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Keywords
(13)
Boundary Layer
Environmental Conditions
Exact Solution
Friction Coefficient
Internal Waves
korteweg de vries equation
Model Validation
Numerical Simulation
Reynolds Number
Solitary Wave
Stratification
Benthic Boundary Layer
reynolds average navier stokes
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The wave-induced boundary layer under long internal waves
The wave-induced boundary layer under long internal waves,10.1007/s10236-011-0413-8,Ocean Dynamics,Yuncheng Lin,Larry G. Redekopp
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The wave-induced boundary layer under long internal waves
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Yuncheng Lin
,
Larry G. Redekopp
The
boundary layer
formed under the footprint of an internal
solitary wave
is studied by
numerical simulation
for waves of depression in a two-layer model of the density stratification. The inviscid outer flow, in the perspective of boundary-layer theory, is based on an
exact solution
for the long wave-phase speed, yielding a family of fully nonlinear
solitary wave
solutions of the extended Korteweg–de Vries equation. The wave-induced
boundary layer
corresponding to this outer flow is then studied by means of simulation employing the Reynolds-averaged Navier–Stokes (RANS) formulation coupled with a turbulence closure model validated for wall-bounded flows. Boundary-layer characteristics are computed for an extensive range of
environmental conditions
and wave amplitudes. Boundary-layer transition, identified by monitoring the eddy viscosity, is correlated in terms of a boundary-layer Reynolds number. The frictional drag is evaluated for laminar, transitional, and turbulent cases, and correlations are presented for the
friction coefficient
plus relevant measures of the boundary-layer thickness.
Journal:
Ocean Dynamics - OCEAN DYN
, vol. 61, no. 8, pp. 1045-1065, 2011
DOI:
10.1007/s10236-011-0413-8
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References
(13)
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