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dc.contributor.authorSiegert, M
dc.date.accessioned2024-07-17T15:50:43Z
dc.date.issued2024-07-14
dc.date.updated2024-07-17T07:00:13Z
dc.description.abstractSatellite observations of the Antarctic surface since the 1990s, coupled with geophysical surveys ofthe flow and form of its giant ice sheet, have revealed accelerating loss of ice to the oceans. This,coupled with a reduction in floating sea ice surrounding the continent and the occurrence ofunprecedented heatwaves, point to a continent being changed irreversibly by fossil-fuel burningand the global heating that results. A changing Antarctic continent will have global consequences,including sea level rise of possibly more than 1 meter in this century (and much more afterward)and by a reduced ability to naturally reflect incoming solar energy—which would lead to furtherheating by absorption on land and at sea as the ice pack retreats.en_GB
dc.format.extent239-245
dc.identifier.citationVol. 80, No. 4, pp. 239-245en_GB
dc.identifier.doihttps://doi.org/10.1080/00963402.2024.2364507
dc.identifier.urihttp://hdl.handle.net/10871/136749
dc.identifierORCID: 0000-0002-0090-4806 (Siegert, Martin)
dc.identifierScopusID: 7004861061 (Siegert, Martin)
dc.identifierResearcherID: A-3826-2008 | M-9939-2019 (Siegert, Martin)
dc.language.isoenen_GB
dc.publisherRoutledgeen_GB
dc.rights© 2024 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The terms on which this article has been published allow the posting of the Accepted Manuscript in a repository by the author(s) or with their consent.en_GB
dc.subjectAntarcticaen_GB
dc.subjectclimate changeen_GB
dc.subjectgeophysicsen_GB
dc.subjectglaciologyen_GB
dc.subjectsea levelen_GB
dc.subjectmitigationen_GB
dc.titleHow we know Antarctica is rapidly losing more iceen_GB
dc.typeArticleen_GB
dc.date.available2024-07-17T15:50:43Z
dc.identifier.issn0096-3402
dc.descriptionThis is the final version. Available from Routledge via the DOI in this record. en_GB
dc.identifier.eissn1938-3282
dc.identifier.journalBulletin of the Atomic Scientistsen_GB
dc.relation.ispartofBulletin of the Atomic Scientists, 80(4)
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2024-05-31
dcterms.dateSubmitted2024-05-05
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2024-07-14
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2024-07-17T07:00:17Z
refterms.versionFCDAM
refterms.dateFOA2024-07-17T15:50:51Z
refterms.panelBen_GB
refterms.dateFirstOnline2024-07-14
exeter.rights-retention-statementYes


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© 2024 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The terms on which this article has been published allow the posting of the Accepted Manuscript in a repository by the author(s) or with their consent.
Except where otherwise noted, this item's licence is described as © 2024 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The terms on which this article has been published allow the posting of the Accepted Manuscript in a repository by the author(s) or with their consent.