Numerical study on frequency downshift of gravity wave spectra in deep and intermediate water depths due to nonlinear energy transfer

Noriaki Hashimoto, Fitri Suciaty, Masaru Yamashiro, Masaki Yokota, Mitsuyoshi Kodama

Research output: Chapter in Book/Report/Conference proceedingConference contribution

2 Citations (Scopus)

Abstract

Frequency downshift of gravity wave spectra in deep and finite water depths due to the nonlinear energy transfer are discussed. In deep water depths, numerical computationes of the nonlinera energy transfer are performed with DIA (Hasselmann et al., 1985), RIAM (Komatsu et al., 1993) and SRIAM (Komatsu et al., 1996). Then, differences in temporal changes of directional spectra computed with a modified WAM implemented with RIAM and SRIAM are compared with those computed with the original WAM implemented with DIA. In finite water depth, numerical computations are performed with a modified WAM implemented with FD-RIAM (Hashimoto, et al., 2002), an exact method, which was upgraded from an earlier version (Hashimoto et al., 1998) based on Komatsu et al., (2001). Differeces in frequency downshift of gravity wave spectra in deep and finite water depths are discussed based on the numerial results for various directional spectra in various water depths.

Original languageEnglish
Title of host publicationProceedings of the 34th International Conference on Coastal Engineering, ICCE 2014
PublisherAmerican Society of Civil Engineers (ASCE)
Volume2014-January
ISBN (Electronic)9780989661126
Publication statusPublished - 2014
Event34th International Conference on Coastal Engineering, ICCE 2014 - Seoul, Korea, Republic of
Duration: Jun 15 2014Jun 20 2014

Other

Other34th International Conference on Coastal Engineering, ICCE 2014
CountryKorea, Republic of
CitySeoul
Period6/15/146/20/14

All Science Journal Classification (ASJC) codes

  • Civil and Structural Engineering
  • Ocean Engineering
  • Oceanography

Fingerprint Dive into the research topics of 'Numerical study on frequency downshift of gravity wave spectra in deep and intermediate water depths due to nonlinear energy transfer'. Together they form a unique fingerprint.

Cite this