A climate network perspective on the intertropical convergence zone

dc.bibliographicCitation.firstPage353eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.journalTitleEarth System Dynamics : ESDeng
dc.bibliographicCitation.lastPage366eng
dc.bibliographicCitation.volume12eng
dc.contributor.authorWolf, Frederik
dc.contributor.authorVoigt, Aiko
dc.contributor.authorDonner, Reik V.
dc.date.accessioned2022-01-18T13:05:09Z
dc.date.available2022-01-18T13:05:09Z
dc.date.issued2021
dc.description.abstractThe intertropical convergence zone (ITCZ) is an important component of the tropical rain belt. Climate models continue to struggle to adequately represent the ITCZ and differ substantially in its simulated response to climate change. Here we employ complex network approaches, which extract spatiotemporal variability patterns from climate data, to better understand differences in the dynamics of the ITCZ in state-of-the-art global circulation models (GCMs). For this purpose, we study simulations with 14 GCMs in an idealized slab-ocean aquaplanet setup from TRACMIP – the Tropical Rain belts with an Annual cycle and a Continent Model Intercomparison Project. We construct network representations based on the spatial correlation patterns of monthly surface temperature anomalies and study the zonal-mean patterns of different topological and spatial network characteristics. Specifically, we cluster the GCMs by means of the distributions of their zonal network measures utilizing hierarchical clustering. We find that in the control simulation, the distributions of the zonal network measures are able to pick up model differences in the tropical sea surface temperature (SST) contrast, the ITCZ position, and the strength of the Southern Hemisphere Hadley cell. Although we do not find evidence for consistent modifications in the network structure tracing the response of the ITCZ to global warming in the considered model ensemble, our analysis demonstrates that coherent variations of the global SST field are linked to ITCZ dynamics. This suggests that climate networks can provide a new perspective on ITCZ dynamics and model differences therein.eng
dc.description.fondsLeibniz_Fonds
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/7847
dc.identifier.urihttps://doi.org/10.34657/6888
dc.language.isoengeng
dc.publisherGöttingen : Copernicus Publ.eng
dc.relation.doihttps://doi.org/10.5194/esd-12-353-2021
dc.relation.essn2190-4987
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.otherAtmospheric temperatureeng
dc.subject.otherBeltseng
dc.subject.otherComplex networkseng
dc.subject.otherDynamicseng
dc.subject.otherGlobal warmingeng
dc.subject.otherHierarchical clusteringeng
dc.subject.otherOceanographyeng
dc.subject.otherRaineng
dc.subject.otherSurfaceeng
dc.subject.otherSurface propertieseng
dc.subject.otherSurface waterseng
dc.subject.otherTropicseng
dc.subject.otherGlobal circulation modeleng
dc.subject.otherIntertropical convergence zoneeng
dc.subject.otherModel inter comparisonseng
dc.subject.otherNetwork representationeng
dc.subject.otherSea surface temperature (SST)eng
dc.subject.otherSpatial correlationseng
dc.subject.otherSpatiotemporal variabilityeng
dc.subject.otherSurface temperature anomalieseng
dc.subject.otherClimate modelseng
dc.subject.otherair-sea interactioneng
dc.subject.otherclimate modelingeng
dc.subject.otherHadley celleng
dc.subject.otherintertropical convergence zoneeng
dc.subject.othersea surface temperatureeng
dc.subject.otherSouthern Hemisphereeng
dc.subject.otherspatiotemporal analysiseng
dc.subject.othersurface temperatureeng
dc.subject.otherwarmingeng
dc.titleA climate network perspective on the intertropical convergence zoneeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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