This item is licensed Korea Open Government License
dc.contributor.author
박정현
dc.contributor.author
육진희
dc.contributor.author
주원균
dc.contributor.author
이한수
dc.date.accessioned
2022-01-12T02:30:16Z
dc.date.available
2022-01-12T02:30:16Z
dc.date.issued
2019-09-09
dc.identifier.issn
0749-0208
dc.identifier.uri
https://repository.kisti.re.kr/handle/10580/16243
dc.description.abstract
The accuracy of numerical calculations is highly dependent on the grid spacing, and the smaller the grid spacing the better the accuracy. However, the portion requiring high accuracy often corresponds to only a part of the entire model domain. Setting a small grid interval for the entire model domain to study the calculation region is undesirable from the viewpoint of computation load and computation time. In this study, we illustrate the efficiency of the adaptive mesh refinement method for wave run-up modelling in terms of computational time and accuracy using numerical experiments. In this study, we conducted numerical experiments of wave run-up to verify the efficacy of the Adaptive Mesh Refinement (AMR) method in terms of accuracy and computation load for typhoon Chaba (1618). We determined that wave propagation modelling with storm surge height using the AMR method might be a good alternative to calculated wave run-up height. The difference between the observed and AMR model values for wave run-up height was calculated to be less than 1 m. Compared to the results of non-adaptive experiments with fixed spatial resolutions, those with the AMR method produced highly accurate results, while requiring only 75% of the computation time. The estimation of wave run-up height using AMR is expected to allow the accurate estimation of coastal inundation if more accurate topography and input conditions are given.
dc.language.iso
eng
dc.publisher
Coastal Education and Research Foundation
dc.relation.ispartofseries
Journal of coastal research : JCR;
dc.title
Wave Run-up Modeling with Adaptive Mesh Refinement (AMR) Method in the Busan Marine City during Typhoon Chaba (1618)