Abstract
Turbulent patches occurring in environmental flows can arise from breaking internal waves generated topographically. The convective overturning of waves leads to shear instability and then to turbulence which develops into the fully mixed region in the place of initial wave breaking. The objective of the present studies is to explore the steady internal wave breaking observed in stably stratified flows past obstacles [1]. We use a numerical approach based on well-resolved Navier–Stokes DNS/LES methods using parallel multi-block architecture [2] with the Boussinesq approximation and sponge layer treatment to avoid wave reflection from upstream/downstream boundaries.
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References
Castro IP, Snyder WH (1993) J Fluid Mech 255:195–211
Thomas TG, Williams JJR (1997) J Wind Eng Ind Aero 67&68:155–167
Kasagi N, Nishimura M (1997) Int J Heat Fluid Flow 18:88–99
Castro IP, Snyder WH, Marsh GL (1983) J Fluid Mech 135:261–282
Gheusi F, Stein J, Eiff OF (2000) J Fluid Mech 410:67–99
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Yakovenko, S.N., Thomas, T.G., Castro, I.P. (2010). Internal Wave Breaking in Stratified Flows Past Obstacles. In: Armenio, V., Geurts, B., Fröhlich, J. (eds) Direct and Large-Eddy Simulation VII. ERCOFTAC Series, vol 13. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-3652-0_65
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DOI: https://doi.org/10.1007/978-90-481-3652-0_65
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