Geometry-Based Preliminary Quantification of Landslide-Induced Impulse Wave Attenuation in Mountain Lakes

被引:8
|
作者
Franco, Andrea [1 ]
Schneider-Muntau, Barbara [2 ]
Roberts, Nicholas J. [3 ,4 ]
Clague, John J. [3 ]
Gems, Bernhard [1 ]
机构
[1] Univ Innsbruck, Unit Hydraul Engn, Technikerstr 13, A-6020 Innsbruck, Austria
[2] Univ Innsbruck, Unit Geotech Engn, Technikerstr 13, A-6020 Innsbruck, Austria
[3] Simon Fraser Univ, Dept Earth Sci, 8888 Univ Dr, Burnaby, BC V5A 1S6, Canada
[4] Mineral Resources Tasmania, Dept State Growth, 30 Gordons Hill Rd,Rosny Pk, Rosny Pk, Tas 7018, Australia
来源
APPLIED SCIENCES-BASEL | 2021年 / 11卷 / 24期
关键词
landslide-induced wave; lake-tsunami assessment; mountain lakes; CHEHALIS LAKE; TSUNAMI; FLUID; DYNAMICS; LUCERNE; MODEL;
D O I
10.3390/app112411614
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
In this work, a simple methodology for preliminarily assessing the magnitude of potential landslide-induced impulse waves' attenuation in mountain lakes is presented. A set of metrics is used to define the geometries of theoretical mountain lakes of different sizes and shapes and to simulate impulse waves in them using the hydrodynamic software Flow-3D. The modeling results provide the 'wave decay potential', a ratio between the maximum wave amplitude and the flow depth at the shoreline. Wave decay potential is highly correlated with what is defined as the 'shape product', a metric that represents lake geometry. The relation between these two parameters can be used to evaluate wave dissipation in a natural lake given its geometric properties, and thus estimate expected flow depth at the shoreline. This novel approach is tested by applying it to a real-world event, the 2007 landslide-generated wave in Chehalis Lake (Canada), where the results match well with those obtained using the empirical equation provided by ETH Zurich (2019 Edition). This work represents the initial stage in the development of this method, and it encourages additional research and modeling in which the influence of the impacting characteristics on the resulting waves and flow depths is investigated.
引用
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页数:21
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