Skip to main content
Log in

Fourier analysis of the roll-up and merging of coherent structures in shallow mixing layers

  • Original Article
  • Published:
Environmental Fluid Mechanics Aims and scope Submit manuscript

Abstract

The current study investigates the role of nonlinearity in the development of two-dimensional coherent structures (2DCS) in shallow mixing layers. A nonlinear numerical model based on the depth-averaged shallow water equations is used to investigate temporal shallow mixing layers, where the mapping from temporal to spatial results is made using the velocity at the center of the mixing layer. The flow is periodic in the stream-wise direction and the transmissive boundary conditions are used in the cross-stream boundaries to prevent reflections. The numerical results are examined with the aid of Fourier decomposition. Results show that the previous success in applying local linear theory to shallow mixing layers does not imply that the flow is truly linear. Linear stability theory is confirmed to be only valid within a short distance from the inflow boundary. Downstream of this linear region, nonlinearity becomes important for the roll-up and merging of 2DCS. While the energy required for the merging of 2DCS is still largely provided by the velocity shear, the merging mechanism is one where nonlinear mode interaction changes the velocity field of the subharmonic mode and the gradient of the along-stream velocity profile which, in turn, changes the magnitude of the energy production of the subharmonic mode by the velocity shear implicitly. The nonlinear mode interaction is associated with energy up-scaling and is consistent with the inverse energy cascade which is expected to occur in shallow shear flows. Current results also show that such implicit nonlinear interaction is sensitive to the phase angle difference between the most unstable mode and its subharmonic. The bed friction effect on the 2DCS is relatively small initially and grows in tandem with the size of the 2DCS. The bed friction also causes a decrease in the velocity gradient as the flow develops downstream. The transition from unstable to stable flow occurs when the bed friction balances the energy production. Beyond this point, the bed friction is more dominant and the 2DCS are progressively damped and eventually get annihilated. The energy production by the velocity shear plays an important role from the upstream end all the way to the point of transition to stable flow. The fact that linear stability theory is valid only for a short distance from the inflow boundary suggests that some elements of nonlinearity is incorporated in the mean velocity profile in experiments by the averaging process. The implicit nature of nonlinear interaction in shallow mixing layers and the sensitivity of the nonlinear interaction to phase angle difference between the most unstable mode and its subharmonic allows local linear theory to be successful in reproducing features of the instability such as the dominant mode of the 2DCS and its amplitude.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13

Similar content being viewed by others

References

  1. Jirka (2001) Large scale flow structures and mixing processes in shallow flows. J Hydraul Res 39(6):567–573

    Article  Google Scholar 

  2. Chu VH, Babarutsi S (1988) Confinement and bed-friction effects in shallow turbulent mixing layers. J Hydraul Eng 114(10):1257–1274

    Article  Google Scholar 

  3. Rhoads BL, Sukhodolov AN (2004) Spatial and temporal structure of shear layer turbulence at a stream confluence. Water Resour Res 40:W06304

    Article  Google Scholar 

  4. van Prooijen BC, Uijttewaal WSJ (2009) The relevance of a backscatter model for depth-averaged flow simulation. Flow Turbul Combust 82(1):73–91

    Article  Google Scholar 

  5. Jirka GH, Seol DG (2010) Dynamics of isolated vortices in shallow flows. J Hydro-Environ Res 4:65–73

    Article  Google Scholar 

  6. Constantinescu G (2014) LES of shallow mixing interfaces: a review. Environ Fluid Mech 14(2):295–317

    Article  Google Scholar 

  7. Constantinescu G, Miyawaki S, Rhoads B, Sukhodolov A (2012) Numerical analysis of the effect of momentum ratio on the dynamics and sediment entrainment capacity of coherent flow structures at a stream confluence. J Geophys Res 117(F4):F04028

    Google Scholar 

  8. Constantinescu G, Miyawaki S, Rhoads B, Sukhodolov A, Kirkil G (2011) Structure of turbulent flow at a river confluence with momentum and velocity ratios close to 1: insights from an eddy-resolving numerical simulation. Water Resour Res 47:W05507

