Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric Model

We search for the signature of universal properties of extreme events, theoretically predicted for Axiom A flows, in a chaotic and high-dimensional dynamical system. We study the convergence of GEV (Generalized Extreme Value) and GP (Generalized Pareto) shape parameter estimates to the theoretical v...

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Main Authors: Vera Melinda Gálfi, Tamás Bódai, Valerio Lucarini
Format: Article
Language:English
Published: Hindawi-Wiley 2017-01-01
Series:Complexity
Online Access:http://dx.doi.org/10.1155/2017/5340858
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spelling doaj-0a02ceb02c77492eae5a613433a70ede2020-11-25T01:14:56ZengHindawi-WileyComplexity1076-27871099-05262017-01-01201710.1155/2017/53408585340858Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric ModelVera Melinda Gálfi0Tamás Bódai1Valerio Lucarini2Meteorological Institute, CEN, University of Hamburg, Hamburg, GermanyDepartment of Mathematics and Statistics, University of Reading, Reading, UKMeteorological Institute, CEN, University of Hamburg, Hamburg, GermanyWe search for the signature of universal properties of extreme events, theoretically predicted for Axiom A flows, in a chaotic and high-dimensional dynamical system. We study the convergence of GEV (Generalized Extreme Value) and GP (Generalized Pareto) shape parameter estimates to the theoretical value, which is expressed in terms of the partial information dimensions of the attractor. We consider a two-layer quasi-geostrophic atmospheric model of the mid-latitudes, adopt two levels of forcing, and analyse the extremes of different types of physical observables (local energy, zonally averaged energy, and globally averaged energy). We find good agreement in the shape parameter estimates with the theory only in the case of more intense forcing, corresponding to a strong chaotic behaviour, for some observables (the local energy at every latitude). Due to the limited (though very large) data size and to the presence of serial correlations, it is difficult to obtain robust statistics of extremes in the case of the other observables. In the case of weak forcing, which leads to weaker chaotic conditions with regime behaviour, we find, unsurprisingly, worse agreement with the theory developed for Axiom A flows.http://dx.doi.org/10.1155/2017/5340858
collection DOAJ
language English
format Article
sources DOAJ
author Vera Melinda Gálfi
Tamás Bódai
Valerio Lucarini
spellingShingle Vera Melinda Gálfi
Tamás Bódai
Valerio Lucarini
Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric Model
Complexity
author_facet Vera Melinda Gálfi
Tamás Bódai
Valerio Lucarini
author_sort Vera Melinda Gálfi
title Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric Model
title_short Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric Model
title_full Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric Model
title_fullStr Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric Model
title_full_unstemmed Convergence of Extreme Value Statistics in a Two-Layer Quasi-Geostrophic Atmospheric Model
title_sort convergence of extreme value statistics in a two-layer quasi-geostrophic atmospheric model
publisher Hindawi-Wiley
series Complexity
issn 1076-2787
1099-0526
publishDate 2017-01-01
description We search for the signature of universal properties of extreme events, theoretically predicted for Axiom A flows, in a chaotic and high-dimensional dynamical system. We study the convergence of GEV (Generalized Extreme Value) and GP (Generalized Pareto) shape parameter estimates to the theoretical value, which is expressed in terms of the partial information dimensions of the attractor. We consider a two-layer quasi-geostrophic atmospheric model of the mid-latitudes, adopt two levels of forcing, and analyse the extremes of different types of physical observables (local energy, zonally averaged energy, and globally averaged energy). We find good agreement in the shape parameter estimates with the theory only in the case of more intense forcing, corresponding to a strong chaotic behaviour, for some observables (the local energy at every latitude). Due to the limited (though very large) data size and to the presence of serial correlations, it is difficult to obtain robust statistics of extremes in the case of the other observables. In the case of weak forcing, which leads to weaker chaotic conditions with regime behaviour, we find, unsurprisingly, worse agreement with the theory developed for Axiom A flows.
url http://dx.doi.org/10.1155/2017/5340858
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AT tamasbodai convergenceofextremevaluestatisticsinatwolayerquasigeostrophicatmosphericmodel
AT valeriolucarini convergenceofextremevaluestatisticsinatwolayerquasigeostrophicatmosphericmodel
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