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Impact of ocean-wave coupling on typhoon-induced waves and surge levels around the Korean Peninsula: a case study of Typhoon Bolaven

机译:海浪耦合对朝鲜半岛台风诱发的海浪和潮汐水平的影响:以台风“波拉文”为例

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摘要

Typhoon-induced waves and surges are important when predicting potential hazards near coastal regions. In this paper, we applied a coupled modeling system for ocean-wave interaction to examine prediction capabilities for typhoon-induced waves and surges around the Korean Peninsula. To identify how ocean-wave coupling impacts wave and surge simulations during typhoon conditions, a set of comparative experiments was performed during Typhoon Bolaven (2012): (1) a fully coupled ocean-wave model, (2) a one-way coupled ocean-wave model without surface current feedback and ocean-to-wave water levels, and (3) a stand-alone ocean model without considering wave-based sea surface roughness (SSR). When coupled with the ocean model, the surface current reduced significantly the wave height on the right-hand side of the advancing typhoon track and improved prediction accuracy along the southern coast of Korea. Compared with the observed surge levels, the simulated surge height yielded improved results for peak height magnitude and timing compared with the uncoupled model. For wave-to-surge feedback, we found that wave-induced SSR plays an important role by modulating wind stress in the surface layer. The modulated wind stress directly affected the surge height, which improved surge peak prediction during the typhoon.
机译:在预测沿海地区附近的潜在危害时,台风引起的海浪和海浪很重要。在本文中,我们为海浪相互作用应用了耦合建模系统,以检查台风诱发的朝鲜半岛周围海浪和海浪的预测能力。为了确定海浪耦合如何影响台风条件下的波浪和浪涌模拟,在台风玻尔文(2012)期间进行了一系列比较实验:(1)完全耦合的海浪模型,(2)单向耦合的海洋没有地表电流反馈和海浪水位的波浪模型,以及(3)不考虑基于波浪的海面粗糙度(SSR)的独立海洋模型。当与海洋模型结合使用时,地表水流显着降低了前进台风轨道右侧的波高,并提高了韩国南部海岸的预测精度。与观察到的喘振水平相比,与未耦合模型相比,模拟的喘振高度在峰高大小和时间方面产生了改进的结果。对于波到浪涌反馈,我们发现波诱发的SSR通过调节表层的风应力起着重要作用。调制的风应力直接影响浪涌高度,从而改善了台风期间的浪涌峰值预测。

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