    Google Scholar 

  9. Wolansky E, Imberger J, Heron ML (1984) Island wakes in shallow coastal waters. J Geophys Res 89(C6):10553–10569

    Article  Google Scholar 

  10. Ingram RG, Chu VH (1987) Flow around islands in Rupert bay: an investigation of the bottom friction effect. J Geophys Res 92(C13):14521–14533

    Article  Google Scholar 

  11. Rummel A, Carmer CF, Jirka GH (2002) Combined planar measurements of flow velocity and mass concentration in shallow flows part 1: development of a planar concentration analysis (PCA) system. In: Proceedings of international conference on hydraulic measurements and experimental methods, EWRI-ASCE and IAHR

  12. Carmer CF, Rummel A, Jirka GH (2002) Combined planar measurements of flow velocity and mass concentration in shallow flows part 2: application of couples PIV-PCA technique to turbulent shallow wake flows. In: Proceedings of international conference on hydraulic measurements and experimental methods, EWRI-ASCE and IAHR

  13. Chen D, Jirka GH (1999) LIF study of plane jet bounded in shallow water layer. J Hydraul Eng 125(8):817–826

    Article  Google Scholar 

  14. Kolyshkin AA, Ghidaoui MS (2003) Stability analysis of shallow wake flows. J Fluid Mech 494:355–377

    Article  Google Scholar 

  15. van Prooijen BC (2004) Shallow mixing layers. PhD thesis, Delft University of Technology

  16. Drazin PG, Reid WH (2004) Hydrodynamic stability, 2nd edn. Cambridge University Press, Cambridge

    Book  Google Scholar 

  17. Chu VH, Wu JH, Khayat R (1991) Stability of transverse shear flows in shallow open channels. J Hydraul Eng 117(10):1370–1388

    Article  Google Scholar 

  18. Jirka GH, Uijttewaal WSJ (2004) Shallow flows: a definition. In: Jirka GH, Uijttewaal WSJ (eds) Shallow flows: selected papers of the international symposium on shallow flows, 16–18 June 2003. Taylor and Francis, London, pp 3–11

  19. Liang JH (2006) Linear and nonlinear analysis of shallow mixing layers. Master thesis, HKUST

  20. Uijttewaal WSJ, Tukker J (1998) Development of quasi two-dimensional structures in a shallow free-surface mixing layer. Exp Fluids 24:192–200

    Article  Google Scholar 

  21. Uijttewaal WSJ, Booij R (2000) Effects of shallowness on the development of free-surface mixing layers. Phys Fluids 12(2):392–402

    Article  Google Scholar 

  22. Dracos T, Giger M, Jirka GH (1991) Plane turbulent jets in a bounded fluid layer. J Fluid Mech 241:587–614

    Article  Google Scholar 

  23. van Prooijen BC, Uijttewaal WSJ (2002) A linear approach for the evolution of coherent structures in shallow mixing layers. Phys Fluids 14(12):4105–4114

    Article  Google Scholar 

  24. Ghidaoui MS, Kolyshkin AA, Liang JH, Chan FC, Li Q, Xu K (2006) Linear and nonlinear analysis of shallow wakes. J Fluid Mech 548:309340

    Article  Google Scholar 

  25. Vreugdenhil CB (1994) Numerical methods for shallow-water flow. Kluwer, Dordrecht

    Book  Google Scholar 

  26. Pouquet A, Frisch U, chollet JP (1983) Turbulence with a spectral gap. Phys Fluids 24(4):877–879

    Article  Google Scholar 

  27. Geyer WR, Lavery AC, Scully ME, Trowbridge JH (2010) Mixing by shear instability at high Reynolds number. Geophys Res Lett 37:L22607

    Article  Google Scholar 

  28. Kolyshkin AA, Ghidaoui MS (2002) Gravitational and shear instabilities in compound and composite channels. J Hydraul Eng 128(12):1076–1086

