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dc.contributor.authorPoltronieri, Anna
dc.contributor.authorBochow, Nils Ole Ronald
dc.contributor.authorAksamit, Nikolas Olson
dc.contributor.authorBoers, Niklas
dc.contributor.authorJakobsen, Per Kristen
dc.contributor.authorRypdal, Martin Wibe
dc.date.accessioned2024-07-03T07:46:08Z
dc.date.available2024-07-03T07:46:08Z
dc.date.issued2024-06-17
dc.description.abstractThe Arctic sea ice (ASI) is expected to decrease with further global warming. However, considerable uncertainty remains regarding the temperature range that would lead to a completely ice-free Arctic. Here, we combine satellite data and a large suite of models from the latest phase of the Coupled Model Intercomparison Project (CMIP6) to develop an empirical, observation-based projection of the September ASI area for increasing global mean surface temperature (GMST) values. This projection harnesses two simple linear relationships that are statistically supported by both observations and model data. First, we show that the September ASI area is linearly proportional to the area inside a specific northern hemisphere January–September mean temperature contour <i><b>T</i></b><sub>c</sub>. Second, we use observational data to show how zonally averaged temperatures have followed a positive linear trend relative to the GMST, consistent with Arctic amplification. To ensure the reliability of these observations throughout the rest of the century, we validate this trend by employing the CMIP6ensemble.Combiningthesetwolinearrelationships, we show that the September ASI area decrease will accelerate with respect to the GMST increase. Our analysis of observations and CMIP6 model data suggests a complete loss of the September ASI (area below 10<sup>6</sup> km<sup>2</sup>) for global warming between 1.5<sup>◦</sup>C and 2.2<sup>◦</sup>C above pre-industrial GMST levels.en_US
dc.descriptionSource at <a href=https://iopscience.iop.org/journal/1748-9326></a>.en_US
dc.identifier.citationPoltronieri, Bochow, Aksamit, Boers, Jakobsen, Rypdal. Arctic summer sea ice loss will accelerate in coming decades. Environmental Research Letters. 2024en_US
dc.identifier.cristinIDFRIDAID 2279089
dc.identifier.doi10.1088/1748-9326/ad5194
dc.identifier.issn1748-9326
dc.identifier.urihttps://hdl.handle.net/10037/34052
dc.language.isoengen_US
dc.publisherIOS Pressen_US
dc.relation.journalEnvironmental Research Letters
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/820970/Norway/Tipping Points in the Earth System/TiPES/en_US
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/956170/Norway/Multiscales and Critical Transitions in the Earth System/CriticalEarth/en_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2024 The Author(s)en_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0en_US
dc.rightsAttribution 4.0 International (CC BY 4.0)en_US
dc.titleArctic summer sea ice loss will accelerate in coming decadesen_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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Attribution 4.0 International (CC BY 4.0)
Except where otherwise noted, this item's license is described as Attribution 4.0 International (CC BY 4.0)