Focusing of long waves with finite crest over constant depth


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KANOĞLU U., Titov V. V. , Aydin B., Moore C., Stefanakis T. S. , Zhou H., ...More

PROCEEDINGS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, vol.469, no.2153, 2013 (Peer-Reviewed Journal) identifier identifier

  • Publication Type: Article / Article
  • Volume: 469 Issue: 2153
  • Publication Date: 2013
  • Doi Number: 10.1098/rspa.2013.0015
  • Journal Name: PROCEEDINGS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES
  • Journal Indexes: Science Citation Index Expanded, Scopus
  • Keywords: shallow-water wave equations, finite crest length tsunami, tsunami directivity, tsunami focusing, tsunami run-up, tsunami, SOLITARY WAVES, FIELD TSUNAMIS, RUN-UP, PROPAGATION, AMPLITUDE, EVOLUTION, BEACHES, MODELS

Abstract

Tsunamis are long waves that evolve substantially, through spatial and temporal spreading from their source region. Here, we introduce a new analytical solution to study the propagation of a finite strip source over constant depth using linear shallow-water wave theory. This solution is not only exact, but also general and allows the use of realistic initial waveforms such as N-waves. We show the existence of focusing points for N-wave-type initial displacements, i.e. points where unexpectedly large wave heights may be observed. We explain the effect of focusing from a strip source analytically, and explore it numerically. We observe focusing points using linear non-dispersive and linear dispersive theories, analytically; and nonlinear non-dispersive and weakly nonlinear weakly dispersive theories, numerically. We discuss geophysical implications of our solutions using the 17 July 1998 Papua New Guinea and the 17 July 2006 Java tsunamis as examples. Our results may also help to explain high run-up values observed during the 11 March 2011 Japan tsunami, which are otherwise not consistent with existing scaling relationships. We conclude that N-waves generated by tectonic displacements feature focusing points, which may significantly amplify run-up beyond what is often assumed from widely used scaling relationships.