    Article  Google Scholar 

  29. Duran-Matute M, Albagnac J, Kamp LPJ, van Heijst GJF (2010) Dynamics and structure of decaying shallow dipolar vortices. Phys Fluids 22:116606

    Article  Google Scholar 

  30. Lloyd PM, Stansby PK (1997) Shallow-water flow around model conical islands of small side slope. I: surface piercing. J Hydraul Eng 123(12):1057–1067

    Article  Google Scholar 

  31. Stansby PK (2006) Limitations of depth-averaged modeling for shallow wakes. J Hydraul Eng 132(7):737–740

    Article  Google Scholar 

  32. Geyer WR (1993) Three-dimensional tidal flow around headlands. J Geophys Res 98(C1):955–966

    Article  Google Scholar 

  33. Akkermans RAD, Cieslik AR, Kamp LPJ, Trieling RR, Clercx HJH, vanHeijst GJF (2008) three-dimensional structure of an electromagnetically generated dipolar vortex in a shallow fluid layer. Phys Fluids 20:116601

    Article  Google Scholar 

  34. Kamp LPJ (2012) Strain-vorticity induced secondary motion in shallow flows. Phys Fluids 24:023601

    Article  Google Scholar 

  35. van Senden DC, Imberger J (1990) Effects of initial conditions and Ekman suction on tidal outflows from inlets. J Geophys Res 95(C8):13373–13391

    Article  Google Scholar 

  36. Pedlosky J (1987) Geophysical fluid dynamics, 2nd edn. Springer, New York

    Book  Google Scholar 

  37. Wolanski E, Asaeda T, Tanaka A, Deleersnijder E (1996) Three-dimensional island wakes in the field, laboratory experiments and numerical models. Cont Shelf Res 16(11):1437–1452

    Article  Google Scholar 

  38. Alaee MJ, Ivey G, Pattiaratchi C (2004) Secondary circulation induced by flow curvature and coriolis effects around headlands and islands. Ocean Dyn 54:27–38

    Article  Google Scholar 

  39. Kalkwijk JPT, Booij R (1986) Adaptation of secondary flow in nearly-horizontal flow. J Hydraul Res 24:19–37

    Article  Google Scholar 

  40. Alaee MJ, Pattiaratchi C, Ivey G (1998) A field study of the three-dimensional structure of the Rottnest Island wake. In: Dronkers J, Scheffers MBAM (eds) Physics of estuaries and coastal seas. Balkema, Rotterdam, pp 239–245

    Google Scholar 

  41. Marques GM, Brown WS (2013) Tidal eddy motions in the western Gulf of Marine, Part 2: secondary flow. Cont Shelf Res 63:5114–5125

    Article  Google Scholar 

  42. Hinterberger C, Frohlich J, Rodi W (2007) Three-dimensional and depth averaged large-eddy simulations of some shallow water flows. J Hydraul Eng 133(8):857–872

    Article  Google Scholar 

  43. Nadaoka K, Yagi H (1998) Shallow-water turbulence modeling and horizontal large-eddy computation of river flow. J Hydraul Eng 124(5):493–500

    Article  Google Scholar 

  44. Stansby PK (2003) A mixing-length model for shallow turbulent wakes. J Fluid Mech 495:369–384

    Article  Google Scholar 

  45. Kirkil G, Constantinescu G (2009) Mean flow and coherent structures in a shallow mixing layer developing between parallel streams. In: 33nd IAHR congress conference proceedings (on CD), 9 Aug 2009–14 Aug 2009, Vancouver, BC

  46. Kimura I, Uijttewaal WSJ, Hosoda T, Mds Ali (2009) URANS computations of shallow grid turbulence. J Hydraul Eng 135(2):118–131

    Article  Google Scholar 

  47. Ghidaoui MS, Deng JQ, Gray WG, Xu K (2001) A boltzmann based model for open channel flows. Int J Comput Fluid D 20(6):436–451

