波罗的海爱沙尼亚海岸的大风浪上升

A. Rodin, I. Didenkuolova, I. Nikolkina
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引用次数: 1

摘要

用WAM模式对有冰条件下COSMO风强迫的35年风浪模拟进行了波罗的海爱沙尼亚海岸最大淹没分析。在爱沙尼亚波罗的海沿岸所选的18个海滩剖面中,每一个都找到了最大有效波高和相应的周期。可取得海浪资料的地点位于水深约10至20米,距离海岸达8公里。这些波浪在爱沙尼亚海滩上的上升是使用CLAWPACK软件包(www.clawpack.org)根据浅水理论计算的。海滩的地形取自地质实地调查,并在需要时与GEBCO地图相结合。我们考虑了相应波高和周期的单色波向海岸逼近的情况。为此,我们采用了近海造波器产生规则波的边界条件。所有波浪上升计算的时间步长和空间步长保持不变,分别为1 m和1 s。将最大助跑的估计与文献中使用不同助跑公式的估计进行了比较。
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Run-up of large storm waves on Estonian coasts of the Baltic Sea
Analysis of maximal inundation of Estonian coasts of the Baltic Sea is conducted on 35-year wind wave simulations with WAM model forced by COSMO winds in the presence of ice. For each of selected along the Estonian Baltic Sea coast 18 beach profiles, the maximal significant wave heights and corresponding periods are found. The locations with available wave data are located at the water depth of about 10 to 20 m and at a distance up to 8 km from the shore. Run-up of these waves on Estonian beaches is calculated within the shallow water theory using the CLAWPACK software package (www.clawpack.org). The topography of the beach is taken from Geological field surveys and combined with GEBCO maps, where needed. We consider the case, when monochromatic waves of corresponding wave height and period are approaching the coast. For this we use boundary conditions of wave-maker located offshore and generating regular waves. Time and space step during all calculations of wave run-up remains constant (1 m and 1 s respectively). The estimates of maximal run-up are compared with the estimations made using different run-up formulas, available in the literature.
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