Taking some heat off the NDCs? The limited potential of additional short-lived climate forcers’ mitigation

dc.bibliographicCitation.firstPage1443eng
dc.bibliographicCitation.issue3eng
dc.bibliographicCitation.lastPage1461eng
dc.bibliographicCitation.volume163eng
dc.contributor.authorHarmsen, Mathijs
dc.contributor.authorFricko, Oliver
dc.contributor.authorHilaire, Jérôme
dc.contributor.authorvan Vuuren, Detlef P.
dc.contributor.authorDrouet, Laurent
dc.contributor.authorDurand-Lasserve, Olivier
dc.contributor.authorFujimori, Shinichiro
dc.contributor.authorKeramidas, Kimon
dc.contributor.authorKlimont, Zbigniew
dc.contributor.authorLuderer, Gunnar
dc.contributor.authorAleluia Reis, Lara
dc.contributor.authorRiahi, Keywan
dc.contributor.authorSano, Fuminori
dc.contributor.authorSmith, Steven J.
dc.date.accessioned2021-09-21T05:59:19Z
dc.date.available2021-09-21T05:59:19Z
dc.date.issued2019
dc.description.abstractSeveral studies have shown that the greenhouse gas reduction resulting from the current nationally determined contributions (NDCs) will not be enough to meet the overall targets of the Paris Climate Agreement. It has been suggested that more ambition mitigations of short-lived climate forcer (SLCF) emissions could potentially be a way to reduce the risk of overshooting the 1.5 or 2 °C target in a cost-effective way. In this study, we employ eight state-of-the-art integrated assessment models (IAMs) to examine the global temperature effects of ambitious reductions of methane, black and organic carbon, and hydrofluorocarbon emissions. The SLCFs measures considered are found to add significantly to the effect of the NDCs on short-term global mean temperature (GMT) (in the year 2040: − 0.03 to − 0.15 °C) and on reducing the short-term rate-of-change (by − 2 to 15%), but only a small effect on reducing the maximum temperature change before 2100. This, because later in the century under assumed ambitious climate policy, SLCF mitigation is maximized, either directly or indirectly due to changes in the energy system. All three SLCF groups can contribute to achieving GMT changes. © 2019, The Author(s).eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6866
dc.identifier.urihttps://doi.org/10.34657/5913
dc.language.isoengeng
dc.publisherDordrecht [u.a.] : Springer Science + Business Media B.Veng
dc.relation.doihttps://doi.org/10.1007/s10584-019-02436-3
dc.relation.essn1573-1480
dc.relation.ispartofseriesClimatic change 163 (2020), Nr. 3eng
dc.relation.issn0165-0009
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectCost effectivenesseng
dc.subjectGreenhouse gaseseng
dc.subjectClimate agreementeng
dc.subjectEnergy systemseng
dc.subjectGlobal-mean temperatureeng
dc.subjectGreenhouse gas reductionseng
dc.subjectHydrofluorocarbonseng
dc.subjectIntegrated assessment modelseng
dc.subjectMaximum temperatureeng
dc.subjectState of the arteng
dc.subjectOrganic carboneng
dc.subject.ddc550eng
dc.titleTaking some heat off the NDCs? The limited potential of additional short-lived climate forcers’ mitigationeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleClimatic changeeng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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