Characterizing the evolution of climate networks

dc.bibliographicCitation.firstPage705eng
dc.bibliographicCitation.issue3eng
dc.bibliographicCitation.volume21eng
dc.contributor.authorTupikina, L.
dc.contributor.authorRehfeld, K.
dc.contributor.authorMolkenthin, N.
dc.contributor.authorStolbova, V.
dc.contributor.authorMarwan, N.
dc.contributor.authorKurths, J.
dc.date.accessioned2020-08-01T15:36:11Z
dc.date.available2020-08-01T15:36:11Z
dc.date.issued2014
dc.description.abstractComplex network theory has been successfully applied to understand the structural and functional topology of many dynamical systems from nature, society and technology. Many properties of these systems change over time, and, consequently, networks reconstructed from them will, too. However, although static and temporally changing networks have been studied extensively, methods to quantify their robustness as they evolve in time are lacking. In this paper we develop a theory to investigate how networks are changing within time based on the quantitative analysis of dissimilarities in the network structure. Our main result is the common component evolution function (CCEF) which characterizes network development over time. To test our approach we apply it to several model systems, ErdA's-Rényi networks, analytically derived flow-based networks, and transient simulations from the START model for which we control the change of single parameters over time. Then we construct annual climate networks from NCEP/NCAR reanalysis data for the Asian monsoon domain for the time period of 1970-2011 CE and use the CCEF to characterize the temporal evolution in this region. While this real-world CCEF displays a high degree of network persistence over large time lags, there are distinct time periods when common links break down. This phasing of these events coincides with years of strong El Niño/Southern Oscillation phenomena, confirming previous studies. The proposed method can be applied for any type of evolving network where the link but not the node set is changing, and may be particularly useful to characterize nonstationary evolving systems using complex networks.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/5287
dc.identifier.urihttps://doi.org/10.34657/3916
dc.language.isoengeng
dc.publisherGöttingen : Copernicus GmbHeng
dc.relation.doihttps://doi.org/10.5194/npg-21-705-2014
dc.relation.ispartofseriesNonlinear Processes in Geophysics 21 (2014), Nr. 3eng
dc.relation.issn1023-5809
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectclimate modelingeng
dc.subjectclimate predictioneng
dc.subjectmonsooneng
dc.subjectnetwork analysiseng
dc.subjectnumerical modeleng
dc.subjectquantitative analysiseng
dc.subjecttemporal evolutioneng
dc.subjecttopologyeng
dc.subject.ddc550eng
dc.titleCharacterizing the evolution of climate networkseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleNonlinear Processes in Geophysicseng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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