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dc.contributor.authorVannitsem, Stéphane
dc.date2017-03
dc.date.accessioned2018-07-02T11:46:32Z
dc.date.available2018-07-02T11:46:32Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/6982
dc.descriptionThe deterministic equations describing the dynamics of the atmosphere (and of the climate system) are known to display the property of sensitivity to initial conditions. In the ergodic theory of chaos, this property is usually quantified by computing the Lyapunov exponents. In this review, these quantifiers computed in a hierarchy of atmospheric models (coupled or not to an ocean) are analyzed, together with their local counterparts known as the local or finite-time Lyapunov exponents. It is shown in particular that the variability of the local Lyapunov exponents (corresponding to the dominant Lyapunov exponent) decreases when the model resolution increases. The dynamics of (finite-amplitude) initial condition errors in these models is also reviewed, and in general found to display a complicated growth far from the asymptotic estimates provided by the Lyapunov exponents. The implications of these results for operational (high resolution) atmospheric and climate modelling are also discussed.en_US
dc.languageengen_US
dc.publisherAIP Publishingen_US
dc.titlePredictability of large-scale atmospheric motions: Lyapunov exponents and error dynamicsen_US
dc.typeArticleen_US
dc.subject.frascatiPhysical sciencesen_US
dc.subject.frascatiEarth and related Environmental sciencesen_US
dc.audienceScientificen_US
dc.source.titleChaosen_US
dc.source.volume27en_US
dc.source.page032101en_US
Orfeo.peerreviewedYesen_US
dc.identifier.doihttps://doi.org/10.1063/1.4979042
dc.relation.belspo-projectBR/121/ A2/STOCHCLIMen_US


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