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Influence of optimally amplified streamwise streaks on the Kelvin–Helmholtz instability

Published online by Cambridge University Press:  17 January 2018

Mathieu Marant
Affiliation:
IMFT, CNRS-INP-UPS, 2 allée du Professeur Camille Soula, 31400 Toulouse, France
Carlo Cossu*
Affiliation:
IMFT, CNRS-INP-UPS, 2 allée du Professeur Camille Soula, 31400 Toulouse, France LHEEA, CNRS – Ecole Centrale de Nantes, 1 rue de la Noé, 44300 Nantes, France
*
†Email address for correspondence: carlo.cossu@imft.fr

Abstract

The optimal energy amplifications of streamwise-uniform and spanwise-periodic perturbations of the hyperbolic-tangent mixing layer are computed and found to be very large, with maximum amplifications increasing with the Reynolds number and with the spanwise wavelength of the perturbations. The optimal initial conditions are streamwise vortices and the most amplified structures are streamwise streaks with sinuous symmetry in the cross-stream plane. The leading suboptimal perturbations have opposite (varicose) symmetry. When forced with finite amplitudes these perturbations modify the characteristics of the Kelvin–Helmholtz instability. Maximum temporal growth rates are reduced by optimal sinuous perturbations and are slightly increased by varicose suboptimal ones. In contrast, the onset of absolute instability is delayed by varicose suboptimal perturbations and is slightly promoted by sinuous optimal ones. We show that if, instead of the computed fully nonlinear basic-flow distortions, the stability analysis is based on a shape assumption for the flow distortions, then opposite effects on the flow stability are predicted in most of the considered cases. These strong differences are attributed to the spanwise-uniform component of the nonlinear basic-flow distortion which, we conclude, should be systematically included in sensitivity analyses of the stability of two-dimensional basic flows to three-dimensional basic-flow perturbations. We finally show that the leading-order quadratic sensitivity of the eigenvalues to the amplitude of the streaks is preserved if the effects of the mean flow distortion are included in the sensitivity analysis.

Information

Type
JFM Papers
Copyright
© 2018 Cambridge University Press 
Figure 0

Figure 1. (a) Optimal energy growth curves $G(t)$ for three selected spanwise wavenumbers for $Re=1000$. (b) Dependence of the rescaled maximum energy growth $G_{max}/Re^{2}$ on the spanwise wavenumber $\unicode[STIX]{x1D6FD}$ for optimal sinuous perturbations (S-type, solid line, violet) and suboptimal varicose perturbations (V-type, dashed line, green). Results obtained at three selected Reynolds numbers are shown to verify the accuracy of the $Re^{2}$ scaling.

Figure 1

Figure 2. Cross-stream view of the optimal (a) and suboptimal (b) streamwise-uniform perturbations of the hyperbolic-tangent 2D reference mixing layer for $Re=1000$ and $\unicode[STIX]{x1D6FD}=2$. The arrows represent the cross-stream velocity components of optimal initial vortices and the contour lines the iso-levels of the streamwise component of the corresponding maximally amplified streak (solid lines correspond to positive levels, dashed lines to negative levels).

Figure 2

Figure 3. Profiles of the hyperbolic-tangent reference basic velocity $U_{2D}(y)$ (a) and of the $\widehat{v}$ component of the optimal initial ($t=0$) vortices (b,d) and of the $\widehat{u}$ component of the corresponding optimally amplified ($t=t_{max}$) streaks (c,e), respectively, corresponding to the optimal sinuous (b,c) and suboptimal varicose (d,e) perturbations for $\unicode[STIX]{x1D6FD}=1$ ($\unicode[STIX]{x1D706}_{z}=6.3$, solid, violet), $\unicode[STIX]{x1D6FD}=2$ ($\unicode[STIX]{x1D706}_{z}=3.1$, dashed, green) and $\unicode[STIX]{x1D6FD}=3$ ($\unicode[STIX]{x1D706}_{z}=2.1$, dotted, dark red) and $Re=1000$.

Figure 3

Figure 4. Dependence of the maximum streak amplitude $A_{s}$ on the amplitude $A_{0}$ of the optimal initial condition for the optimal sinuous (a) and suboptimal varicose (b) perturbations for three selected spanwise wavenumbers at $Re=1000$.

