2021
DOI: 10.1007/s00162-021-00574-y
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Crossflow effects on shock wave/turbulent boundary layer interactions

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Cited by 14 publications
(9 citation statements)
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References 33 publications
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“…As shown in previous studies (Di Renzo et al. 2022; Larsson et al. 2022), the presence of a non-zero sweep angle yields substantial enlargement of the interaction zone, as compared to the case of two-dimensional, non-swept interactions.…”
Section: Discussionsupporting
confidence: 50%
See 1 more Smart Citation
“…As shown in previous studies (Di Renzo et al. 2022; Larsson et al. 2022), the presence of a non-zero sweep angle yields substantial enlargement of the interaction zone, as compared to the case of two-dimensional, non-swept interactions.…”
Section: Discussionsupporting
confidence: 50%
“…The flow set-up replicates that used in previous studies aimed at establishing the effects of cross-flow on SBLIs (Gross & Fasel 2016; Lee & Gross 2021; Di Renzo et al. 2022; Larsson et al. 2022), as sketched in figure 1.…”
Section: Computational Set-upmentioning
confidence: 99%
“…Using a very large database of experimental and simulation results, these authors catalog unsteady phenomena on the basis of frequency bands and describe qualitative differences between two-dimensional, axisymmetric, open three-dimensional separation in the absence of sidewalls, as well as the effect of the latter on the proposed characterization. Di Renzo, Oberoi, Larsson and Pirozzoli [20] use DNS to address the fundamental problem of shock wave/turbulent boundary layer interaction in the presence of three-dimensionality induced by crossflow. In line with predictions of earlier high-fidelity DNS work [29], these authors find an augmentation of the (mean) size of the separation bubble, associated by changes in the mean flow direction.…”
Section: Summary Of Articles In This Special Issuementioning
confidence: 99%
“…Mainly three types of phenomena have been identified. When the upstream boundary layer is turbulent and the SWBLI weak (incipient separated zone), streaks from the upstream boundary layer and associated with longitudinal vortices can interact with the shock system (Ganapathisubramani et al 2007;Ganapathisubramani, Clemens & Dolling 2009;Di Renzo et al 2022). However, when the SWBLI is strong enough to generate a significant separated zone, the latter can induce a streamline curvature of the boundary layer and initiate a centrifugal Görtler-like instability (Pasquariello, Hickel & Adams 2017;Zhuang et al 2018).…”
Section: Introductionmentioning
confidence: 99%
“…2007; Ganapathisubramani, Clemens & Dolling 2009; Di Renzo et al. 2022). However, when the SWBLI is strong enough to generate a significant separated zone, the latter can induce a streamline curvature of the boundary layer and initiate a centrifugal Görtler-like instability (Pasquariello, Hickel & Adams 2017; Zhuang et al.…”
Section: Introductionmentioning
confidence: 99%