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Drainage network response to Arctic warming

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  • Joel C. Rowland

    (Los Alamos National Laboratory)

Abstract

Rapid Arctic warming may increase erosion and stream channel formation, which alters the flux of sediments, carbon, and nutrients in these sensitive ecosystems. Yet, understanding landscape change is hampered by a lack of predictive tools applicable to permafrost settings.

Suggested Citation

  • Joel C. Rowland, 2023. "Drainage network response to Arctic warming," Nature Communications, Nature, vol. 14(1), pages 1-2, December.
    • Handle: RePEc:nat:natcom:v:14:y:2023:i:1:d:10.1038_s41467-023-40796-8
    DOI: 10.1038/s41467-023-40796-8
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    References listed on IDEAS

    as
    1. Daniel Fortier & Michel Allard & Yuri Shur, 2007. "Observation of rapid drainage system development by thermal erosion of ice wedges on Bylot Island, Canadian Arctic Archipelago," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 18(3), pages 229-243, July.
    2. Shawn M. Chartrand & A. Mark Jellinek & Antero Kukko & Anna Grau Galofre & Gordon R. Osinski & Shannon Hibbard, 2023. "High Arctic channel incision modulated by climate change and the emergence of polygonal ground," Nature Communications, Nature, vol. 14(1), pages 1-12, December.
    Full references (including those not matched with items on IDEAS)

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