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Northern permafrost represents a limit on the northward shift of climatically feasible agricultural frontiers under future warming
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  • Published: 30 May 2026

Northern permafrost represents a limit on the northward shift of climatically feasible agricultural frontiers under future warming

  • Song Xu  ORCID: orcid.org/0009-0003-1842-20171,
  • Cunde Xiao  ORCID: orcid.org/0000-0002-1706-47941,
  • Jonas Jägermeyr  ORCID: orcid.org/0000-0002-8368-00182,3,4,
  • Vladimir E. Romanovsky  ORCID: orcid.org/0000-0002-9515-20875,
  • Zhao Zhang  ORCID: orcid.org/0000-0002-5697-80116,
  • Jianping Duan  ORCID: orcid.org/0000-0002-0095-07141,
  • Bo Su1,7,8,9 &
  • …
  • Tong Zhang  ORCID: orcid.org/0000-0001-9074-41661 

Communications Earth & Environment (2026) Cite this article

We are providing an unedited version of this manuscript to give early access to its findings. Before final publication, the manuscript will undergo further editing. Please note there may be errors present which affect the content, and all legal disclaimers apply.

Subjects

  • Cryospheric science
  • Projection and prediction

Abstract

Global warming is expected to shift crop suitability northward, but the role of permafrost remains unclear. Here we integrate permafrost degradation impacts to project the suitability of seven major crops across the Northern Hemisphere (30°N–83°N). By the end of the century, the northern boundary of crop climatic suitability zones shifts northward by ~331 km and ~739 km under the SSP1–2.6 and SSP5–8.5 scenarios, respectively. Considering this shift and permafrost degradation, zones with persistent near-surface permafrost remain limited (~5%) but vary widely (3–19%) across different permafrost degradation assumptions. By the end of the century, newly emerging frontiers of climatically feasible agriculture reach 4.86 and 11.64 million km² under SSP1–2.6 and SSP5–8.5, respectively, of which 29% and 18% may remain unsuitable for cultivation due to persistent permafrost thaw disturbances. Our results indicate that permafrost is a non-negligible constraint on the northward shift of climatically feasible agricultural frontiers.

Acknowledgements

We are grateful to Hui Ju, Yang Yang, and Renjie Hou for their valuable feedback on the conceptualization and formal analysis.

Funding

S.X. and C.X. disclose support for the research of this work from the National Key Research and Development Program of China (2022YFF0801903) and the Faculty of Geographical Sciences, Beijing Normal University (2022-GJTD-01).

Author information

Authors and Affiliations

  1. State Key Laboratory of Earth Surface Processes and Disaster Risk Reduction, Faculty of Geographical Science, Beijing Normal University, Beijing, China

    Song Xu, Cunde Xiao, Jianping Duan, Bo Su & Tong Zhang

  2. NASA Goddard Institute for Space Studies, New York, NY, USA

    Jonas Jägermeyr

  3. Columbia University, Center for Climate Systems Research, New York, NY, USA

    Jonas Jägermeyr

  4. Potsdam Institute for Climate Impacts Research (PIK), Member of the Leibniz Association, Potsdam, Germany

    Jonas Jägermeyr

  5. Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA

    Vladimir E. Romanovsky

  6. Joint International Research Laboratory of Catastrophe Simulation and Systemic Risk Governance, School of National Safety and Emergency Management, Beijing Normal University, Beijing, P. R. China

    Zhao Zhang

  7. School of Environment, Beijing Normal University, Beijing, China

    Bo Su

  8. Regional Climate Group, Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden

    Bo Su

  9. Stockholm Resilience Centre, Stockholm University, Stockholm, Sweden

    Bo Su

Authors
  1. Song Xu
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  2. Cunde Xiao
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  3. Jonas Jägermeyr
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  4. Vladimir E. Romanovsky
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  5. Zhao Zhang
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  6. Jianping Duan
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  7. Bo Su
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  8. Tong Zhang
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Corresponding author

Correspondence to Cunde Xiao.

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Cite this article

Xu, S., Xiao, C., Jägermeyr, J. et al. Northern permafrost represents a limit on the northward shift of climatically feasible agricultural frontiers under future warming. Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03702-w

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  • Received: 07 December 2025

  • Accepted: 26 May 2026

  • Published: 30 May 2026

  • DOI: https://doi.org/10.1038/s43247-026-03702-w

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