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Recent permafrost degradation in bogs of the James Bay area, northern Quebec, Canada

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  • Simon Thibault
  • Serge Payette

Abstract

Small palsas with very thin frozen layers are present within the peat deposits east of James Bay. Most of these permafrost landforms are in an advanced stage of decay within raised bogs between 51°45′N and 55°N. Air photographs, air‐borne surveys and ground‐truthing of permafrost indicate a recent northward recession of the permafrost boundary by about 130 km, most of which likely happened in the past 50 years. Copyright © 2009 John Wiley & Sons, Ltd.

Suggested Citation

  • Simon Thibault & Serge Payette, 2009. "Recent permafrost degradation in bogs of the James Bay area, northern Quebec, Canada," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 20(4), pages 383-389, October.
  • Handle: RePEc:wly:perpro:v:20:y:2009:i:4:p:383-389
    DOI: 10.1002/ppp.660
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    Cited by:

    1. C. Derksen & S. Smith & M. Sharp & L. Brown & S. Howell & L. Copland & D. Mueller & Y. Gauthier & C. Fletcher & A. Tivy & M. Bernier & J. Bourgeois & R. Brown & C. Burn & C. Duguay & P. Kushner & A. L, 2012. "Variability and change in the Canadian cryosphere," Climatic Change, Springer, vol. 115(1), pages 59-88, November.

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