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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Evaluation of the numerical wave model (SWAN) for wave simulation in the Black Sea
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Evaluation of the numerical wave model (SWAN) for wave simulation in the Black Sea

机译:评估黑海中波浪模拟的数值波浪模型(SWAN)

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摘要

This study summaries the implementation of the SWAN model forced by the ECMWF ERA Interim dataset reanalyzed 10. m winds over the Black Sea which will be used to study the wind-wave climate and wave energy potential in the region, and its verification. The SWAN model results were compared with directional buoy measurements at three locations along the north and south coasts of the Black Sea, parametric model results based on the JONSWAP growth relations, and the results of previous studies. The SWAN model has been applied in a third generation and non-stationary mode with spherical coordinates. The linear and exponential growth from wind input, depth-induced wave breaking, bottom friction, whitecapping, four-wave (for deep water) and triad-wave (for shallow water) nonlinear interactions have been activated in the simulations. The results of this study indicate that agreement between simulated and observed wave parameters is satisfactory and it is slightly more accurate than the results of the previous studies. However, it still has lower estimates for the maximum values of both wave parameters. These lower estimates are probably due to too low wind speeds in the applied ECMWF wind fields, which is probably caused by orographic effects, and due to the relatively course resolution in time and space of the ECMWF (ERA-Interim) wind fields for the Black Sea.
机译:这项研究总结了由ECMWF ERA临时数据集强制重新实施的SWAN模型的实施,该数据集重新分析了黑海上的10 m风,将用于研究该地区的风浪气候和波能潜力及其验证。将SWAN模型的结果与沿黑海北部和南部海岸的三个位置的定向浮标测量结果,基于JONSWAP增长关系的参数模型结果以及以前的研究结果进行了比较。 SWAN模型已应用于具有球坐标的第三代非平稳模式。在模拟中,已经激活了来自风输入,深度引起的波浪破碎,底部摩擦,白盖,四波(对于深水)和三重波(对于浅水)非线性相互作用的线性和指数增长。这项研究的结果表明,模拟波浪参数和观测波浪参数之间的一致性令人满意,并且比以前的研究结果更准确。但是,对于两个波动参数的最大值,它仍然具有较低的估计值。这些较低的估计值可能是由于所应用的ECMWF风场中的风速太低,这可能是由地形效应引起的,并且是由于Black的ECMWF(ERA-Interim)风场在时间和空间上的相对航向分辨率海。

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