Permafrost is warming at a global scale
By B. Biskaborn, Sharon L Smith, J. Noetzli, H. Matthes, G. Vieira, D. Streletskiy, P. Schoeneich, Vladimir E. Romanovsky, A. Lewkowicz, A. Abramov and 38 more. Nature Communications, 2019
1,572 citations recorded by the source corpus.
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. Climate change strongly impacts regions in high latitudes and altitudes that store high amounts of carbon in yet frozen ground. Here the authors show that the consequence of these changes is global warming of permafrost at depths greater than 10 m in the Northern Hemisphere, in mountains, and in Antarctica.
Subfields: Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/3f1f4fff514345d449a197597b1e0d75e19b140a
Citations in the corpus
- Large stocks of peatland carbon and nitrogen are vulnerable to permafrost thaw (2020, neutral): “Presently, broad-scale permafrost thaw is evident at +1 °C above preindustrial temperatures (67), and the effects on permafrost peatland extent and GHG release have already been observed for several decades (56, 68, 69).”