Turbulence during the generation of internal tide on a critical slope
Three-dimensional direct numerical simulations are performed to examine nonlinear processes during the generation of internal tides on a model continental slope. An intense boundary flow is generated in the critical case where the slope angle is equal to
|Collections||ANU Research Publications|
|Source:||Physical Review Letters|
|01_Gayen_Turbulence_during_the_2010.pdf||1.29 MB||Adobe PDF||Request a copy|
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