Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D...

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Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin Wu and Tom Chang

Transcript of Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D...

Page 1: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows,

2D MHD simulation and solar wind data

Cheng-chin Wu and Tom Chang

Page 2: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

ROMA • a generic fluctuating temporal X(t)• a scale dependent difference series δX(t,τ)=X(t+ τ)-X(t) time lag τ• the probability distribution functions (PDFs) P(δX, τ) of δX(t,τ) for different time lag values τ. • If the fluctuating event X(t) is monofractal –- self-similar, the PDFs would scale (collapse) onto one scaling function Ps : P(δX, τ) τs=Ps(δX/τs)=Ps(Y), with Y= δX/τs (1)

where s, a constant, is the scaling exponent.• Data and model (MHD and fluid) results indicate turbulent flows are generally not monofractal and are multifractal.• Chang and Wu [2008] proposed ROMA for multifractal fluctuations with the following scaling: P(δX, τ) τs(Y)=Ps(Y) with Y= δX/τs(Y) (2) where the scaling exponent s(Y) is a function of Y.• Data and model (MHD and fluid) results indicate the applicability of ROMA. Some will be discussed in the talk.

Page 3: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

ROMA •The key in ROMA is then to find s(Y) and Ps(Y) from P(δX, τ) with the following scaling: P(δX, τ) τs(Y)=Ps(Y) with Y= δX/τs(Y) (2)• Existence of s(Y) and Ps(Y) is not trivial: a function P(δX, τ) of two variables is replaced by two functions of a single variable.•Two methods of finding s(Y) and Ps(Y): (a) using (2) directly. [Given s →Y] (b) using ranked-ordered structure functions for the small range Y1<Y<Y2:

with α=Y1 τs, β=Y2 τs. Search for s such that Sm ~ τ sm and s(Y)=s. [Given Y →s]• Consistency check: From s(Y) and Ps(Y), P(δX, τ) can be calculated from the scaling relation (2) and can be checked with the data/model results.

Xd),X()X(),X(

PmmS

Page 4: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

ROMA •3D fluid turbulence from the JHU turbulence database •2D MHD simulations•Solar wind data

•Finding s(Y) and Ps(Y) using method (a) and Consistency check

Page 5: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

3D fluid turbulence flowfrom the JHU turbulence database cluster

turbulence.pha.jhu.edu

• Forced isotropic turbulence:• Direct numerical simulation (DNS) using

1,0243 nodes. Domain: (2π)3

• Navier-Stokes (with explicit viscosity terms) is solved using pseudo-spectral method.

• Energy is injected by keeping constant the total energy in shells shuch that |k| is less or equal to 2.

• There is one dataset ("coarse") with 1024 timesteps available, for time t between 0 and 2.048.

• There is another dataset ("fine") that stores every single time-step of the DNS for t between 0.0002 and 0.0198)

Page 6: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

3D fluid turbulence flow

• There are 10244 data points in the data set. • Here we use only 5 x 10242 values of velocity fields, which consists of values on 5 z-planes: (t, z) = (1, 0), (0, 9 Δ), (2, 99 Δ), (0.5, 499 Δ), and (1.5, 499 Δ) with Δ=grid spacing=2π/1024.• fluctuating field δX(r,δ)=|δv||(r,δ)|=|[v(r+δi)-v(r)]·i|, with i unit vector.

In the calculation: |δv||(r,δ)| = |vx(r+δix)-vx(r)| or |vy(r+δiy)-vy(r)| and δ= (16,…, 160) Δ; Δ=grid spacing=2π/1024.

• According to Kolmogorov (K41), S3(δv||,δ) ~ δ, meaning 3 s=1 and s=1/3.

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3D fluid turbulence flow

PDF(δv||,δ) on 5 z-planes: left panel with δ=32Δ and Right panel with δ=96Δ.

Page 8: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

3D fluid turbulence flow

PDF(δv||,δ) average over 5 z-planes: blue with δ=32Δ and

red with δ=96Δ. Normalization:

Note the cross over of PDFs. 1dX),X(PDF

Page 9: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

S=0.2: pdfs collapse at Y~38.5 and Ps~1.16 10-2

Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δgreen:48 Δ; black: 64 Δ.

Page 10: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

S=0.3: PDFs collapse at Y~25 with Ps~1.8 10-2, and Y~144 with Ps~2.2 10-5.

Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δgreen:48 Δ; black: 64 Δ.

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S=1/3: PDFs collapse at Y~20 with Ps~2.2 10-2, and Y~80 with Ps~8. 10-4.

Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δgreen:48 Δ; black: 64 Δ.

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S=0.35 PDFs collapse at Y~17.5 with Ps~2.45 10-2, and Y~62 with Ps~1.98 10-3.

Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δgreen:48 Δ; black: 64 Δ.

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S=0.4 PDFs collapse at Y~0 with Ps~3.9 10-2, and Y~32 with Ps~1.1 10-2.

Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δgreen:48 Δ; black: 64 Δ.

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S=0.5 PDFs collapse at Y~15 with Ps~3 10-2.

Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δgreen:48 Δ; black: 64 Δ.

Page 15: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Summary: blue + and green * indicate obtained s(Y) and Ps(Y). s(Y) and Ps(Y) given by red curves are used in the consistence check.

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Consistency check 1: Given s(Y) and Ps(Y), one can compute PDF through the scaling relations: P(δX, δ)=Ps(Y)/τs(Y) and δX= τs(Y) Y. The results are consistent with the raw PDF from the simulation.

Computed PDFs by markers; raw PDFs by solid curvesRed circles: δ=32∆; green squares: δ=48∆;Magenta diamonds: δ=64∆; blue triangles: δ=96∆ Left panel for the whole range of δv||; right panel is an expanded view.

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Consistency check 2: δ=24, 48, 96, 128∆

Computed PDFs by markers; raw PDFs by solid curvesRed circles: δ=24∆; green squares: δ=48∆;Magenta diamonds: δ=96∆; blue triangles: δ=128∆

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Consistency check 3: δ=16, 48, 96, 160∆

Computed PDFs by markers; raw PDFs by solid curvesRed circles: δ=16∆; green squares: δ=48∆;Magenta diamonds: δ=96∆; blue triangles: δ=160∆

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Consistency check 4: sensitivity to changes in s(Y) and Ps(Y)

Y, s(Y), f(Y)Red circle: 40, 0.38, 7.1 10-3Green right triangle: 40, 0.36, 7.1 10-3Blue left triangle: 40, 0.40, 7.1 10-3Magenta up triangle:40, 0.38, 7.8 10-3Black down triangle:40, 0.38, 6.3 10-3

Black curves are PDFat δ=32, 48, 64, 96Δ

δ=32Δ

δ=96Δ

Page 20: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Consistency check 5: sensitivity to changes in s(Y) and Ps(Y)

Y, s(Y), f(Y)Red circle: 5, 0.398, 3.75 10-3Green right triangle: 5, 0.44, 3.75 10-3Blue left triangle: 5, 0.36, 3.75 10-3Magenta up triangle:5, 0.398, 4.05 10-3Black down triangle:5, 0.398, 3.45 10-3

Black curves are PDFat δ=32, 48, 64, 96Δ

δ=32Δ

δ=96Δ

δ=32Δ

δ=96Δ

Page 21: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Red circles: δ=16∆; green squares: δ=48∆;Magenta diamonds: δ=96∆; blue triangles: δ=160∆

Consistency check 6: PDF for 0.4 < s(Y) < 0.8

δ=96Δs

Ps

Page 22: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

3D fluid turbulence: fluctuations of v2

Ps(Y)

Page 23: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

3D fluid turbulence: fluctuations of v2

Computed PDFs by markers; raw PDFs by solid curvesRed circles: δ=16∆; green squares: δ=32∆;Magenta diamonds: δ=64∆; blue triangles: δ=96∆

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2D MHD simulations: fluctuations of B2

sPs

Page 25: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

2D MHD simulations: fluctuations of B2

Computed PDFs by markers; raw PDFs from simulations by solid curvesRed circles: δ=32∆; green squares: δ=48∆; blue triangles: δ=96∆ Left panel for a large range of δB2; right panel is an expanded view.

Page 26: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Solar wind data: fluctuations of B2 Scaled PDF [solar wind data: Chang, Wu, and Podesta, AIP Conf Proc, 1039, 75 (2008)]

From solar wind dataPs(Y) used in the calculation

Page 27: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Solar wind data: fluctuations of B2

ROMA spectrum from datas(Y) used in the calculation

Page 28: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Solar wind data: fluctuations of B2

Computed PDFs from the scaling relations are shown in the front; data are shown in the back. Green (o): τ=1000s; blue (x): 96s; red(+): 9s.

Page 29: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Solar wind data: fluctuations of B2

Using s=0.44 (monofractal) and the same Ps(Y), computed PDFs from the scaling relations are shown in the front; data are shown in the back. Green (o): τ=1000s; blue (x): 96s; red(+): 9s.

S=0.44

Page 30: Application of rank-ordered multifractal analysis (ROMA) to intermittent fluctuations in 3D turbulent flows, 2D MHD simulation and solar wind data Cheng-chin.

Conclusion

ROMA is robust in the three cases studied here: 3D turbulent flows,

2D MHD simulation and solar wind data.