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dc.contributor.authorMüller, Rhonda C.
dc.contributor.authorKim, Jin-Soo
dc.contributor.authorLee, Hanna
dc.contributor.authorMuri, Helene
dc.contributor.authorTjiputra, Jerry
dc.contributor.authorYoon, Jin-Ho
dc.contributor.authorSchaepman-Strub, Gabriela
dc.date.accessioned2024-04-11T11:09:47Z
dc.date.available2024-04-11T11:09:47Z
dc.date.created2024-04-09T11:30:36Z
dc.date.issued2024
dc.identifier.issn2662-4435
dc.identifier.urihttps://hdl.handle.net/11250/3126057
dc.description.abstractRadiative forcing geoengineering is discussed as an intermediate solution to partially offset greenhouse gas-driven warming by altering the Earth’s energy budget. Here we use an Earth System Model to analyse the response in Arctic temperatures to radiative geoengineering applied under the representative concentration pathway 8.5 to decrease the radiative forcing to that achieved under the representative concentration pathway 4.5. The three methods Stratospheric Aerosol Injection, Marine Cloud Brightening, and Cirrus Cloud Thinning, mitigate the global mean temperature rise, however, under our experimental designs, the projected Arctic temperatures are higher than if the same temperature was achieved under emission mitigation. The maximum temperature increase under Cirrus Cloud Thinning and Marine Cloud Brightening is linked to carbon dioxide plant physiological forcing, shifting the system into climatic conditions favouring the development of fires. Under Stratospheric Aerosol Injection, the Arctic land with temperatures permanently below freezing decreased by 7.8% compared to the representative concentration pathway 4.5. This study concludes that these specific radiative forcing geoengineering designs induce less efficient cooling of the Arctic than the global mean and worsen extreme conditions compared to the representative concentration pathway 4.5.en_US
dc.language.isoengen_US
dc.publisherSpringer Natureen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleRadiative forcing geoengineering causes higher risk of wildfires and permafrost thawing over the Arctic regionsen_US
dc.title.alternativeRadiative forcing geoengineering causes higher risk of wildfires and permafrost thawing over the Arctic regionsen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.source.volume5en_US
dc.source.journalCommunications Earth & Environmenten_US
dc.source.issue180en_US
dc.identifier.doi10.1038/s43247-024-01329-3
dc.identifier.cristin2260187
dc.relation.projectSigma2: NS2345Ken_US
dc.relation.projectSigma2: nn9182ken_US
dc.relation.projectSigma2: NS9033Ken_US
dc.relation.projectSigma2: nn9448ken_US
dc.relation.projectNorges forskningsråd: 229760en_US
dc.relation.projectSigma2: NS9576Ken_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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