NUMERICAL INVESTIGATIONS OF INFRAGRAVITY WAVE DEVELOPMENT ON A BARRED BEACH

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  • バー型海岸における長周期波発達過程の数値解析
  • バーカタ カイガン ニ オケル チョウ シュウキハ ハッタツ カテイ ノ スウチ カイセキ

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 We constructed a 1-D Boussinesq model to reproduce previously observed infragravity waves developed on a barred beach on Hiratsuka Coast. We applied pressure gradient at sea surface for detection of wave-breaking and introduced numerical viscosity satisfying TVD condition to represent wave attenuation by wave-breaking. This model showed good agreements with both experiments and the observations. Modeled cross-shore distribution of wave spectra suggested development of long standing waves whose amplified frequency components had nodes/antinodes above the bar. We also confirmed gradual infragravity wave development which was inferred from the field observations.The model results suggested that 3rd order nonlinear interacton gives unignorable impacts on the development around the sand bar.

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