2017
DOI: 10.1155/2017/3076810
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Independent Subspace Analysis of the Sea Surface Temperature Variability: Non-Gaussian Sources and Sensitivity to Sampling and Dimensionality

Abstract: We propose an expansion of multivariate time-series data into maximally independent source subspaces. The search is made among rotations of prewhitened data which maximize non-Gaussianity of candidate sources. We use a tensorial invariant approximation of the multivariate negentropy in terms of a linear combination of squared coskewness and cokurtosis. By solving a high-order singular value decomposition problem, we extract the axes associated with most non-Gaussianity. Moreover, an estimate of the Gaussian su… Show more

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Cited by 11 publications
(8 citation statements)
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“…In geophysical applications EOF analysis have been applied to spatio-temporal climate data to obtain data-driven models [10] and have been further developed in different directions like independent subspace analysis [11], linear and nonlinear dynamical mode decomposition [12], [13] to name only a few.…”
Section: A Related Workmentioning
confidence: 99%
See 1 more Smart Citation
“…In geophysical applications EOF analysis have been applied to spatio-temporal climate data to obtain data-driven models [10] and have been further developed in different directions like independent subspace analysis [11], linear and nonlinear dynamical mode decomposition [12], [13] to name only a few.…”
Section: A Related Workmentioning
confidence: 99%
“…Furthermore we now also get an estimate for the parameter n, which we call n. In order to explain the idea behind this estimation procedure, however, we first return to the original u i and v i from ( 9) and (11). In consequence of the linear independence of {u 1 , .…”
Section: ) Estimation Of the Parameter Nmentioning
confidence: 99%
“…Another way to obtain these derivatives is to define random variable Z * τ = u(Z τ ) = Z τ / 1 + Z 2 τ and using (14) with Z τ and µ k = E(Z τ ) replaced by Z * τ and µ * k = E{(Z * τ ) k }, respectively. Thus, we obtain the series expansion:…”
Section: Modified Skew-normal Distributionmentioning
confidence: 99%
“…Whereas external orbital variations are believed to be the dominant driving force for macroclimate (on millennial time scales), weather, macro-weather (Lovejoy, 2018) and climate variations (on shorter time scales) are mainly the result of complex nonlinear interactions between very many degrees-of-freedom (Sura and Hannachi, 2015) and also due to many climate subcomponents with different time scales The atmospheric (and climate) system is an excellent example of highdimensional and highly complex dynamical system. One outstanding and ubiquitous feature of the large scale (and low frequency) atmospheric (and climate) variability is non-Gaussianity (Franzke et al, 2007;Proistosescu et al, 2016;Pires and Hannachi, 2017;Hannachi and Iqbal, 2019). For instance, Sura and Sardeshmukh (2008) show that sea surface temperature (SST) has non-Gaussian probability distribution function (PDF) with particular tail extrema.…”
Section: Introductionmentioning
confidence: 99%