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One-dimensional modelling of individual waves and wave-induced longshore currents in the surf zone

机译:冲浪区内单个波浪和波浪引起的近岸海流的一维建模

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摘要

A probabilistic model (WAVIS-model) was developed to describe the propagation and transformation of individual waves (wave by wave approach). The individual waves shoal until an empirical criterion for breaking is satisfied. Wave height decay after breaking is modelled by using an energy dissipation method. Wave-induced set-up and set-down and breaking-associated longshore currents are also modelled. Laboratory and field data were used to calibrate and verify the model. The model was calibrated by adjusting the wave breaking coefficient (as a function of local wave steepness and bottom slope) to obtain optimum agreement between measured and computed wave height. Four tests carried out in the large Delta flume of Delft Hydraulics were considered. Generally, the measured H_(1/3)-wave heights are reasonably well represented by the model in all zones from deep water to the shallow surf zone. The fraction of breaking waves was reasonably well represented by the model in the upsloping zones of the bottom profile. Verification of the model results with respect to wave-induced longshore current velocities was not extensive, because of a lack of data. In case of a barred profile the measured longshore velocities showed a relatively uniform distribution in the (trough) zone between the bar crest and the shoreline, which could to some extent be modelled by including space-averaging of the radiation force gradient, horizontal mixing and longshore water surface gradients related to variations in set-up. In case of a monotonically upsloping profile the cross-shore distribution of the longshore current velocities is reasonably well represented.
机译:开发了概率模型(WAVIS模型)来描述单个波的传播和转换(逐波方法)。各个波浪浅滩直到满足破碎的经验标准。通过使用能量耗散方法对破裂后的波高衰减进行建模。还对波浪引起的建立和下沉以及与断裂相关的近岸海流进行了建模。实验室和现场数据用于校准和验证模型。通过调整波浪破碎系数(作为局部波浪陡度和底部坡度的函数)对模型进行校准,以获得测量和计算的波浪高度之间的最佳一致性。考虑了在代尔夫特液压公司的大型Delta水槽中进行的四项测试。通常,模型在从深水到浅海浪的所有区域中都可以很好地表示所测得的H_(1/3)波高度。该模型在底部剖面的上坡带中合理地代表了破碎波的比例。由于缺乏数据,关于波浪引起的近岸海流速度的模型结果的验证并不广泛。在有条状剖面的情况下,测得的近岸速度在条形波峰和海岸线之间的(波谷)区内显示出相对均匀的分布,在一定程度上可以通过对辐射力梯度,水平混合和与设置变化有关的近岸水面梯度。在单调向上倾斜的情况下,合理地表示出了近岸流速的跨岸分布。

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  • 来源
    《Coastal engineering 》 |1996年第4期| p.121-145| 共25页
  • 作者

    L.C. van Rijn; K.M. Wijnberg;

  • 作者单位

    Dept. Phys. Geography, Univ. of Utrecht, P.O. Box. 80115, 3508 TC Utrecht, Netherlands;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 水路运输 ;
  • 关键词

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