    Google Scholar 

  48. Fisher HB, List EJ, Koh RCY, Imberger J, Brooks NH (1979) Mixing in inland and coastal waters, 2nd edn. Academic Press, San Diego

    Google Scholar 

  49. Corcos GM, Sherman FS (1984) The mixing layer: deterministic models of a turbulent flow. Part 1. Introduction and the two-dimensional flow. J Fluid Mech 139:29–65

    Article  Google Scholar 

  50. Schmid PJ, Henningson DS (2001) Stability and transition in shear flows. Springer, New York

    Book  Google Scholar 

  51. Metcalfe RW, Orszag SA, Brachet ME, Menon S, Riley JJ (1987) Secondary instability of a temporally growing mixing layer. J Fluid Mech 184:207–243

    Article  Google Scholar 

  52. Carmar CFV (2005) Shallow turbulent wake flows: momentum and mass transfer due to large scale coherent vortical structures. PhD thesis, University of Karlsruhe, Germany

  53. Lesieur M (2008) Turbulence in fluids, 4th revised and enlarged edn. Springer, Dordrecht

  54. Weiss J (1991) The dynamics of enstrophy transfer in two-dimensional hydrodynamics. Physica D 48:273–294

    Article  Google Scholar 

  55. Pierrehumbert RT, Widnall SE (1982) The two- and three-dimensional instabilities of a spatially periodic shear layer. J Fluid Mech 114:59–82

    Article  Google Scholar 

  56. Lam MY, Liu HW, Ghidaoui MS (2010) Investigation of temporal mixing layer in shallow water with BGK algorithm. J Hydro-Environ Res 4:123–129

    Article  Google Scholar 

  57. Ghidaoui MS, Kolyshkin AA (1999) Linear stability analysis of lateral motion in compound channels with free surface. J Hydraul Eng 125(8):871–880

    Article  Google Scholar 

Download references

Acknowledgments

The financial support by the Hong Kong Grant Council, Project 612712, 612910 and 612511, is gratefully acknowledged.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to M. Y. Lam.

Appendix: Derivation of the modal kinetic energy equations

Appendix: Derivation of the modal kinetic energy equations

The derivation of the modal kinetic energy equation is detailed here. The derivation starts with applying the rigid-lid assumption to the Galilean transformed shallow water equations (5)–(7). The assumption is to replace the free-surface with a rigid-lid, and to replace the hydrostatic pressure with the pressure under the rigid-lid, \(p(x,y,t)\). This assumption is shown to be valid for shallow flows with small Froude numbers [14, 57]. Then, since the perturbations in shallow mixing layers are superpositions of interacting modes, a convenient way to investigate the growth and interaction of the modes is to perform Fourier decomposition of the flow variables. Substitute equations (12)–(14) into Eqs. (5)–(7). The mass equation for the mean flow vanishes. The mass equation for the perturbation is then:

$$\begin{aligned} i\left( \frac{2\pi k}{L_x}\right) \hat{u}_k+\frac{\partial \hat{v}_k}{\partial y}=0 \end{aligned}$$
(20)

Concerning the momentum equations, apply the normal flow condition at the inflexion point of the mixing layer:

$$\begin{aligned} 0=-\frac{c_f}{2} \overline{U}^2+g \overline{H}S_{0X} \end{aligned}$$
(21)

The momentum equation for the mean flow is then:

$$\begin{aligned} \frac{\partial (\overline{U}+\widetilde{u_m})}{\partial {t}} + 2 \mathfrak {R}\sum _{k=1}^N \frac{\partial \hat{u}_{-k} \hat{v}_k}{\partial y}&= -\frac{c_f}{\overline{H}}(\overline{U} \widetilde{u_m}) -\frac{c_f}{2\overline{H}}\widetilde{u_m}^2 -\frac{c_f}{\overline{H}}\sum _{k=1}^N \left( |\hat{u}_k|^2 +\frac{1}{2} |\hat{v}_k|^2\right) \nonumber \\&+\nu _{total}^t \frac{\partial ^2(\overline{U}+\widetilde{u_m})}{\partial y^2} \end{aligned}$$
(22)

