Near-field tsunami edge waves and complex earthquake rupture

Pure and Applied Geophysics
By:

Links

Abstract

The effect of distributed coseismic slip on progressive, near-field edge waves is examined for continental shelf tsunamis. Detailed observations of edge waves are difficult to separate from the other tsunami phases that are observed on tide gauge records. In this study, analytic methods are used to compute tsunami edge waves distributed over a finite number of modes and for uniformly sloping bathymetry. Coseismic displacements from static elastic theory are introduced as initial conditions in calculating the evolution of progressive edge-waves. Both simple crack representations (constant stress drop) and stochastic slip models (heterogeneous stress drop) are tested on a fault with geometry similar to that of the M w = 8.8 2010 Chile earthquake. Crack-like ruptures that are beneath or that span the shoreline result in similar longshore patterns of maximum edge-wave amplitude. Ruptures located farther offshore result in reduced edge-wave excitation, consistent with previous studies. Introduction of stress-drop heterogeneity by way of stochastic slip models results in significantly more variability in longshore edge-wave patterns compared to crack-like ruptures for the same offshore source position. In some cases, regions of high slip that are spatially distinct will yield sub-events, in terms of tsunami generation. Constructive interference of both non-trapped and trapped waves can yield significantly larger tsunamis than those that produced by simple earthquake characterizations.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Near-field tsunami edge waves and complex earthquake rupture
Series title Pure and Applied Geophysics
DOI 10.1007/s00024-012-0491-7
Volume 170
Issue 9-10
Year Published 2013
Language English
Publisher Springer
Contributing office(s) Pacific Coastal and Marine Science Center
Description 27 p.
First page 1475
Last page 1491
Online Only (Y/N) N
Additional Online Files (Y/N) N