Active layer and permafrost thermal regimes in the ice-free areas of Antarctica

dc.contributor.authorHrbacek, Filip
dc.contributor.authorOliva, Marc
dc.contributor.authorHansen, Christel
dc.contributor.authorBalks, Megan
dc.contributor.authorO'Neill, Tanya Ann
dc.contributor.authorDe Pablo, Miguel Angel
dc.contributor.authorPonti, Stefano
dc.contributor.authorRamos, Miguel
dc.contributor.authorVieira, Goncalo
dc.contributor.authorAbramov, Andrey
dc.contributor.authorKaplan Pastírikova, Lucia
dc.contributor.authorGuglielmin, Mauro
dc.contributor.authorGoyanes, Gabriel
dc.contributor.authorFrancelino, Marcio Rocha
dc.contributor.authorSchaefer, Carlos
dc.contributor.authorLacelle, Denis
dc.date.accessioned2023-06-28T06:04:35Z
dc.date.issued2023-07
dc.descriptionDATA AVAILABILITY : Data will be made available on request.en_US
dc.description.abstractPlease read abstract in the article.en_US
dc.description.departmentGeography, Geoinformatics and Meteorologyen_US
dc.description.embargo2024-06-07
dc.description.librarianhj2023en_US
dc.description.sponsorshipCzech Scientific Foundation, Masaryk University internal project and Czech Antarctic Research Programme funded by MEYS of Czech Republic; project NUNANTAR (Fundação para a Ciência e Tecnologia of Portugal) and the research groups ANTALP (Antarctic, Arctic, Alpine Environments) funded by the Agència de Gestió d'Ajuts Universitaris i de Recerca of the Government of Catalonia; PNRA (Programma Nazionale di Ricerca in Antartica) for the logistical and financial support in Continental Antarctica, Antarctic Peninsula and in Signy Island.en_US
dc.description.urihttps://www.elsevier.com/locate/earscireven_US
dc.identifier.citationHrbáček, F., Oliva, M., Hansen, C. et al. 2023, 'Active layer and permafrost thermal regimes in the ice-free areas of Antarctica', Earth-Science Reviews, vol. 242, art. 104458, pp. 1-29, doi : 10.1016/j.earscirev.2023.104458.en_US
dc.identifier.issn0012-8252 (print)
dc.identifier.issn1872-6828 (online)
dc.identifier.other10.1016/j.earscirev.2023.104458
dc.identifier.urihttp://hdl.handle.net/2263/91232
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.rights© 2023 Elsevier. All rights reserved. Notice : this is the author’s version of a work that was accepted for publication in Earth-Science Reviews. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. A definitive version was subsequently published in Earth-Science Reviews, vol. 242, art. 104458, pp. 1-29, doi : 10.1016/j.earscirev.2023.104458.en_US
dc.subjectGround thermal regimeen_US
dc.subjectActive layer thicknessen_US
dc.subjectClimate changeen_US
dc.subjectAntarctic ice-free environmenten_US
dc.subjectCryosolsen_US
dc.subjectGelisolsen_US
dc.subjectPermafrosten_US
dc.subjectSDG-13: Climate actionen_US
dc.titleActive layer and permafrost thermal regimes in the ice-free areas of Antarcticaen_US
dc.typePostprint Articleen_US

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