Permafrost is warming at a global scale

Многомасштабное потепление вечной мерзлоты
Mauro Guglielmin, V. E. Romanovsky, Qingbai Wu, Bernd Etzelmüller, Reynald Delaloye, Julia Boike, Kenji Yoshikawa, Sharon L. Smith, Marc Oliva, Bernhard Diekmann, Miguel Ramos, Boris K. Biskaborn, Jeannette Noetzli, Heidrun Matthes, Gonçalo Vieira, D. A. Streletskiy, Philippe Schoeneich, Antoni G. Lewkowicz, Andrey Abramov, Michel Allard, William Cable, Hanne H. Christiansen, Dmitry Drozdov, Guido Grosse, Thomas Ingeman‐Nielsen, Ketil Isaksen, Mamoru Ishikawa, Margareta Johansson, Halldór Jóhannsson, Anseok Joo, Dmitry Kaverin, Alexander Kholodov, Pavel Konstantinov, Tim Kröger, Christophe Lambiel, Jean-Pierre Lanckman, Dongliang Luo, Г. В. Малкова, Ian Meiklejohn, NATALIIA MOSKALENKO, Marcia Phillips, A. Britta K. Sannel, D. O. Sergeev, C. A. Seybold, Pavel N Skryabin, Alexander Vasiliev, M. N. Zheleznyak, Hugues Lantuit, Natalia Moskalenko
2019-01-10

Arctic amplificationGlobal Terrestrial Network for Permafrostcontinuous vs discontinuous permafrostground temperature changepermafrost warming
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.
1
Antarctic permafrost warmed by 0.37 ± 0.10 °C during the reference decade.
2
Continuous permafrost warmed by 0.39 ± 0.15 °C near the depth of zero annual amplitude between 2007 and 2016.
3
Discontinuous permafrost warmed by 0.20 ± 0.10 °C over the same period.
4
Global permafrost temperature increased by 0.29 ± 0.12 °C for the period since the International Polar Year (2007–2009) evaluated over the reference decade 2007–2016.
5
In discontinuous permafrost zones, ground warming was driven by increased snow thickness despite statistically unchanged air temperatures.
6
Mountain permafrost warmed by 0.19 ± 0.05 °C between 2007 and 2016.
7
Observed permafrost warming follows Arctic amplification of Northern Hemisphere air temperature increases.

Permafrost regions worldwide (continuous, discontinuous, mountain, and Antarctic permafrost) as measured by ground temperature time series

Observed changes and trends in permafrost ground temperature since 2007–2009, including regional warming magnitudes and drivers (e.g., Arctic air-temperature amplification and snow-thickness effects)

Publication Details
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2019-01-10
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Authors
Mauro Guglielmin
V. E. Romanovsky
Qingbai Wu
Bernd Etzelmüller
Reynald Delaloye
Julia Boike
Kenji Yoshikawa
Sharon L. Smith
Marc Oliva
Bernhard Diekmann
Miguel Ramos
Boris K. Biskaborn
Jeannette Noetzli
Heidrun Matthes
Gonçalo Vieira
D. A. Streletskiy
Philippe Schoeneich
Antoni G. Lewkowicz
Andrey Abramov
Michel Allard
William Cable
Hanne H. Christiansen
Dmitry Drozdov
Guido Grosse
Thomas Ingeman‐Nielsen
Ketil Isaksen
Mamoru Ishikawa
Margareta Johansson
Halldór Jóhannsson
Anseok Joo
Dmitry Kaverin
Alexander Kholodov
Pavel Konstantinov
Tim Kröger
Christophe Lambiel
Jean-Pierre Lanckman
Dongliang Luo
Г. В. Малкова
Ian Meiklejohn
NATALIIA MOSKALENKO
Marcia Phillips
A. Britta K. Sannel
D. O. Sergeev
C. A. Seybold
Pavel N Skryabin
Alexander Vasiliev
M. N. Zheleznyak
Hugues Lantuit
Natalia Moskalenko
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