where \(\mathfrak {R}\) mean taking the real part. The momentum equation for mode \(k\) is:

$$\begin{aligned}&\frac{\partial {\hat{u}_k}}{\partial {t}} + i\left( \frac{2 \pi k}{L_x}\right) \widetilde{u_m}\hat{u}_k + \hat{v}_k\frac{\partial \widetilde{u_m}}{\partial {y}}+ i\left( \frac{2 \pi k}{L_x}\right) \sum _{n+s=k}\hat{u}_n\hat{u}_s+\sum _{n+s=k} \frac{\partial \hat{u}_n \hat{v}_s}{\partial y}\nonumber \\&\quad = -i\left( \frac{2 \pi k}{L_x}\right) \hat{p}_k-\frac{c_f}{\overline{H}}(\overline{U}+\widetilde{u_m})\hat{u}_k\nonumber \\&\quad \quad -\frac{c_f}{2\overline{H}}\sum _{n+s=k}\left[ \left( \hat{u}_n \hat{u}_s+\frac{1}{2} \hat{v}_n \hat{v}_s\right) \right] +\nu _{total}^t \left[ -\left( \frac{2 \pi k}{L_x}\right) ^2 \hat{u}_k+\frac{\partial {^2 \hat{u}_k}}{\partial {y^2}}\right] \end{aligned}$$
(23)
$$\begin{aligned}&\frac{\partial {\hat{v}_k}}{\partial {t}} + i\left( \frac{2 \pi k}{L_x}\right) \widetilde{u_m}\hat{v}_k + i\left( \frac{2 \pi k}{L_x}\right) \sum _{n+s=k}\hat{u}_n\hat{v}_s+\sum _{n+s=k} \frac{\partial \hat{v}_n \hat{v}_s}{\partial y} \nonumber \\&\quad = -\frac{\partial \hat{p}_k}{\partial y}-\frac{c_f}{2\overline{H}}(\overline{U}+\widetilde{u_m})\hat{v}_k -\frac{c_f}{2\overline{H}}\sum _{n+s=k}(\hat{u}_n \hat{v}_s)+\nu _{total}^t \left[ -\left( \frac{2 \pi k}{L_x}\right) ^2 \hat{v}_k+\frac{\partial {^2 \hat{v}_k}}{\partial {y^2}}\right] \nonumber \\ \end{aligned}$$
(24)

where \(n\) and \(s\) goes from \(-N\) to \(N\), and \(n \ne 0\) and \(s \ne 0\). \(\nu _{total}^t\) is assumed to be a constant, corresponding to the eddy viscosity at the center of the mixing layer where the 2DCS are situated. It is a simplifying assumption to prevent from including additional nonlinearity stemming from the eddy viscosity in the current work.

To obtain the modal kinetic energy equation for mode \(k\), multiply equation (23) by \(\hat{u}_{-k}\) and multiply the conjugate equation of (23) by \(\hat{u}_k\). The pair of conjugate equations are added together. The pair of equations become:

