风暴波对淹没特征影响的实例研究

Yoshimitsu Tajima
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引用次数: 5

摘要

模拟风暴波和风暴潮的相互作用特征可能是一个重要但具有挑战性的任务,以更准确地估计严重风暴下的海岸灾害。本文通过对近期沿海灾害的几个案例研究的概述,讨论了风暴波和波浪与风暴潮的相互作用如何影响局部淹没特征的放大。本文首先描述了超强台风海燕在菲律宾圣佩德罗湾沿岸和东萨马岛东海岸造成的目击淹没特征。在圣佩德罗湾西海岸,无论是风暴潮预报还是风暴波预报都不能很好地反映以下观测特征:圣佩德罗湾口周围的淹没开始于湾内发生淹没的时间前1小时左右,在湾口附近的水位达到峰值后迅速下降,而湾内的水位则保持在一个小时的高位。在东萨马岛东海岸,风浪分量的变形强烈依赖于边缘珊瑚礁的水深测量,折射、衍射和波-波相互作用对观测到的局部变化的破坏程度和淹没特征有显著影响。超级台风莫兰蒂从菲律宾巴丹岛北部经过时,该岛西海岸也出现了类似的局部集中淹没。2007年台风菲特(Fitow)袭击日本太平洋沿岸的Seisho沿岸灾害也观察到次重力波对局地集中淹没特征的显著影响。在此基础上,本文最后讨论了数值模型应如何扩展以更好地估计海岸灾害,并以模型在南太平洋岛屿的应用为例。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Case study on impact of storm waves on inundation characteristics

Modeling interactive features of storm waves and surges may be one of important but challenging tasks toward more accurate estimations of coastal hazards under severe storms. This paper discusses how storm waves and interactions of waves and surges affect amplification of local inundation characteristics through overviews of several case studies of recent coastal disasters. The paper first describes witnessed inundation characteristics caused by Super Typhoon Haiyan along the coast of San Pedro Bay and also the east coast of Eastern Samar in the Philippines. Along the west coast of San Pedro Bay, neither predicted storm surge nor storm wave can reasonably represent the following observed features: inundation around the mouth of San Pedro Bay started about an hour prior to the time when the inundation was witnessed at the inner part of the bay and the water level quickly descended after the peak around the bay mouth while it was kept high for an hour in the inner part of the bay. Along the east coast of Eastern Samar, deformation of wind wave components strongly depends on bathymetry of fringing coral reefs and refraction, diffraction and wave-wave interactions appear to have significant influence on observed locally varying damage levels and inundation characteristics. Similar locally concentrated inundation was also observed along the west coast of Batan island, the Philippines when the super typhoon Meranti passed north of the island. Significant influence of infra-gravity waves on the locally concentrated inundation characteristics was also observed in the disaster along Seisho coast on the Pacific coast of Japan when the typhoon, Fitow, hit the coast in 2007. Based on these findings, finally, this paper discusses how the numerical model should be extended for better estimations of coastal hazard with brief example of model application to South Pacific islands.

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