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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.

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

1 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

2 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 P s : P(δX, τ) τ s =P s (δX/τ s )=P s (Y), with Y= δX/τ s (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) τ s(Y) =Ps(Y) with Y= δX/τ s(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.

3 ROMA The key in ROMA is then to find s(Y) and P s (Y) from P(δX, τ) with the following scaling: P(δX, τ) τ s(Y) =Ps(Y) with Y= δX/τ s(Y) (2) Existence of s(Y) and P s (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 P s (Y): (a) using (2) directly. [Given s →Y] (b) using ranked-ordered structure functions for the small range Y 1 <Y<Y 2 : with α=Y 1 τ s, β=Y 2 τ s. Search for s such that S m ~ τ sm and s(Y)=s. [Given Y →s] Consistency check: From s(Y) and P s (Y), P(δX, τ) can be calculated from the scaling relation (2) and can be checked with the data/model results.

4 ROMA 3D fluid turbulence from the JHU turbulence database 2D MHD simulations Solar wind data Finding s(Y) and P s (Y) using method (a) and Consistency check

5 3D fluid turbulence flow from the JHU turbulence database cluster turbulence.pha.jhu.edu Forced isotropic turbulence: Direct numerical simulation (DNS) using 1,024 3 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)

6 3D fluid turbulence flow There are 1024 4 data points in the data set. Here we use only 5 x 1024 2 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)| = |v x (r+δi x )-v x (r)| or |v y (r+δi y )-v y (r)| and δ= (16,…, 160) Δ; Δ=grid spacing=2π/1024. According to Kolmogorov (K41), S 3 (δv ||,δ) ~ δ, meaning 3 s=1 and s=1/3.

7 3D fluid turbulence flow PDF( δv ||,δ) on 5 z-planes: left panel with δ=32Δ and Right panel with δ=96Δ.

8 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.

9 S=0.2: pdfs collapse at Y~38.5 and P s ~1.16 10 -2 Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δ green:48 Δ; black: 64 Δ.

10 S=0.3: PDFs collapse at Y~25 with P s ~1.8 10 -2, and Y~144 with P s ~2.2 10 -5. Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δ green:48 Δ; black: 64 Δ.

11 S=1/3: PDFs collapse at Y~20 with P s ~2.2 10 -2, and Y~80 with P s ~8. 10 -4. Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δ green:48 Δ; black: 64 Δ.

12 S=0.35 PDFs collapse at Y~17.5 with P s ~2.45 10 -2, and Y~62 with P s ~1.98 10 -3. Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δ green:48 Δ; black: 64 Δ.

13 S=0.4 PDFs collapse at Y~0 with P s ~3.9 10 -2, and Y~32 with P s ~1.1 10 -2. Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δ green:48 Δ; black: 64 Δ.

14 S=0.5 PDFs collapse at Y~15 with P s ~3 10 -2. Left: blue δ=32Δ; red δ=96Δ right: blue: δ=32Δ; red δ=96Δ green:48 Δ; black: 64 Δ.

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

16 Consistency check 1: Given s(Y) and P s (Y), one can compute PDF through the scaling relations: P(δX, δ)=P s (Y)/τ s(Y) and δX= τ s(Y) Y. The results are consistent with the raw PDF from the simulation. Computed PDFs by markers; raw PDFs by solid curves Red 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.

17 Consistency check 2: δ=24, 48, 96, 128∆ Computed PDFs by markers; raw PDFs by solid curves Red circles: δ=24∆; green squares: δ=48∆; Magenta diamonds: δ=96∆; blue triangles: δ=128∆

18 Consistency check 3: δ=16, 48, 96, 160∆ Computed PDFs by markers; raw PDFs by solid curves Red circles: δ=16∆; green squares: δ=48∆; Magenta diamonds: δ=96∆; blue triangles: δ=160∆

19 Consistency check 4: sensitivity to changes in s(Y) and P s (Y) Y, s(Y), f(Y) Red circle: 40, 0.38, 7.1 10-3 Green right triangle: 40, 0.36, 7.1 10-3 Blue left triangle: 40, 0.40, 7.1 10-3 Magenta up triangle:40, 0.38, 7.8 10-3 Black down triangle:40, 0.38, 6.3 10-3 Black curves are PDF at δ=32, 48, 64, 96Δ δ=32Δ δ=96Δ

20 Consistency check 5: sensitivity to changes in s(Y) and P s (Y) Y, s(Y), f(Y) Red circle: 5, 0.398, 3.75 10-3 Green right triangle: 5, 0.44, 3.75 10-3 Blue left triangle: 5, 0.36, 3.75 10-3 Magenta up triangle:5, 0.398, 4.05 10-3 Black down triangle:5, 0.398, 3.45 10-3 Black curves are PDF at δ=32, 48, 64, 96Δ δ=32Δ δ=96Δ δ=32Δ δ=96Δ

21 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=96Δ s PsPs

22 3D fluid turbulence: fluctuations of v 2 P s (Y)

23 3D fluid turbulence: fluctuations of v 2 Computed PDFs by markers; raw PDFs by solid curves Red circles: δ=16∆; green squares: δ=32∆; Magenta diamonds: δ=64∆; blue triangles: δ=96∆

24 2D MHD simulations: fluctuations of B 2 s PsPs

25 Computed PDFs by markers; raw PDFs from simulations by solid curves Red circles: δ=32∆; green squares: δ=48∆; blue triangles: δ=96∆ Left panel for a large range of δB 2 ; right panel is an expanded view.

26 Solar wind data: fluctuations of B 2 Scaled PDF [solar wind data: Chang, Wu, and Podesta, AIP Conf Proc, 1039, 75 (2008)] From solar wind data P s (Y) used in the calculation

27 Solar wind data: fluctuations of B 2 ROMA spectrum from data s(Y) used in the calculation

28 Solar wind data: fluctuations of B 2 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.

29 Solar wind data: fluctuations of B 2 Using s=0.44 (monofractal) and the same P s (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

30 Conclusion ROMA is robust in the three cases studied here: 3D turbulent flows, 2D MHD simulation and solar wind data.


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