scholarly journals PIV applied to landslide generated impulse waves

Author(s):  
H. M. Fritz
Keyword(s):  
2021 ◽  
Vol 18 (5) ◽  
pp. 1159-1176
Author(s):  
Ting Cao ◽  
Ping-yi Wang ◽  
Zhen-feng Qiu ◽  
Jing-xuan Ren
Keyword(s):  

2021 ◽  
Vol 595 ◽  
pp. 126012
Author(s):  
Xiaoliang Wang ◽  
Chuanqi Shi ◽  
Qingquan Liu ◽  
Yi An

2020 ◽  
Vol 359 ◽  
pp. 112750 ◽  
Author(s):  
Jia Mao ◽  
Lanhao Zhao ◽  
Yingtang Di ◽  
Xunnan Liu ◽  
Weiya Xu
Keyword(s):  

Author(s):  
Frederic M Evers ◽  
Willi H Hager

Large subaerial mass wasting into water may generate large waves along coast lines and in bays. Hazard assessment of such an events is based on the decay rate of these impulse waves along their propagation path to populated areas and infrastructure along the shoreline. The spatial propagation processes of impulse waves generated by deformable slides was investigated in a wave basin. A videometric measurement approach allowed for a detailed tracking of the free water surface and key wave characteristics during the experimental runs including the wave height. Based on selected tests, the slide width effect on spatial wave propagation is discussed.


Landslides ◽  
2018 ◽  
Vol 15 (12) ◽  
pp. 2385-2398 ◽  
Author(s):  
Lili Xiao ◽  
Jiajia Wang ◽  
Steven N Ward ◽  
Lixia Chen

2015 ◽  
Vol 9 (6) ◽  
pp. 6471-6493 ◽  
Author(s):  
M. P. Lüthi ◽  
A. Vieli

Abstract. Glacier calving can cause violent impulse waves which, upon landfall, can lead to destructive tsunami-like waves. Here we present data acquired during a calving event from Eqip Sermia, an ocean-terminating glacier in West Greenland. During an exceptionally well documented event, the collapse of 9 × 105 m3 ice from a 200 m high ice cliff caused an impulse wave of 50 m height, traveling at a speed of 25–30 m s-1. This wave was filmed from a tour boat in 800 m distance from the calving face, and simultaneously measured with a terrestrial radar interferometer and a tide gauge. Tsunami wave run-up height on the steep opposite shore in 4 km distance was 10–15 m, destroying infrastructure and eroding old vegetation. These observations indicate that such high tsunami waves are a recent phenomenon in the history of this glacier. Analysis of the data shows that only moderately bigger tsunami waves are to be expected in the future, even under rather extreme scenarios.


2018 ◽  
Vol 19 (1) ◽  
pp. 203-230 ◽  
Author(s):  
Hongcheng Xue ◽  
Qian Ma ◽  
Mingjun Diao ◽  
Lei Jiang

2007 ◽  
Vol 44 (5) ◽  
pp. 691-703 ◽  
Author(s):  
Valentin Heller ◽  
Willi H. Hager ◽  
Hans-Erwin Minor

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