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Large loss of CO2 in winter observed across the northern permafrost region

  • Susan M. Natali
  • , Jennifer D. Watts
  • , Brendan M. Rogers
  • , Stefano Potter
  • , Sarah M. Ludwig
  • , Anne Katrin Selbmann
  • , Patrick F. Sullivan
  • , Benjamin W. Abbott
  • , Kyle A. Arndt
  • , Leah Birch
  • , Mats P. Björkman
  • , A. Anthony Bloom
  • , Gerardo Celis
  • , Torben R. Christensen
  • , Casper T. Christiansen
  • , Roisin Commane
  • , Elisabeth J. Cooper
  • , Patrick Crill
  • , Claudia Czimczik
  • , Sergey Davydov
  • Jinyang Du, Jocelyn E. Egan, Bo Elberling, Eugenie S. Euskirchen, Thomas Friborg, Hélène Genet, Mathias Göckede, Jordan P. Goodrich, Paul Grogan, Manuel Helbig, Elchin E. Jafarov, Julie D. Jastrow, Aram A.M. Kalhori, Yongwon Kim, John S. Kimball, Lars Kutzbach, Mark J. Lara, Klaus S. Larsen, Bang Yong Lee, Zhihua Liu, Michael M. Loranty, Magnus Lund, Massimo Lupascu, Nima Madani, Avni Malhotra, Roser Matamala, Jack McFarland, A. David McGuire, Anders Michelsen, Christina Minions, Walter C. Oechel, David Olefeldt, Frans Jan W. Parmentier, Norbert Pirk, Ben Poulter, William Quinton, Fereidoun Rezanezhad, David Risk, Torsten Sachs, Kevin Schaefer, Niels M. Schmidt, Edward A.G. Schuur, Philipp R. Semenchuk, Gaius Shaver, Oliver Sonnentag, Gregory Starr, Claire C. Treat, Mark P. Waldrop, Yihui Wang, Jeffrey Welker, Christian Wille, Xiaofeng Xu, Zhen Zhang, Qianlai Zhuang, Donatella Zona
  • Woods Hole Research Center
  • University of Bayreuth
  • University of Alaska Anchorage
  • Brigham Young University
  • San Diego State University
  • University of Gothenburg
  • Jet Propulsion Laboratory, California Institute of Technology
  • Northern Arizona University
  • Aarhus University
  • Bjerknes Centre for Climate Research
  • Columbia University
  • University of Tromsø – The Arctic University of Norway
  • Stockholm University
  • University of California at Irvine
  • RAS - Pacific Geographical Institute, Far Eastern Branch
  • University of Montana
  • Dalhousie University
  • University of Copenhagen
  • University of Alaska Fairbanks
  • Max Planck Institute for Biogeochemistry
  • University of California at San Diego
  • Queen's University Kingston
  • McMaster University
  • University of Montreal
  • Los Alamos National Laboratory
  • Argonne National Laboratory
  • University of Hamburg
  • University of Illinois at Urbana-Champaign
  • Korea Polar Research Institute
  • Colgate University
  • National University of Singapore
  • Stanford University
  • United States Geological Survey
  • University of Exeter
  • University of Alberta
  • University of Oslo
  • Lund University
  • NASA Goddard Space Flight Center
  • Wilfrid Laurier University
  • University of Waterloo
  • Saint Francis Xavier University
  • Helmholtz Centre Potsdam - German Research Centre for Geosciences
  • University of Colorado Boulder
  • University of Vienna
  • The University of Chicago
  • University of Alabama
  • University of Eastern Finland
  • University of Oulu
  • University of Maryland, College Park
  • Purdue University
  • University of Sheffield

Research output: Contribution to journalArticlepeer-review

318 Scopus citations

Abstract

Recent warming in the Arctic, which has been amplified during the winter1–3, greatly enhances microbial decomposition of soil organic matter and subsequent release of carbon dioxide (CO2)4. However, the amount of CO2 released in winter is not known and has not been well represented by ecosystem models or empirically based estimates5,6. Here we synthesize regional in situ observations of CO2 flux from Arctic and boreal soils to assess current and future winter carbon losses from the northern permafrost domain. We estimate a contemporary loss of 1,662 TgC per year from the permafrost region during the winter season (October–April). This loss is greater than the average growing season carbon uptake for this region estimated from process models (−1,032 TgC per year). Extending model predictions to warmer conditions up to 2100 indicates that winter CO2 emissions will increase 17% under a moderate mitigation scenario—Representative Concentration Pathway 4.5—and 41% under business-as-usual emissions scenario—Representative Concentration Pathway 8.5. Our results provide a baseline for winter CO2 emissions from northern terrestrial regions and indicate that enhanced soil CO2 loss due to winter warming may offset growing season carbon uptake under future climatic conditions.

Original languageEnglish
Pages (from-to)852-857
Number of pages6
JournalNature Climate Change
Volume9
Issue number11
DOIs
StatePublished - Nov 1 2019

Funding

This study was supported by funding from NASA’s Arctic-Boreal Vulnerability Experiment (ABoVE; grant no. NNX15AT81A to S.M.N.), with additional funding from NASA New Investigator Program (grant no. NNX17AF16G to J.D.W.), National Science Foundation (grant nos. 955713 and 1331083 to E.A.G.S.; no. 1503559 to E.E.J.), the Next-Generation Ecosystem Experiments Arctic Project, Department of Energy Office of Science to E.E.J., Department of Energy Office of Science, Office of Biological and Environmental Research to J.D.J and R.M. (grant no. DE-AC02-06CH11357), National Research Foundation of Korea (grant nos. NRF-2016M1A5A1901769 and KOPRI-PN-19081 to B.-Y.L. and Y.K.), and funds that supported the data included in this synthesis.

FundersFunder number
DE-AC02-06CH11357
1331083, 955713, 1503559
National Aeronautics and Space AdministrationNNX15AT81A, NNX17AF16G

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 15 - Life on Land
      SDG 15 Life on Land

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