$$\begin{aligned}&\frac{\partial {|\hat{u}_k|^2}}{\partial {t}} + (\hat{u}_{-k}\hat{v}_k + \hat{v}_{-k}\hat{u}_k) \frac{\partial \widetilde{u_m}}{\partial {y}}\nonumber \\&+ i\left( \frac{2 \pi k}{L_x}\right) \sum _{n+s=k}(\hat{u}_n\hat{u}_s\hat{u}_{-k} - \hat{u}_{-n}\hat{u}_{-s}\hat{u}_{k}) +\sum _{n+s=k} \left( \hat{u}_{-k} \frac{\partial \hat{u}_n \hat{v}_s}{\partial y} + \hat{u}_{k} \frac{\partial \hat{u}_{-n} \hat{v}_{-s}}{\partial y}\right) \nonumber \\&\quad = -i\left( \frac{2 \pi k}{L_x}\right) \hat{p}_k\hat{u}_{-k} +i\left( \frac{2 \pi k}{L_x}\right) \hat{p}_{-k}\hat{u}_k - \frac{2c_f}{\overline{H}}(\overline{U}+\widetilde{u_m}) |\hat{u}_k|^2\nonumber \\&\quad \quad -\frac{c_f}{2\overline{H}}\sum _{n+s=k}(\hat{u}_n \hat{u}_s \hat{u}_{-k} + \hat{u}_{-n} \hat{u}_{-s} \hat{u}_{k}) - \frac{c_f}{4\overline{H}}\sum _{n+s=k} (\hat{v}_n \hat{v}_s \hat{u}_{-k} + \hat{v}_{-n} \hat{v}_{-s} \hat{u}_k))\nonumber \\&\quad \quad +\nu _{total}^t \left[ -2\left( \frac{2 \pi k}{L_x}\right) ^2 |\hat{u}_k|^2+ \hat{u}_{-k}\frac{\partial {^2 \hat{u}_k}}{\partial {y^2}} + \hat{u}_k\frac{\partial {^2 \hat{u}_{-k}}}{\partial {y^2}}\right] \end{aligned}$$
(25)

Also, multiply equation (24) by \(\hat{v}_{-k}\) and multiply the conjugate equation of (24) by \(\hat{v}_k\). The pair of conjugate equations are added together. The pair of equations become:

$$\begin{aligned}&\frac{\partial {|\hat{v}_k|^2}}{\partial {t}} + i\left( \frac{2 \pi k}{L_x}\right) \sum _{n+s=k}(\hat{u}_n\hat{v}_s\hat{v}_{-k} - \hat{u}_{-n}\hat{v}_{-s}\hat{v}_{k}) +\sum _{n+s=k} \left( \hat{v}_{-k}\frac{\partial \hat{v}_n \hat{v}_s}{\partial y} + \hat{v}_{k}\frac{\partial \hat{v}_{-n} \hat{v}_{-s}}{\partial y}\right) \nonumber \\&=-\hat{v}_{-k}\frac{\partial \hat{p}_k}{\partial y}-\hat{v}_{k}\frac{\partial \hat{p}_{-k}}{\partial y} -\frac{c_f}{\overline{H}}(\overline{U}+\widetilde{u_m})|\hat{v}_k|^2 -\frac{c_f}{2\overline{H}}\sum _{n+s=k}(\hat{u}_n \hat{v}_s\hat{v}_{-k}+\hat{u}_{-n} \hat{v}_{-s}\hat{v}_{k})\nonumber \\&\quad +\nu _{total}^t \left[ -2\left( \frac{2 \pi k}{L_x}\right) ^2 |\hat{v}_k|^2 + \hat{v}_{-k}\frac{\partial {^2 \hat{v}_k}}{\partial {y^2}}+ \hat{v}_{k}\frac{\partial {^2 \hat{v}_{-k}}}{\partial {y^2}}\right] \end{aligned}$$
(26)

Equations (25) and (26) are added together and then take domain average along \(y\)-direction (i.e. \(\frac{1}{L_y} \int _{-L_y/2}^{L_y/2}\ldots dy\)). The mean flow is further decomposed into a base flow and a mean flow correction, \(\widetilde{u_m}(y,t) = \widetilde{u_b}(y,t)+\hat{u}_0(y,t)\). Use the mass equation (20) and take \(L_y\) to be much larger than the coherent structures so that \(\hat{u}_k=0\), \(\hat{v}_k=0\), \(\partial (\widetilde{u_b}+\hat{u}_0) /\partial y=0\), \(\partial \hat{u}_k/\partial y=0\) and \(\partial \hat{v}_k/\partial y=0\) at \(y=\pm \frac{L_y}{2}\). This implies the turbulent energy fluxes by turbulent convection, the viscous diffusion of turbulent energy and the turbulent energy flux by turbulent pressure across \(y= \frac{L_y}{2}\) and \(y= -\frac{L_y}{2}\) are zero. The modal kinetic energy equation for mode \(k\) is derived as:

