VALENTIN HELLER VALENTIN.HELLER@NOTTINGHAM.AC.UK
Associate Professor
A universal parameter to predict subaerial landslide tsunamis?
Heller, Valentin; Hager, Willi H.
Authors
Willi H. Hager
Abstract
The significance of the impulse product parameter P is reviewed, which is believed to be the most universal parameter for subaerial landslide tsunami (impulse wave) prediction. This semi-empirical parameter is based on the streamwise slide momentum flux component and it was refined with a multiple regression laboratory data analysis. Empirical equations based on P allow for a simple prediction of wave features under diverse conditions (landslides and ice masses, granular and block slides, etc.). Analytical evidence reveals that a mass sliding down a hill slope of angle 51.6° results in the highest waves. The wave height ―observed‖ in the 1958 Lituya Bay case was well predicted using P. Other real-world case studies illustrate how efficient empirical equations based on P deliver wave estimates which support hazard assessment. Future applications are hoped to further confirm the applicability of P to cases with more complex water body geometries and bathymetries.
Keywords: hazard
Citation
Heller, V., & Hager, W. H. (2014). A universal parameter to predict subaerial landslide tsunamis?. Journal of Marine Science and Engineering, 2(2), https://doi.org/10.3390/jmse2020400
Journal Article Type | Article |
---|---|
Acceptance Date | Mar 31, 2014 |
Publication Date | Apr 29, 2014 |
Deposit Date | Jul 26, 2016 |
Publicly Available Date | Jul 26, 2016 |
Journal | Journal of Marine Science and Engineering |
Electronic ISSN | 2077-1312 |
Publisher | MDPI |
Peer Reviewed | Peer Reviewed |
Volume | 2 |
Issue | 2 |
DOI | https://doi.org/10.3390/jmse2020400 |
Keywords | hazard assessment; impulse wave; landslide; landslide tsunami; physical modelling; wave generation |
Public URL | https://nottingham-repository.worktribe.com/output/726442 |
Publisher URL | http://www.mdpi.com/2077-1312/2/2/400 |
Files
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Copyright Statement
Copyright information regarding this work can be found at the following address: http://creativecommons.org/licenses/by/4.0
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