Permafrost is warming at a global scale

dc.contributor.author
Biskaborn, Boris K.
dc.contributor.author
Smith, Sharon L.
dc.contributor.author
Noetzli, Jeannette
dc.contributor.author
Matthes, Heidrun
dc.contributor.author
Vieira, Gonçalo
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Streletskiy, Dmitry A.
dc.contributor.author
Schoeneich, Philippe
dc.contributor.author
Romanovsky, Vladimir E.
dc.contributor.author
Lewkowicz, Antoni G.
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Abramov, Andrey Y.
dc.contributor.author
Allard, Michel
dc.contributor.author
Boike, Julia
dc.contributor.author
Cable, William L.
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Christiansen, Hanne H.
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Delaloye, Reynald
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Diekmann, Bernhard
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Drozdov, Dmitry
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Etzelmüller, Bernd
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Grosse, Guido
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Guglielmin, Mauro
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Ingeman-Nielsen, Thomas
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Isaksen, Ketil
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Ishikawa, Mamoru
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Johansson, Margareta
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Johannsson, Halldor
dc.contributor.author
Joo, Anseok
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Kaverin, Dmitry
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Kholodov, Alexander
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Konstantinov, Pavel
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Kröger, Tim
dc.contributor.author
Lambiel, Christophe
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Lanckman, Jean-Pierre
dc.contributor.author
Luo, Dongliang
dc.contributor.author
Malkova, Galina
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Meiklejohn, Ian
dc.contributor.author
Moskalenko, Natalia
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Oliva Franganillo, Marc
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Phillips, Marcia
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Ramos, Miguel
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Sannel, A. Britta K.
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Sergeev, Dmitrii
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Seybold, Cathy
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Skryabin, Pavel
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Vasiliev, Alexander
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Wu, Qingbai
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Yoshikawa, Kenji
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Zheleznyak, Mikhail
dc.contributor.author
Lantuit, Hugues
dc.date.issued
2019-01-22T11:16:58Z
dc.date.issued
2019-01-22T11:16:58Z
dc.date.issued
2019-01-16
dc.date.issued
2019-01-22T11:16:58Z
dc.identifier
2041-1723
dc.identifier
https://hdl.handle.net/2445/127505
dc.identifier
674962
dc.description.abstract
Permafrost warming has the potential to amplify global climate change, because when frozen sediments thaw it unlocks soil organic carbon. Yet to date, no globally consistent assessment of permafrost temperature change has been compiled. Here we use a global data set of permafrost temperature time series from the Global Terrestrial Network for Permafrost to evaluate temperature change across permafrost regions for the period since the International Polar Year (2007-2009). During the reference decade between 2007 and 2016, ground temperature near the depth of zero annual amplitude in the continuous permafrost zone increased by 0.39 ± 0.15 °C. Over the same period, discontinuous permafrost warmed by 0.20 ± 0.10 °C. Permafrost in mountains warmed by 0.19 ± 0.05 °C and in Antarctica by 0.37 ± 0.10 °C. Globally, permafrost temperature increased by 0.29 ± 0.12 °C. The observed trend follows the Arctic amplification of air temperature increase in the Northern Hemisphere. In the discontinuous zone, however, ground warming occurred due to increased snow thickness while air temperature remained statistically unchanged.
dc.format
11 p.
dc.format
application/pdf
dc.format
application/pdf
dc.language
eng
dc.publisher
Nature Publishing Group
dc.relation
Reproducció del document publicat a: https://doi.org/10.1038/s41467-018-08240-4
dc.relation
Nature Communications, 2019, vol. 10, num. 1, p. 264
dc.relation
https://doi.org/10.1038/s41467-018-08240-4
dc.relation
info:eu-repo/grantAgreement/EC/H2020/773421/EU//Nunataryuk
dc.rights
cc-by (c) Biskaborn, Boris K. et al., 2019
dc.rights
http://creativecommons.org/licenses/by/3.0/es
dc.rights
info:eu-repo/semantics/openAccess
dc.source
Articles publicats en revistes (Geografia)
dc.subject
Canvi climàtic
dc.subject
Sòls gelats
dc.subject
Geotèrmia
dc.subject
Terra
dc.subject
Escalfament global
dc.subject
Climatic change
dc.subject
Frozen ground
dc.subject
Earth temperature
dc.subject
Earth
dc.subject
Global warming
dc.title
Permafrost is warming at a global scale
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/publishedVersion


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