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Tsunami generation by ocean floor rupture front propagation: Hamiltonian description

Pavlov, V. I. and Tromp, J. and Tito, E. P. (2009) Tsunami generation by ocean floor rupture front propagation: Hamiltonian description. Natural Hazards and Earth System Sciences, 9 (1). pp. 217-227. ISSN 1561-8633 http://resolver.caltech.edu/CaltechAUTHORS:20090416-145234099

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Abstract

The Hamiltonian method is applied to the problem of tsunami generation caused by a propagating rupture front and deformation of the ocean floor. The method establishes an alternative framework for analyzing the tsunami generation process and produces analytical expressions for the power and directivity of tsunami radiation (in the far-field) for two illustrative cases, with constant and gradually varying speeds of rupture front propagation.


Item Type:Article
Additional Information:© Author(s) 2009. Received: 18 July 2008 – Revised: 16 January 2009 – Accepted: 16 January 2009 – Published: 23 February 2009. Edited by: S. Tinti. Reviewed by: two anonymous referees.
Record Number:CaltechAUTHORS:20090416-145234099
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20090416-145234099
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Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:14004
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:17 Apr 2009 16:30
Last Modified:26 Dec 2012 10:57

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