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Papers on “permafrost thaw methane climate feedback”

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1. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change

   Eric A. Davidson, Ivan A. Janssens · 2006 · Nature · 7,078 cites

2. Climate change and the permafrost carbon feedback

   Edward A. G. Schuur, A. David McGuire, Christina Schädel, et al. · 2015 · Nature · 3,917 cites

3. Permafrost is warming at a global scale

   Boris K. Biskaborn, Sharon L. Smith, Jeannette Noetzli, et al. · 2019 · Nature Communications · 2,144 cites

   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 warm

4. Methane bubbling from Siberian thaw lakes as a positive feedback to climate warming

   K. M. Walter, S. A. Zimov, Jeffrey P. Chanton, et al. · 2006 · Nature · 1,116 cites

5. Carbon release through abrupt permafrost thaw

   Merritt R. Turetsky, Benjamin W. Abbott, Miriam C. Jones, et al. · 2020 · Nature Geoscience · 1,019 cites

6. Permafrost carbon-climate feedbacks accelerate global warming

   Charles D. Koven, Bruno Ringeval, Pierre Friedlingstein, et al. · 2011 · Proceedings of the National Academy of Sciences · 1,003 cites

   Permafrost soils contain enormous amounts of organic carbon, which could act as a positive feedback to global climate change due to enhanced respiration rates with warming. We have used a terrestrial ecosystem model that includes permafrost carbon dynamics, inhibition of respiration in frozen soil layers, vertical mixing of soil carbon from surface to permafrost layers, and CH(4) emissions from flooded areas, and which better matches new circumpolar inventories of soil carbon stocks, to explore the potential for carbon-climate feedbacks at high latitudes. Contrary to model results for the Intergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4), when permafrost processes

7. Permafrost carbon emissions in a changing Arctic

   Kimberley Miner, Merritt R. Turetsky, Edward Malina, et al. · 2022 · Nature Reviews Earth & Environment · 559 cites

8. Methane dynamics regulated by microbial community response to permafrost thaw

   C. K. McCalley, Ben J. Woodcroft, Suzanne B. Hodgkins, et al. · 2014 · Nature · 472 cites