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首页> 外文期刊>Nature Communications >Destructive tsunami-like wave generated by surf beat over a coral reef during Typhoon Haiyan
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Destructive tsunami-like wave generated by surf beat over a coral reef during Typhoon Haiyan

机译:在海燕台风中,海浪拍打珊瑚礁时产生的破坏性海啸状波

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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,我们可以看到,在台风海盐期间,菲律宾海尔尼礁受边缘珊瑚礁保护的城镇附近的海浪破裂,形成了这种波浪,并随大,小波浪群的发生而振荡,并陡峭成类似海啸的波浪,造成了大范围海浪。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,但在发生强力海浪时,它们会加剧洪水泛滥。对于礁石型测深仪而言,典型的是,陡峭礁石面上的非常短的波浪破碎带有利于释放无重力周期波动(冲浪),而能量损失很小。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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