کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4552122 | 1627780 | 2013 | 8 صفحه PDF | دانلود رایگان |

• Energy input, conversion, and radiation increase with the tidal excursion.
• Energy input, conversion, and radiation peak for critical bottom topography.
• The maximum radiation percentage corresponds to the emergence of ISWs.
• Sill slope has opposite effects on barotropic and baroclinic dissipation percentages.
An in-house fully nonlinear, nonhydrostatic numerical model is utilized for simulations of internal solitary waves (ISWs) generated by tidal flows over a Gaussian sill topography. A complete, rigorous theoretical framework is then adopted for the energetics analysis of these ISWs. The ratio of topographic amplitude to the total water depth is fixed, and the tidal excursion parameter (εε) and slope parameter (γγ) are varied by changing the imposed barotropic velocity and the horizontal scale of the topography. It is found that the energy input, conversion, and radiation rates all increase monotonically with εε. They peak when the bottom topography is critical (γ=1γ=1). The energy input is generated by the pressure difference across the domain. The energy conversion rate in percentage (normalized by the corresponding input rate) decreases almost linearly as εε increases. The larger the slope parameter, the higher the conversion percentage. The baroclinic radiation rate in percentage (normalized by the corresponding conversion rate) increases first and then decreases as εε increases. It gets maximum near ε=0.15ε=0.15, which corresponds to the emergence of ISWs in the flow field. The larger the slope parameter, the smaller the radiation percentage. At small εε value when the flow field is in the linear internal tide regime, the conversion and radiation percentages all agree very well with the results in existing literature (Kang and Fringer, 2012) for the Davidson Seamount. The barotropic and baroclinic dissipation percentages behave very differently. While the barotropic one is larger for smaller γγ, the baroclinic one is larger for larger γγ. The present work presents a relatively complete energy budget analysis of ISWs generated by tidal flow over a Gaussian sill topography.
Journal: Ocean Modelling - Volume 68, August 2013, Pages 1–8