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Stability of Parallel Flows

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47 Re 180: Periodic 2D vortex street. Re = 190: Subcritical Mode A ... Example: Initiation of vortex shedding from a circular cylinder at ... layer vortices ... – PowerPoint PPT presentation

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Title: Stability of Parallel Flows


1
Stability of Parallel Flows
2
  • Analysis by LINEAR STABILITY ANALYSIS.
  • Transitions as Re increases
  • 0 lt Re lt 47 Steady 2D wake
  • Re 47 Supercritical Hopf bifurcation
  • 47 lt Re lt 180 Periodic 2D vortex street
  • Re 190 Subcritical Mode A inst. (?d 4d)
  • Re 240 Mode B instability (?d 1d)
  • Re increasing spatio-temporal chaos, rapid
    transition to turbulence.

Mode B instability in the wake behind a circular
cylinder at Re 250 Thompson (1994)
3
Atmospheric Shear Instability
  • Examples -
  • Kelvin-Helmholtz instability
  • Velocity gradient in a continuous fluid or
  • Velocity difference between layers of fluid
  • May also involve density differences, magnetic
    fields

Atmospheric Shear
4
Cylinder Wake - High Re
  • Bloor-Gerrard Instability (cylinder shear layer
    instability)

Karman shedding
Shear layer instability
Prasad and Williamson JFM 1997
5
Transition Types
  • Instability Types
  • Convective versus Absolute instability
  • A convective instability is convected away
    downstream - it grows as it does so, but at a
    fixed location, the perturbation eventually dies
    out.
  • Example KH instability
  • Absolute instability means at a fixed location a
    perturbation will grow exponentially. Even
    without upstream noise - the instability will
    develop
  • Example Karman wake

6
Transition Types
  • Supercritical versus Subcritical transition
  • A supercritical transition occurs at a fixed
    value of the control parameter
  • Example Initiation of vortex shedding from a
    circular cylinder at Re46. Mode B for a cylinder
    wake, Shedding from a sphere.
  • A subcritical transition occurs over a range of
    the control parameter depending on noise level.
    There is an upper limit above which transition
    must occur.
  • Example Mode A instability - first
    three-dimensional mode of a cylinder wake.

Mode A subcritical
Mode B supercritical
U
7
Subcritical (hysteretic transition)
  • First 3D cylinder wake transition (Mode A, Re190)

8
Supercritical transition
  • Mode B (3D cylinder wake at Re260)

9
Shear Layer Instability
  • U(y) tanh(y) - Symmetric Shear Layer

Periodic inflow/outflow
10
Jet instability
  • U(y) sech2(y) - Symmetric jet

Again periodic boundaries
11
Cylinder wake results
  • Shear Layer Instability in a Cylinder Wake

Re gt 1000-2000
Transition point from Convective to
Absolute Instability
12
Frequency Prediction for a Cylinder Wake
  • Numerical Stability Analysis based on Time-Mean
    Flow
  • Extract velocity profiles across wake
  • Analyze using parallel stability analysis to
    predict Strouhal number

Experiments
Rayleigh equation
DNS
13
Interesting Recent Work
  • Barkley (2006 EuroPhys L)
  • Time mean wake is neutrally stable - preferred
    frequency corresponds to observed Strouhal number
    to within 1
  • Chomaz, Huerre, Monkewitz Extension to
    non-parallel wakes
  • Pier (2002, JFM)
  • Non-linear stability modes to predict observed
    shedding frequency of a cylinder wake
  • Hammond and Redekopp (JFM 1997)
  • Analysis of time-mean flow of a flat plate.
  • Also of interest Non-normal mode
    analysis/optimal growth theory.to predict
    transition in Poiseiulle flow.

14
Basic Stability Theory 2 Absolute Convective
Instability
  • Background
  • Generally, part of a wake may be convectively
    unstable and part may be absolutely unstable
  • Recall
  • Convective instability means a disturbance will
    die out locally but will grow in amplitude as it
    convects downstream.
  • Think of shear layer vortices
  • Absolute instability means that a disturbance
    will grow in amplitude locally (where it was
    generated)
  • Think of the Karman wake.

15
Absolute Convective unstable zones
Saturated state
Velocity profiles on vertical lines used for
analysis
Convectively unstable
Absolutely unstable
Either - pre-shedding or time-mean wake
16
Selection of the wake frequency
  • Problem Wake absolutely unstable over a finite
    spatial range.
  • Prediction of frequency at any point in this
    range.
  • So what is the selected frequency?
  • There were three completing theories
  • Monkewitz and Nguyen (1987) proposed the Initial
    Resonance Condition
  • The frequency selected corresponds to the
    predicted frequency at the point where the
    initial transition from convective to absolute
    instability occurs.
  • Koch (1985) proposed the downstream resonance
    condition.
  • This states that it is the downstream transition
    from absolute to convective instability that
    determines the selected frequency.
  • Pierrehumbert (1984) proposed that the selection
    is determined by the point in the absolute
    instability range with the maximum amplification
    rate.
  • These theories are largely ad-hoc.

