Natural Hazards

, Volume 4, Issue 2–3, pp 119–139

The 1987–88 Alaskan Bight tsunamis: Deep ocean data and model comparisons

  • F. I. Gonzalez
  • C. L. Mader
  • M. C. Eble
  • E. N. Bernard
Article

DOI: 10.1007/BF00162783

Cite this article as:
Gonzalez, F.I., Mader, C.L., Eble, M.C. et al. Nat Hazards (1991) 4: 119. doi:10.1007/BF00162783

Abstract

Excellent deep ocean records have been obtained of two tsunamis recently generated in the Alaskan Bight on 30 November 1987 and 6 March 1988, providing the best available data set to date for comparison with tsunami generation/propagation models. Simulations have been performed with SWAN, a nonlinear shallow water numerical model, using source terms estimated by a seafloor deformation model based on the rectangular fault plane formalism. The tsunami waveform obtained from the model is quite sensitive to the specific source assumed. Significant differences were found between the computations and observations of the 30 November 1987 tsunami, suggesting inadequate knowledge of the source characteristics. Fair agreement was found between the data and the model for the first few waves of the 6 March 1988 tsunami. Model estimates of the seismic moment and total slip along the fault plane are also in fair agreement with those derived from the published Harvard centroid solution for the 6 March 1988 event, implying that the computed seafloor deformation does bear some similarity to the actual source.

Key words

Tsunamis ocean measurements model comparisons 

Copyright information

© Kluwer Academic Publishers 1991

Authors and Affiliations

  • F. I. Gonzalez
    • 1
  • C. L. Mader
    • 2
  • M. C. Eble
    • 1
  • E. N. Bernard
    • 1
  1. 1.Pacific Marine Environmental Laboratory, NOAASeattleU.S.A.
  2. 2.Joint Institute for Marine and Atmospheric ResearchHonoluluU.S.A.

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