A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracy

A stochastic version of the Iterative Amplitude Adjusted Fourier Transform (IAAFT) algorithm is presented. This algorithm is able to generate so-called surrogate time series, which have the amplitude distribution and the power spectrum of measured time series or fields. The key difference between th...

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Main Authors: V. Venema, F. Ament, C. Simmer
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/13/321/2006/npg-13-321-2006.pdf
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spelling doaj-f1a1f22c9caa4b8d87b94ae34d99bce42020-11-25T00:56:28ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462006-01-01133321328A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracyV. VenemaF. AmentC. SimmerA stochastic version of the Iterative Amplitude Adjusted Fourier Transform (IAAFT) algorithm is presented. This algorithm is able to generate so-called surrogate time series, which have the amplitude distribution and the power spectrum of measured time series or fields. The key difference between the new algorithm and the original IAAFT method is the treatment of the amplitude adjustment: it is not performed for all values in each iterative step, but only for a fraction of the values. This new algorithm achieves a better accuracy, i.e. the power spectra of the measurement and its surrogate are more similar. We demonstrate the improvement by applying the IAAFT algorithm and the new one to 13 different test signals ranging from rain time series and 3-dimensional clouds to fractal time series and theoretical input. The improved accuracy can be important for generating high-quality geophysical time series and fields. The traditional application of the IAAFT algorithm is statistical nonlinearity testing. Reassuringly, we found that in most cases the accuracy of the original IAAFT algorithm is sufficient for this application.http://www.nonlin-processes-geophys.net/13/321/2006/npg-13-321-2006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author V. Venema
F. Ament
C. Simmer
spellingShingle V. Venema
F. Ament
C. Simmer
A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracy
Nonlinear Processes in Geophysics
author_facet V. Venema
F. Ament
C. Simmer
author_sort V. Venema
title A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracy
title_short A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracy
title_full A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracy
title_fullStr A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracy
title_full_unstemmed A Stochastic Iterative Amplitude Adjusted Fourier Transform algorithm with improved accuracy
title_sort stochastic iterative amplitude adjusted fourier transform algorithm with improved accuracy
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2006-01-01
description A stochastic version of the Iterative Amplitude Adjusted Fourier Transform (IAAFT) algorithm is presented. This algorithm is able to generate so-called surrogate time series, which have the amplitude distribution and the power spectrum of measured time series or fields. The key difference between the new algorithm and the original IAAFT method is the treatment of the amplitude adjustment: it is not performed for all values in each iterative step, but only for a fraction of the values. This new algorithm achieves a better accuracy, i.e. the power spectra of the measurement and its surrogate are more similar. We demonstrate the improvement by applying the IAAFT algorithm and the new one to 13 different test signals ranging from rain time series and 3-dimensional clouds to fractal time series and theoretical input. The improved accuracy can be important for generating high-quality geophysical time series and fields. The traditional application of the IAAFT algorithm is statistical nonlinearity testing. Reassuringly, we found that in most cases the accuracy of the original IAAFT algorithm is sufficient for this application.
url http://www.nonlin-processes-geophys.net/13/321/2006/npg-13-321-2006.pdf
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