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Beyond fractals: surrogate time series and fields

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Beyond fractals: surrogate time series and fields Victor Venema and Clemens Simmer Meteorologisches Institut, Universit t Bonn, Germany Cloud measurements: – PowerPoint PPT presentation

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Title: Beyond fractals: surrogate time series and fields


1
Beyond fractals surrogate time series and fields
  • Victor Venema and Clemens Simmer
  • Meteorologisches Institut, Universität Bonn,
    Germany

Cloud measurements Susanne Crewell, Ulrich
Löhnert , Sebastian Schmidt Climate data
analysis Susanne Bachner, Alice Kapala, Henning
Rust Radiative transfer analysis Sebastián
Gimeno García , Anke Kniffka, Steffen Meyer,
Sebastian Schmidt 3D cloud modelling Andreas
Chlond, Frederick Chosson, Siegfried Raasch,
Michael Schroeter
2
Clouds are not spheres, mountains are not cones,
coastlines are not circles, and bark is not
smooth, nor does lightning travel in a straight
line
  • Benoit B. Mandelbrot in The Fractal Geometry of
    Nature (1983)

3
Fractals
  • Implied nature is fractal
  • Fractal, self-similar
  • Zoom in, looks the same
  • Structure measure is a power law of scale
  • Linear on a double logarithmic plot
  • Beginning of complex system sciences?
  • Structure on all scales
  • My experience good approximation for turbulence
    and stratiform clouds, but often see different
    signals

4
The great tragedy of science the slaying of a
beautiful theory by an ugly fact
  • Thomas Henry Huxley (18251895)

5
Content
  • Motivation What I do
  • Radiative transfer through clouds
  • Basic algorithm
  • Case study 3D clouds
  • Validation - 3D clouds
  • Structure functions of surrogates
  • Motivation compare multifractals
  • Conclusions
  • More information

6
Motivation Cloud structure
7
Motivation Cloud structure
8
Motivation Cloud structure
9
Motivation Cloud structure
10
Motivation
  • Can not measure a full 3D cloud field
  • Need 3D field for radiative transfer calculations
  • Can measure many (statistical) cloud properties
  • Generate cloud field based on statistics
    measurements
  • Nonlinear processes
  • Precise distribution
  • Non-local processes
  • E.g. power spectrum (autocorrelation function)
  • In geophysics you generally do not have full
    fields, but can estimate these two statistics

11
The iterative IAAFT algorithmSchreiber and
Schmitz
Time series
Distribution
Flow diagram
Time series
12
Case study
  • Two flights Stratocumulus, Cumulus
  • Airplane measurements
  • Liquid water content
  • Drop sizes
  • Triangle horizontal leg (horizontal structure)
  • A few ramps, for vertical profile
  • Three cloud generators
  • Irradiance modelling and measurement

13
Surrogates from airplane data
14
Three reconstructions
15
Irradiances stratocumulus
16
Irradiances cumulus
17
Validation 3D clouds
  • 3D models clouds -gt 3D surrogates
  • Full information, perfect statistics
  • Test if the statistics are good enough
  • The root-mean-square (RMS) differences are less
    than 1 percent (not significant)
  • Significant differences
  • Fourier surrogates distribution is important
  • PDF surrogates correlations are important
  • Trivial problem, but just numerical result

18
Validation time series
  • 1D climate time series and clouds
  • 4th order structure function
  • Surrogates more accurate (as multifractal)
  • Full information, perfect statistics
  • Numerical test how good the statistics are

19
(No Transcript)
20
Structure functions
  • Increment time series ?(x,l)?(tl)- ?(t)
  • SF(l,q) (1/N) S ?q
  • SF(l,2) is equivalent to auto-correlation
    function
  • Correlated time series SF increases with l
  • Higher q focuses on larger jumps

21
4th order SF cumulus
22
Error 4th order structure function
23
Generators
  • Iterative amplitude adjusted Fourier transform
    algorithm
  • Schreiber and Schmitz (1996, 2000)
  • Masters and Gurley (2003)
  • ...
  • Search algorithm
  • Simulated annealing (Schreiber, 1998)
  • Genetic algorithm (Venema, 2003)
  • Geostatistics stochastic simulation
  • Search algorithms
  • Gaussian distribution

24
Comparison
  • FARIMA modelling, Fourier methods
  • Gaussian distribution
  • AR modelling Multifractals
  • Idealised structure
  • Linear statistics
  • Kriging
  • Assimilation
  • Optimal estimation
  • Kernel smoothing
  • ....

25
Surrogates vs. multifractals
  • Measured power spectrum
  • Perfect distribution
  • Indirect over distribution
  • One specific measured field
  • Empirical studies
  • Power law fit
  • Indirect control distribution
  • Direct intermittence
  • Ensemble of fields
  • Theoretical studies

26
Cloud structure is not fractal
  • Scale breaks
  • Waves
  • Land sea mask

Satellite pictures Eumetsat
27
Land surface is not fractal
  • 15 Reasons the surface is not uni-fractal
    (Steward and McClean, 1985)
  • Fractal landscape have the same number of tops
    and pits
  • Glacial cirques has a narrow size range and size
    dependent shape

28
Conclusions
  • IAAFT algorithm can generate structures
  • Accurately
  • Flexibly
  • Efficiently
  • Many useful extensions are possible
  • Local values
  • Increment distributions
  • Downscaling

29
More information
  • Homepage
  • Papers, Matlab-programs, examples
  • http//www.meteo.uni-bonn.de/ venema/themes/surrog
    ates/
  • Google
  • surrogate clouds
  • multifractal surrogate time series
  • IAAFT in R Tools homepage Henning Rust
  • http//www.pik-potsdam.de/hrust/tools.html
  • IAAFT in Fortran (multivariate) search for
    TISEAN (Time SEries ANalysis)
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