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首页> 外文期刊>Brazilian Journal of Oceanography >Wave run-up on embayed beaches. Study case: Itapocor?3i Bay, Southern Brazil
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Wave run-up on embayed beaches. Study case: Itapocor?3i Bay, Southern Brazil

机译:波涛汹涌的海滩上。研究案例:巴西南部Itapocor?3i湾

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This paper presents a new approach for estimating run-up on embayed beaches based on a study of the microtidal coast of Itapocor?3i Bay, Southern Brazil using the surf similarity parameter and wave height at break location. The four step methodology involved: 1) direct wave measurement (34 days), wave run-up measurement (19 days at 7 points within the bay), measurement of bathymetry and beach topography in the entire bay; 2) tests on available formulae to calculate wave run-up; 3) use of the SWAN spectral wave model to simulate wave parameters at breaking at each wave run-up measurement point and; 4) development of a new formula/approach to assess wave run-up on embayed beaches (in both exposed and protected areas). During the experiments the significant wave height varied from 0.5 m to 3.01 m, the mean wave period from 2.79 s to 7.76 s (the peak period varied between 2.95 s and 17.18 s), the mean wave direction from 72.5?° to 141.9?° (the peak direction varied from 39.2?° to 169.8?°) and the beach slope (tan ?2) from 0.041 to 0.201. The proposed formula is in good agreement with measured data for different wave conditions and varying degrees of protection. The analysis demonstrates that although R?2 varies from 0.52 to 0.75, the wave run-up distribution over the measurements agreed well with the proposed model, as shown by quantile-quantile analysis (R?2=0.98 to 0.99). The errors observed in individual cases may be related to errors of measurements, modeling and to non-linear processes in the swash zone, such as infragavity waves.
机译:本文基于对巴西南部Itapocor?3i湾微潮海岸的研究,基于冲浪相似性参数和断裂位置处的波高,提出了一种估算套叠海滩上升的新方法。包括四个步骤的方法:1)直接波浪测量(34天),波浪上升测量(在海湾内7个点的19天),整个海湾的测深和海滩地形测量; 2)测试可用公式以计算波浪起伏; 3)使用SWAN频谱波模型来模拟每个波上升测量点处的断裂波参数,以及4)制定新的公式/方法,以评估隐蔽海滩(裸露和保护区)的波浪上升。在实验过程中,有效波高从0.5 m到3.01 m,平均波周期从2.79 s到7.76 s(峰值周期在2.95 s和17.18 s之间变化),平均波向从72.5?°到141.9?° (峰值方向从39.2°变化到169.8°),海滩倾斜度(tan?2)从0.041变化到0.201。所提出的公式与针对不同波浪条件和不同防护等级的测量数据非常吻合。分析表明,尽管R?2在0.52至0.75之间变化,但分位数分位数分析显示,测量范围内的波上升分布与所提出的模型吻合得很好(R?2 = 0.98至0.99)。在个别情况下观察到的误差可能与测量误差,建模误差以及旋转斜带中的非线性过程(例如,过流波)有关。

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