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印度西海岸马卡兰俯冲带至卡纳塔克邦海岸的概率海啸灾害评估

The probabilistic tsunami hazard assessment along Karnataka Coast from Makran Subduction Zone, west coast of India.

机构信息

Department of Marine Geology, Mangalore University, Mangalore, Karnataka, 574 199, India.

Indian National Centre for Ocean Information Services, Hyderabad, India.

出版信息

Environ Monit Assess. 2018 Oct 27;190(11):679. doi: 10.1007/s10661-018-7048-x.

Abstract

Coastal tsunami amplitudes were calculated to identify areas susceptible to tsunami hazard at selected locations of the coast of Karnataka, west of India, due to earthquakes in the Makran Subduction Zone. This is the first time that the probabilistic tsunami hazard assessment along this study area has been attempted. A series of earthquake source scenarios with magnitudes of Mw 8.0, Mw 8.5, and a mega thrust of Mw 9.1 were modeled by using the Community Model Interface for Tsunami interface with the MOST model of Titov and Synolakis (J. Waterway, Port, Coastal and Ocean Engineering, 121(6), 308-316, 1995). As per the previous occurrences, the two least magnitudes are probable, while Mw 9.1 is a worst-case scenario as described by Heidarzadeh et al. (Ocean Engineering, 36(5), 368-376, 2009) and the same is reported by Burbidge et al. (Geoscience Australia Professional Opinion No. 2009/11) as high magnitude. These are not at all historical earthquakes or specifically from historical catalogues. The results of modeling show that all the seven coastal locations are inundated barely in our worst-case scenario with maximum water levels in the range of 100-200 cm. The first tsunami wave strikes the coast within 4-5 h of earthquake occurrence.

摘要

计算了沿海海啸的振幅,以确定印度西部卡纳塔克邦沿海选定地点因马尔卡兰俯冲带地震而容易受到海啸灾害的区域。这是首次尝试对该研究区域进行概率海啸灾害评估。使用社区模型接口海啸接口和 Titov 和 Synolakis 的 MOST 模型模拟了一系列震级为 Mw8.0、Mw8.5 和 Mw9.1 的mega thrust 地震源情景(J. Waterway,Port,Coastal and Ocean Engineering,121(6),308-316,1995)。根据以往的情况,最有可能发生的是前两个较小的震级,而 Mw9.1 是 Heidarzadeh 等人(Ocean Engineering,36(5),368-376,2009)描述的最坏情况情景,Burbidge 等人(Geoscience Australia Professional Opinion No. 2009/11)也报告称该震级很高。这些都不是历史地震或专门从历史目录中获得的。建模结果表明,在我们的最坏情况下,所有七个沿海地点都被淹没,最高水位在 100-200cm 之间。第一次海啸波在地震发生后 4-5 小时内袭击海岸。

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