Skip to main content
Log in

Computation of Tsunamis in the East (Japan) Sea Using Dynamically Interfaced Nested Model

  • Original Paper
  • Published:
pure and applied geophysics Aims and scope Submit manuscript

Abstract

— A study of 1983 and 1993 tsunami events in the East (Japan) Sea using multigrid dynamically-interfaced finite difference models was performed to produce detailed features of coastal inundations along the eastern coast of Korea. The computational domain is composed of several subregions with different grid sizes connected in parallel or inclined directions. The innermost subregion represents the coastal alignment reasonably well and has a grid size of about 30 meters. Numerical simulations have been performed in the framework of shallow-water equations (linear, as well as nonlinear) over the plane or spherical coordinate system, depending on the dimensions of the subregion. Results of simulations show the general agreements with the observed data of the runup height for both tsunamis. The evolution of the distribution function of tsunami heights is studied numerically and it shows a tendency to the log-normal curve for a long distance from the source.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

Author information

Authors and Affiliations

Authors

Additional information

(Received May 26, 2001, accepted January 5, 2002)

Address for correspondence: Professor Byung Ho Choi, E-mail : bhchoi@yurim.skku.ac.kr

Rights and permissions

Reprints and permissions

About this article

Cite this article

Choi, B., Pelinovsky, E., Hong, S. et al. Computation of Tsunamis in the East (Japan) Sea Using Dynamically Interfaced Nested Model. Pure appl. geophys. 160, 1383–1414 (2003). https://doi.org/10.1007/s00024-003-2352-x

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00024-003-2352-x

Navigation