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dc.contributor.authorRypdal, Kristoffer
dc.contributor.authorFredriksen, Hege-Beate
dc.date.accessioned2018-10-11T08:58:24Z
dc.date.available2018-10-11T08:58:24Z
dc.date.issued2017-12
dc.description.abstract<i>Introduction</i>: Scale invariance of natural variability of global surface temperatures is often interpreted as a signature of nonlinear dynamics. However, the observed scaling can be adequately explained by linear energy balance involving subsystems with different response times.en_US
dc.descriptionSource at <a href=https://doi.org/10.22498/pages.25.3.138> https://doi.org/10.22498/pages.25.3.138</a>.en_US
dc.identifier.citationRypdal, K. & Fredriksen, H. (2017). Scaling of global temperatures explained by linear energy balance models. Past Global Changes Magazine, 25(3), 138-139. https://doi.org/10.22498/pages.25.3.138en_US
dc.identifier.cristinIDFRIDAID 1555140
dc.identifier.doi10.22498/pages.25.3.138
dc.identifier.issn2411-605X
dc.identifier.urihttps://hdl.handle.net/10037/13944
dc.language.isoengen_US
dc.publisherPast Global Changes Magazineen_US
dc.relation.journalPast Global Changes Magazine
dc.rights.accessRightsopenAccessen_US
dc.subjectVDP::Mathematics and natural science: 400::Mathematics: 410en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410en_US
dc.titleScaling of global temperatures explained by linear energy balance modelsen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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