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Destructive tsunami-like wave generated by surf beat over a coral reef during Typhoon Haiyan

机译:海燕台风席卷海浪拍打珊瑚礁时产生的破坏性海啸状波

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摘要

Storm surges cause coastal inundation due to setup of the water surface resulting from atmospheric pressure, surface winds and breaking waves. Here we show that during Typhoon Haiyan, the setup generated by breaking waves near the fringing-reef-protected town of Hernani, the Philippines, oscillated with the incidence of large and small wave groups, and steepened into a tsunami-like wave that caused extensive damage and casualties. Though fringing reefs usually protect coastal communities from moderate storms, they can exacerbate flooding during strong events with energetic waves. Typical for reef-type bathymetries, a very short wave-breaking zone over the steep reef face facilitates the freeing of infragravity-period fluctuations (surf beat) with little energy loss. Since coastal flood planning relies on phase-averaged wave modelling, infragravity surges are not being accounted for. This highlights the necessity for a policy change and the adoption of phase-resolving wave models for hazard assessment in regions with fringing reefs.
机译:由于大气压,地表风和碎波引起的水面形成,风暴潮导致沿海淹没。在这里,我们表明,在台风海盐期间,菲律宾边缘礁保护的城镇埃尔纳尼附近的海浪破裂产生的装置,随大,小波浪群的发生而振荡,并变陡成海啸状的海浪,引起了广泛的海浪。损害和人员伤亡。尽管边缘礁通常可以保护沿海社区免受中度风暴的侵袭,但在发生强烈事件时,它们可能会加剧高潮,洪水泛滥。对于礁石型测深仪而言,典型的做法是,在陡峭的礁石面上非常短的波浪破碎区有助于在无能量损失的情况下释放出重力下的周期波动(海浪拍打)。由于沿海洪水规划依赖于相位平均波模拟,因此不考虑次重力浪潮。这凸显了在边缘珊瑚礁地区进行政策变更和采用阶段解析波浪模型进行危害评估的必要性。

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