Figure 4

Figure 5. Cross-stream view of the $U_{3D}(y,z)$ iso-contours of the streamwise-uniform streaky basic flows obtained by forcing optimal sinuous perturbations ($A_{s}=14.8\,\%$, a) and suboptimal varicose perturbations ($A_{s}=14.6\,\%$, b) for $Re=1000$ and $\unicode[STIX]{x1D6FD}=2$. Solid (dashed) lines correspond to positive (negative) contours.

Figure 5

Figure 6. Influence of increasing amplitudes of the streaks on the temporal growth rates $\unicode[STIX]{x1D714}_{i}(\unicode[STIX]{x1D6FC})$ for optimal sinuous (a) and suboptimal varicose (b) perturbations for $\unicode[STIX]{x1D6FD}=2$ and $Re=1000$.

Figure 6

Figure 7. Influence of increasing amplitudes of the streaks on the maximum temporal growth rates $\unicode[STIX]{x1D714}_{i,max}$ for optimal sinuous (a) and suboptimal varicose (b) perturbations for selected values of the spanwise wavenumber $\unicode[STIX]{x1D6FD}$ at $Re=1000$.

Figure 7

Figure 8. Influence of increasing amplitudes of the streaks on spatio-temporal growth rates $\unicode[STIX]{x1D70E}(v_{g})$ for optimal sinuous (a) and suboptimal varicose (b) perturbations for $\unicode[STIX]{x1D6FD}=2$ and $Re=1000$. The wave packet’s leading and trailing edge velocities $v_{-}$ and $v_{+}$ are given by the left and right, respectively, velocities for which $\unicode[STIX]{x1D70E}=0$. While the shifts of $v_{-}$ and $v_{+}$ with $A_{s}$ are almost negligible in the sinuous case (a), they clearly consist in a reduction of the absolute value of $v_{-}$ and $v_{+}$ in the varicose case (b).

Figure 8

Figure 9. Influence of increasing amplitudes of the streaks on the critical velocity ratio $R_{t}$ separating the convectively and absolutely unstable regimes for optimal sinuous (a) and suboptimal varicose (b) perturbations for selected values of the spanwise wavenumber $\unicode[STIX]{x1D6FD}$ at $Re=1000$.

Figure 9

Figure 10. Influence of increasing amplitudes of the streaks on the maximum temporal growth rates $\unicode[STIX]{x1D714}_{i,max}(A_{s})$ for optimal sinuous (a–c) and suboptimal varicose (d–f) perturbations for $\unicode[STIX]{x1D6FD}=1$ (a,d), $\unicode[STIX]{x1D6FD}=2$ (b,e), $\unicode[STIX]{x1D6FD}=3$ (c,f) at $Re=1000$. The results pertain to the velocity profiles given by nonlinear simulations (black lines, filled circles), profiles under the shape assumption (magenta lines, crosses), the fictitious $\widetilde{U}$ (red lines, open circles) and $\overline{U}$ (blue lines, open squares) profiles. The predictions of (5.2) are also reported (green lines, $\times$-symbols).

Figure 10

Figure 11. Influence of increasing amplitudes of the streaks on critical velocity ratios $R_{t}(A_{s})$ for the onset of the absolute instability for optimal sinuous (a–c) and suboptimal varicose (d–f) perturbations for $\unicode[STIX]{x1D6FD}=1$ (a,d), $\unicode[STIX]{x1D6FD}=2$ (b,e), $\unicode[STIX]{x1D6FD}=3$ (c,f) at $Re=1000$. Same legends as in figure 10.

Figure 11

Figure 12. Mean flow distortion rescaled by the square of the streaks amplitude $\overline{\unicode[STIX]{x0394}U}(y)/A_{s}^{2}$ corresponding to the forcing of the optimal sinuous (a) and suboptimal varicose (b) streaks with $\unicode[STIX]{x1D6FD}=2$ at $Re=1000$. The profiles obtained for the three amplitudes $A_{s}\approx 5\,\%$, $A_{s}\approx 10\,\%$ and $A_{s}\approx 15\,\%$ are reported in order to appreciate the accuracy of the scaling.