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Ocean surface waves in Hurricane Ike (2008) and Superstorm Sandy (2012): Coupled model predictions and observations

机译:飓风艾克(2008)和超级风暴桑迪(2012)中的海面波:耦合模型预测和观测

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摘要

Forecasting hurricane impacts of extreme winds and flooding requires accurate prediction of hurricane structure and storm-induced ocean surface waves days in advance. The waves are complex, especially near landfall when the hurricane winds and water depth varies significantly and the surface waves refract, shoal and dissipate. In this study, we examine the spatial structure, magnitude, and directional spectrum of hurricane-induced ocean waves using a high resolution, fully coupled atmosphere-wave-ocean model and observations. The coupled model predictions of ocean surface waves in Hurricane Ike (2008) over the Gulf of Mexico and Superstorm Sandy (2012) in the northeastern Atlantic and coastal region are evaluated with the NDBC buoy and satellite altimeter observations. Although there are characteristics that are general to ocean waves in both hurricanes as documented in previous studies, wave fields in Ike and Sandy possess unique properties due mostly to the distinct wind fields and coastal bathymetry in the two storms. Several processes are found to significantly modulate hurricane surface waves near landfall. First, the phase speed and group velocities decrease as the waves become shorter and steeper in shallow water, effectively increasing surface roughness and wind stress. Second, the bottom-induced refraction acts to turn the waves toward the coast, increasing the misalignment between the wind and waves. Third, as the hurricane translates over land, the left side of the storm center is characterized by offshore winds over very short fetch, which opposes incoming swell. Landfalling hurricanes produce broader wave spectra overall than that of the open ocean. The front-left quadrant is most complex, where the combination of windsea, swell propagating against the wind, increasing wind-wave stress, and interaction with the coastal topography requires a fully coupled model to meet these challenges in hurricane wave and surge prediction. (C) 2015 Published by Elsevier Ltd.
机译:预测极端风和洪水的飓风影响需要提前几天准确预测飓风结构和风暴引起的海面波。波浪是复杂的,特别是在飓风和水深变化很大且地表波折射,浅滩和消散时靠近登陆处。在这项研究中,我们使用高分辨率,完全耦合的大气波海洋模型和观测资料检查了飓风诱发的海浪的空间结构,强度和方向谱。利用NDBC浮标和卫星高度计观测结果,评估了墨西哥湾飓风艾克(2008)和东北大西洋及沿海地区的超级风暴桑迪(2012)的海面波耦合模型预测。尽管如先前研究中所述,两种飓风都有海浪的共同特征,但艾克和桑迪的海浪场具有独特的性质,这主要是由于两次风暴中独特的风场和沿海测深。发现有几种过程可以显着地调节登陆附近的飓风表面波。首先,随着波浪在浅水中变短和变陡,相速度和群速度降低,从而有效地增加了表面粗糙度和风应力。其次,由底部引起的折射作用将海浪转向海岸,从而增加了风浪之间的失准。第三,飓风在陆地上空移动时,风暴中心的左侧的特征是海上风在很短的时间内就抵御了涌入的涌浪。登陆飓风产生的波谱总体上比公海要宽。左前象限最复杂,在这里,风浪,逆风传播的浪涌,增加的风浪应力以及与沿海地形的相互作用的组合需要完全耦合的模型来应对飓风和潮汐预报中的这些挑战。 (C)2015由Elsevier Ltd.出版

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