaches with contrasting wave exposure in southern Portugal
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Nearshore hydrodynamics at pocket beaches with contrasting wave exposure in southern Portugal

机译:葡萄牙南部波涛汹涌的小型海滩近岸水动力

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Pocket beaches on rocky coasts with headlands that control hydro-sedimentary processes are considered to be constrained sedimentary systems, generally with limited sediment inputs. Pocket beaches face severe changes over time. Under worst-case scenarios, these changes can result in the loss of the beach, causing waves to directly attack adjacent cliffs. Studies of nearshore hydrodynamics can help to understand such changes and optimise sediment nourishment procedures. The present work contributes to the knowledge of hydrodynamic forcing mechanisms at pocket beaches by providing a comprehensive description of the nearshore circulation at two beaches with contrasting wave exposures. Two pocket beaches in southern Portugal were studied by combining field measurements of waves and currents with numerical models (STWAVE and BOUSS-2D). The aim of this analysis was to evaluate nearshore hydrodynamics under different wave exposure forcing conditions (e.g. variable wave heights/directions and different tidal levels). The results show that the beach circulation can rapidly shift from longshore-to rip-dominated depending on changes in both the offshore wave direction and tidal levels. Waves with higher obliquity (for both low and moderate wave energy conditions) tend to generate longshore circulation in all considered tidal stages, while waves with lower obliquity tend to produce rip flow with higher-velocity rip currents during low to intermediate tidal stages. The results indicate that the location and intensity of rip currents strongly depend on geomorphological constraints, that is, the control exerted by shore platforms. A larger morphological control is observed at mean sea level because most platforms are submerged exposed during high/low tide and therefore exert less control on nearshore circulation. (C) 2018 Elsevier Ltd. All rights reserved.
机译:在岩石海岸上具有控制水沉积过程的岬角的小型海滩被认为是受约束的沉积系统,通常只有有限的沉积物输入。随时间推移,口袋海滩面临着严重的变化。在最坏的情况下,这些变化可能会导致海滩的损失,从而使海浪直接袭击相邻的悬崖。对近岸水动力的研究可以帮助理解这种变化并优化沉积物的营养程序。通过提供对两个海滩的近岸环流和波浪暴露对比的全面描述,当前的工作有助于了解袋状海滩的水动力强迫机制。通过将波浪和海流的现场测量与数值模型(STWAVE和BOUSS-2D)相结合,研究了葡萄牙南部的两个口袋海滩。该分析的目的是评估在不同的波浪暴露强迫条件下(例如,不同的波浪高度/方向和不同的潮汐水平)的近岸水动力。结果表明,取决于海上波浪方向和潮汐水平的变化,海滩环流可以迅速地从长岸向以rip裂为主。倾角较高的波浪(在低和中等波浪能条件下)在所有考虑的潮汐阶段都倾向于产生长岸环流,而倾角较低的波浪在中低潮汐阶段倾向于以较高的速度产生激流。结果表明,裂隙水流的位置和强度在很大程度上取决于地貌约束,即岸台施加的控制作用。在平均海平面观察到较大的形态控制,因为大多数平台在涨潮/退潮时都被淹没,因此对近岸环流的控制较少。 (C)2018 Elsevier Ltd.保留所有权利。

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