17
Selection of wake frequency - Saddle Point
Criterion
  • Since then
  • Chomaz, Huerre, Redekopp (1991) Monkewitz in
    various papers have shown that the global
    frequency selection for (near) parallel flows is
    determined by the complex frequency of the saddle
    point in complex space, which can be determined
    by analytic continuation from the behaviour on
    the real axis.
  • This was demonstrated quite nicely by the work of
    Hammond and Redekopp (1997), who examined the
    frequency prediction for the wake from a square
    trailing edge cylinder.

18
Test Case - Flow over trailing edge forming a wake
  • Hammond and Redekopp (JFM 1997)
  • Considered the general case below, but
  • Focus on symmetric wake without base suction.

19
Linear theory assumptions
  • Is the wake parallel?
  • This indicates how parallel the wake is at Re160

20
Frequency prediction with downstream distance
  • The real and imaginary components of the complex
    frequency is determined using both Orr-Sommerfeld
    (viscous) and Rayleigh (inviscid) solvers from
    velocity profiles across the wake.
  • These are used to construct the two plots below

Predicted oscillation frequency
Predicted Growth rate
Downstream distance
21
Saddle point prediction
  • Prediction of selected frequency
  • First note that the downstream point at which the
    minimum frequency occurs does not correspond with
    the point at which the maximum growth rate
    occurs.
  • This means that the saddle point occurs in
    complex space!!!!
  • This is the complex point at which the frequency
    and growth rate reach extrema together.
  • Can use complex Taylor series Cauchy-Riemann
    equations to project off the real axis (the only
    place where you know anything).

Here, both omega and x are complex!
Complex x
Saddle point
x
Real x
22
Accuracy of saddle point prediction
  • Prediction of preferred frequency is
  • Parallel inviscid theory at Re160 gives 0.1006
  • Numerical simulation of (saturated) shedding at
    Re160 gives 0.1000.
  • Better than 1 accuracy!
  • Saddle point at
  • Things to note
  • Spatial selection point is within 1D of the
    trailing edge.
  • Amazing accuracy.
  • Generally, imaginary component of saddle point
    position is small.
  • The predicted frequency (on the real axis) may
    not vary all that much anyway over the absolute
    instability region, and may not vary much from
    the position of maximum growth rate. Hence all
    previous adhoc conditions are generally close.
  • Note prediction is based on time-mean wake not
    the steady (pre-shedding) wake.

23
Linear theory - inviscid and viscous
  • Predictions from Hammond and Redekopp (1997)
  • Inviscid Rayleigh equation on downstream
    profiles
  • Viscous Orr-Sommerfeld equation on downstream
    profiles
  • Re 160.

24
Saturation of wake (Landau Model)
  • Further points
  • Wake frequency varies as the wake saturates

Wake saturating.
Frequency variation Based on Landau equation
Supercritical transition
25
Frequency Prediction for a Circular Cylinder Wake
  • Numerical Stability Analysis based on Time-Mean
    Flow
  • Extract velocity profiles across wake
  • Analyze using parallel stability analysis to
    predict Strouhal number

Experiments
Rayleigh equation
DNS
26
Inadequacy of theory?
  • We need to know the time-mean flow (either by
    numerical simulation or running experiments) to
    computed the preferred wake frequency!!!
  • This is not very satisfying
  • Other option is to undertake a non-linear
    stability analysis on the steady base flow (when
    the wake is still steady - prior to shedding).
  • This was done by Pier (JFM 2002).

Vorticity field - cylinder wake Re 100
Unstable steady wake Re 100
Time-mean wake Re 100
27
Non-linear theory
  • Pier (JFM 2002) Pier and Huerre (2001).
  • Frequency selection based on the (imposed) steady
    cylinder wake using non-linear theory.

Absolute instability
Predictions of growth rate as a function of
Reynolds number for the steady cylinder wake.
Predicted wake frequency
28
Frequency predictions based on near-parallel,
inviscid assumption
  • Nonlinear theory indicates that the saturated
    wake frequency corresponds to the frequency
    predicted from the Initial Resonance Criterion
    (IRC) of Monkewitz and Nguyen (1987) based on
    linear analysis.

IRC criterion ( nonlinear prediction) (Monkewitz
and Nguyen)
DNS
Experiments
From mean flow (saddle point criterion)
Downstream A--gtC transition (Koch)
Max amplication (Pierrehumbert)
Saddle point on Steady flow
29
Global stability analysis
  • Prediction based on Global instability analysis
    of time-mean wake. (Barkley 2006).

Match with experiments DNS For wake frequency
Predicted mode is neutrally stable
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