4.6 Article

Inundation Characteristics of Solitary Waves According to Revetment Type

期刊

WATER
卷 14, 期 23, 页码 -

出版社

MDPI
DOI: 10.3390/w14233814

关键词

solitary wave; coastal inundation; revetment type; flow separation; vorticity; Navier-Stokes solver; large eddy simulation

资金

  1. National Research Foundation of Korea (NRF) - Korean government (MSIT)
  2. [NRF-2021R1A2C4002665]

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This study investigated the effects of wave absorbers on wave overtopping and inundation characteristics through physical modeling tests and numerical analysis. The results showed that wave absorbing revetments have higher horizontal velocities during wave overtopping, but vertical revetments have higher maximum overtopping water surface elevations. However, the order of maximum inundation heights reverses as the waves propagate inland.
Wave absorbers installed in front of revetments are effective in reducing wave overtopping and inundation caused by periodic waves. The wave absorbers' mechanism of reducing wave overtopping and inundation caused by long-period waves such as tsunamis and storm surges is not clearly understood. This study conducted a physical modeling test and numerical analysis based on a large eddy simulation model using in-house code to examine the characteristics of wave overtopping and inundation according to the revetment type for solitary waves. In a vertical revetment (VR), the dominant vertical velocity of the solitary wave cannot bend at a right angle during overtopping, causing flow separation to occur at the crest, which leads to increased drag and vorticity. In a wave absorbing revetment (WAR), the flow cross-sectional area decreases along the slope of the wave absorber, causing the flow velocity of the solitary wave to increase and the horizontal velocity to be dominant during the overtopping and inundation process. In contrast with the general wave overtopping characteristics of periodic waves, the maximum overtopping water surface elevation in front of the vertical wall is higher in a VR than in a WAR. However, the order of maximum inundation heights reverses as the wave propagates inland.

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