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  Random focusing of tsunami waves.

Degueldre, H., Metzger, J. J., Geisel, T., & Fleischmann, R. (2016). Random focusing of tsunami waves. Nature Physics, 12(3), 259-262. doi:10.1038/nphys3557.

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Item Permalink: http://hdl.handle.net/11858/00-001M-0000-0029-A8A1-D Version Permalink: http://hdl.handle.net/11858/00-001M-0000-002D-41EB-F
Genre: Journal Article

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 Creators:
Degueldre, Henri1, Author              
Metzger, Jakob J.1, Author              
Geisel, Theo1, Author              
Fleischmann, Ragnar1, Author              
Affiliations:
1Department of Nonlinear Dynamics, Max Planck Institute for Dynamics and Self-Organization, Max Planck Society, DE, ou_2063286              

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 Abstract: Tsunamis exhibit surprisingly strong height fluctuations. An in-depth understanding of the mechanisms that lead to these variations in wave height is a prerequisite for reliable tsunami forecasting. It is known, for example, that the presence of large underwater islands1 or the shape of the tsunami source2 can affect the wave heights. Here we show that the consecutive effect of even tiny fluctuations in the profile of the ocean floor (the bathymetry) can cause unexpectedly strong fluctuations in the wave height of tsunamis, with maxima several times higher than the average wave height. A novel approach combining stochastic caustic theory and shallow water wave dynamics allows us to determine the typical propagation distance at which the strongly focused waves appear. We demonstrate that owing to this mechanism the small errors present in bathymetry measurements can lead to drastic variations in predicted tsunami heights. Our results show that a precise knowledge of the ocean’s bathymetry is absolutely indispensable for reliable tsunami forecasts.

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Language(s): eng - English
 Dates: 2015-11-232016-03
 Publication Status: Published in print
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 Table of Contents: -
 Rev. Method: Peer
 Identifiers: DOI: 10.1038/nphys3557
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Title: Nature Physics
Source Genre: Journal
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Pages: - Volume / Issue: 12 (3) Sequence Number: - Start / End Page: 259 - 262 Identifier: -