Complex networks for climate model evaluation with application to statistical versus dynamical modeling of South American climate

dc.bibliographicCitation.firstPage1567
dc.bibliographicCitation.issue5-6eng
dc.bibliographicCitation.lastPage1581
dc.bibliographicCitation.volume44
dc.contributor.authorFeldhoff, Jan H.
dc.contributor.authorLange, Stefan
dc.contributor.authorVolkholz, Jan
dc.contributor.authorDonges, Jonathan F.
dc.contributor.authorKurths, Jürgen
dc.contributor.authorGerstengarbe, Friedrich-Wilhelm
dc.date.accessioned2018-08-25T09:40:56Z
dc.date.available2019-06-26T17:18:48Z
dc.date.issued2014
dc.description.abstractIn this study we introduce two new node-weighted difference measures on complex networks as a tool for climate model evaluation. The approach facilitates the quantification of a model’s ability to reproduce the spatial covariability structure of climatological time series. We apply our methodology to compare the performance of a statistical and a dynamical regional climate model simulating the South American climate, as represented by the variables 2 m temperature, precipitation, sea level pressure, and geopotential height field at 500 hPa. For each variable, networks are constructed from the model outputs and evaluated against a reference network, derived from the ERA-Interim reanalysis, which also drives the models. We compare two network characteristics, the (linear) adjacency structure and the (nonlinear) clustering structure, and relate our findings to conventional methods of model evaluation. To set a benchmark, we construct different types of random networks and compare them alongside the climate model networks. Our main findings are: (1) The linear network structure is better reproduced by the statistical model statistical analogue resampling scheme (STARS) in summer and winter for all variables except the geopotential height field, where the dynamical model CCLM prevails. (2) For the nonlinear comparison, the seasonal differences are more pronounced and CCLM performs almost as well as STARS in summer (except for sea level pressure), while STARS performs better in winter for all variables.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/878
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/612
dc.language.isoengeng
dc.publisherHeidelberg : Springereng
dc.relation.doihttps://doi.org/10.1007/s00382-014-2182-9
dc.relation.ispartofseriesClimate Dynamics : Observational, Theoretical and Computational Research on the Climate System, Volume 44, Issue 5-6, Page 1567-1581eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectClimate model evaluationeng
dc.subjectComplex networkseng
dc.subjectSouth American climateeng
dc.subjectNetwork comparisoneng
dc.subject.ddc550eng
dc.titleComplex networks for climate model evaluation with application to statistical versus dynamical modeling of South American climateeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleClimate Dynamics : Observational, Theoretical and Computational Research on the Climate Systemeng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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