Effect of porosity on an internal solitary wave propagating over a porous trapezoidal obstacle
Effect of porosity on an internal solitary wave propagating over a porous trapezoidal obstacle
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DOI:
10.1016/j.oceaneng.2016.11.067
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发表时间:
2017-01
影响因子:
5
通讯作者:
M. Cheng;C. Hsieh;J. R. Hsu;R. Hwang
中科院分区:
文献类型:
--
作者:
M. Cheng;C. Hsieh;J. R. Hsu;R. Hwang
A permeable seabed may influence the evolution of an internal solitary wave propagating on a continental shelf and nearshore. In order to study the porous effect, numerical simulations are performed to investigate the flow field and waveform inversion of a large depression ISW propagating over a porous trapezoidal obstacle. A finite volume based Cartesian grid method is adopted to solve the Reynolds averaged Navier-Stokes equations using ak-εmodel for the turbulent closure and porous media model together. Numerical results reveal that waveform inversion weakens significantly, as the porosity of the obstacle increases, except when porositynf<0.2. At the same time, the magnitude of vorticity and turbulent energy decrease remarkably due to acute reduction of the production term induced by percolation and wave-pore interaction. Moreover, a skewed hump shaped relation appears between the maximum vorticity and the porosity. For transmitted wave energy on a horizontal plateau, total energy may decrease asnf<0.2 but increases moderately whilenf>0.2 during a strong wave-obstacle interaction.