$$\begin{aligned} \frac{dE_k}{dt}&= - \left[ \frac{1}{L_y} \int _{-L_y/2}^{L_y/2}{2 \mathfrak {R}(\hat{u}_{-k} \hat{v}_k) \frac{\partial \widetilde{u_b}}{\partial y} dy}\right] - \left[ \frac{1}{L_y} \int _{-L_y/2}^{L_y/2}{2 \mathfrak {R}(\hat{u}_{-k} \hat{v}_k) \frac{\partial \hat{u}_0}{\partial y} dy}\right] \nonumber \\&- \frac{1}{L_y} \int _{-L_y/2}^{L_y/2}2 \sum _{n+s=k} \mathfrak {R}\left[ i\left( \frac{2 \pi k}{L_x}\right) \hat{u}_n \hat{u}_s \hat{u}_{-k}\!-\!\hat{u}_n \hat{v}_s \frac{\partial \hat{u}_{-k}}{\partial y} \!+\! i\left( \frac{2 \pi k}{L_x}\right) \hat{u}_n \hat{v}_s \hat{v}_{-k} \! -\!\hat{v}_n \hat{v}_s \frac{\partial \hat{v}_{-k}}{\partial y}\right] dy\nonumber \\&- \frac{1}{L_y} \frac{c_f}{\overline{H}} \int _{-L_y/2}^{L_y/2}{2 (\overline{U}+\widetilde{u_b}) \vert \hat{u}_k \vert ^2 + (\overline{U}+\widetilde{u_b}) \vert \hat{v}_k \vert ^2 dy} - \frac{1}{L_y} \frac{c_f}{\overline{H}} \int _{-L_y/2}^{L_y/2} 2 \hat{u}_0 \vert \hat{u}_k \vert ^2 + \hat{u}_0 \vert \hat{v}_k \vert ^2 dy\nonumber \\&- \frac{1}{L_y}\frac{c_f}{\overline{H}} \int _{-L_y/2}^{L_y/2}{\sum _{n+s=k} {\mathfrak {R}\left[ \hat{u}_n \hat{u}_s \hat{u}_{-k} + \hat{u}_n \hat{v}_s \hat{v}_{-k} + \frac{1}{2} \hat{v}_n \hat{v}_s \hat{u}_{-k}\right] }dy}\nonumber \\&+ \nu _{total}^t \frac{1}{L_y} \int _{-L_y/2}^{L_y/2}{-2 (2 \pi k/L_x)^2 (\vert \hat{u}_k \vert ^2 + \vert \hat{v}_k \vert ^2) - 2\left( \vert \frac{\partial \hat{u}_k}{\partial y} \vert ^2 + \vert \frac{\partial \hat{v}_k}{\partial y} \vert ^2\right) dy} \end{aligned}$$
(27)

Where:

$$\begin{aligned} E_k=\frac{1}{L_y}\int _{-L_y/2}^{L_y/2}{\vert \hat{u}_k \vert ^2 + \vert \hat{v}_k \vert ^2 dy} \end{aligned}$$
(28)

There are \(N\) modal kinetic energy equations \(k=1,2,3,\ldots ,N\), because the modal kinetic energy equation for mode \(k\) is derived from both the momentum equation for mode \(k\) and the momentum equation for mode \(-k\) for all \(k \le N\). \(n\) and \(s\) goes from \(-N\) to \(N\), with \(n \ne 0\) and \(s \ne 0\).

The full set of modal kinetic energy equations should in fact include the mean flow kinetic energy equation to be complete, but the derivation of the mean flow kinetic energy equation is omitted here for brevity.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Lam, M.Y., Ghidaoui, M.S. Fourier analysis of the roll-up and merging of coherent structures in shallow mixing layers. Environ Fluid Mech 14, 997–1026 (2014). https://doi.org/10.1007/s10652-014-9371-2

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10652-014-9371-2

Keywords

Navigation