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首页> 外文期刊>Ocean Engineering >Investigating typhoon-induced storm surge and waves in the coast of Taiwan using an integrally-coupled tide-surge-wave model
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Investigating typhoon-induced storm surge and waves in the coast of Taiwan using an integrally-coupled tide-surge-wave model

机译:使用一体耦合的潮汐浪涌模型来调查台湾海岸的台风引起的风暴浪涌和波浪

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摘要

The coupled tide-surge and wave model was established for the coast of Taiwan and applied to simulate the storm surge during typhoon events. To prove the capability and availability of the coupled model, the model was calibrated and validated with measured water levels, atmospheric pressures, wind speeds, wave heights, and wave periods at different gauge stations under different historical typhoon events. Based on the statistical metrics including the mean absolute error, root mean square error, and skill, the simulated tide-surge, wave height, and wave period using coupled tide-surge-wave model reasonably reproduced the observational data. The parametric typhoon model provided reasonably simulated results compared to the observed atmospheric pressure and wind speed. The validated model was then utilized to explore the impact of waves on the storm surge and the influences of typhoon track, wind stress, and atmospheric pressure on the surge height around the Taiwan coast. The results showed that comparing the simulated water levels using the tide-surge-wave model and the tidesurge model, the averaged differences at Taipei Tamsui, Taichung Harbor, Kaohsiung Harbor, and Hualien Harbor are 0.24 m, 0.23 m, 0.22 m, and 0.22 m, respectively. The wave setup contributes between 6% and 35% to the total storm surge on Taiwan's coast. Furthermore, the typhoon track significantly affects the location of low pressure and the wind direction, subsequently causing the increase/decrease in surge height. The intensity of wind stress and the atmospheric pressure play crucial roles in affecting the water level and dominating the surge height along the coast of Taiwan.
机译:为台湾海岸建立了耦合的潮流和波模型,并应用于在台风活动期间模拟风暴浪涌。为了证明耦合模型的能力和可用性,在不同的历史动脉小风事件下的不同规格站的水平,大气压,风速,波浪高度和波段,校准并验证了模型。基于包括平均绝对误差,根均方误差和技能,模拟潮汐浪涌,波形高度和使用耦合潮汐浪波模型的模拟潮汐浪涌,波形高度合理再现观察数据的统计量度。与观察到的大气压和风速相比,参数台风模型提供了合理的模拟结果。然后利用验证的模型来探讨波浪对风暴浪涌的影响以及台风轨道,风力应力和大气压对台湾海岸浪涌高度的影响。结果表明,将模拟水平与潮汐涌波模型和世卫组织,台北汤苏,台中港,高雄港和花莲港口平均差异进行比较,为0.24米,0.23米,0.22米和0.22 m分别。波浪设置贡献了台湾海岸的风暴总浪涌的6%至35%。此外,台风轨道显着影响低压和风向的位置,随后导致喘振高度的增加/减少。风力应力和大气压力的强度起到影响水位并沿着台湾海岸主导喘振高的作用。

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