2019
DOI: 10.1017/jfm.2019.83
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Compressible unsteady Görtler vortices subject to free-stream vortical disturbances

Abstract: The perturbations triggered by free-stream vortical disturbances in compressible boundary layers developing over concave walls are studied numerically and through asymptotic methods. We employ an asymptotic framework based on the limit of high Görtler number, the scaled parameter defining the centrifugal effects; we use an eigenvalue formulation where the free-stream forcing is neglected; and we solve the receptivity problem by integrating the compressible boundary-region equations complemented by appropriate … Show more

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Cited by 9 publications
(22 citation statements)
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“…In the limits of large Reynolds number R≫1, small perturbations ǫ≪R −1 , and low frequency k x ≪1, the linearized unsteady boundary-region (LUBR) equations for the perturbation flow are recovered by inserting the decomposed q(x, t) into the full compressible Navier-Stokes and continuity equations, using (2.2), and collecting O(ǫ) terms. The LUBR equations are coupled with the initial and boundary conditions derived through asymptotic matching to synthesize the effect of the oncoming free-stream vortical disturbances on the boundary layer (Leib et al 1999;Viaro & Ricco 2019). A second-order implicit finite-difference scheme is employed to solve the LUBR equations (Ricco & Wu 2007), which are parabolic along the streamwise direction.…”
Section: Flow Definition and Scalingmentioning
confidence: 99%
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“…In the limits of large Reynolds number R≫1, small perturbations ǫ≪R −1 , and low frequency k x ≪1, the linearized unsteady boundary-region (LUBR) equations for the perturbation flow are recovered by inserting the decomposed q(x, t) into the full compressible Navier-Stokes and continuity equations, using (2.2), and collecting O(ǫ) terms. The LUBR equations are coupled with the initial and boundary conditions derived through asymptotic matching to synthesize the effect of the oncoming free-stream vortical disturbances on the boundary layer (Leib et al 1999;Viaro & Ricco 2019). A second-order implicit finite-difference scheme is employed to solve the LUBR equations (Ricco & Wu 2007), which are parabolic along the streamwise direction.…”
Section: Flow Definition and Scalingmentioning
confidence: 99%
“…The boundary-layer velocity, pressure and temperature are decomposed into their mean and perturbation as . As in Viaro & Ricco (2019), the mean flow is the compressible Blasius boundary layer without an externally imposed pressure gradient. The Dorodnitsyn–Howarth transformation is used to scale the mean-flow equations in similarity form, for which the independent similarity variable is , where .…”
Section: Mathematical Frameworkmentioning
confidence: 99%
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