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dc.contributor.authorNicholls, Z.
dc.contributor.authorMeinshausen, M.
dc.contributor.authorLewis, J.
dc.contributor.authorSmith, C.J.
dc.contributor.authorForster, P.M.
dc.contributor.authorFuglestvedt, Jan S.
dc.contributor.authorRogelj, J.
dc.contributor.authorKikstra, J.S.
dc.contributor.authorRiahi, K.
dc.contributor.authorByers, E.
dc.date.accessioned2024-02-20T14:00:18Z
dc.date.available2024-02-20T14:00:18Z
dc.date.created2022-11-24T14:39:39Z
dc.date.issued2022
dc.identifier.citationGeophysical Research Letters. 2022, 49 (20), .en_US
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/3118722
dc.description.abstractThe IPCC's scientific assessment of the timing of net-zero emissions and 2030 emission reduction targets consistent with limiting warming to 1.5°C or 2°C rests on large scenario databases. Updates to this assessment, such as between the IPCC's Special Report on Global Warming of 1.5°C (SR1.5) of warming and the Sixth Assessment Report (AR6), are the result of intertwined, sometimes opaque, factors. Here we isolate one factor: the Earth System Model emulators used to estimate the global warming implications of scenarios. We show that warming projections using AR6-calibrated emulators are consistent, to within around 0.1°C, with projections made by the emulators used in SR1.5. The consistency is due to two almost compensating changes: the increase in assessed historical warming between SR1.5 (based on AR5) and AR6, and a reduction in projected warming due to improved agreement between the emulators' response to emissions and the assessment to which it is calibrated.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleChanges in IPCC Scenario Assessment Emulators Between SR1.5 and AR6 Unraveleden_US
dc.title.alternativeChanges in IPCC Scenario Assessment Emulators Between SR1.5 and AR6 Unraveleden_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber0en_US
dc.source.volume49en_US
dc.source.journalGeophysical Research Lettersen_US
dc.source.issue20en_US
dc.identifier.doi10.1029/2022GL099788
dc.identifier.cristin2080255
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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