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AGU: Geophysical Research Letters

 

Keywords

  • climate change
  • permafrost degradation
  • Arctic region
  • numerical simulation

Index Terms

  • Cryosphere: Permafrost
  • Cryosphere: Active layer
  • Cryosphere: Thermal regime
  • Global Change: Cryospheric change
  • Global Change: Impacts of global change

Abstract

Near-surface permafrost degradation: How severe during the 21st century?

G. Delisle

Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover, Germany

A previously presented model on nearly complete near-surface permafrost degradation in the Arctic during the 21st century is critically reviewed. An alternative model with a more complete mathematical formulation of the physical processes acting in permafrost terrain is presented, which suggests that permafrost will mostly prevail in this century in areas north of 70°N. Furthermore, permafrost will survive at depth in most areas between 60° to 70°N. Based on paleoclimatic data and in consequence of this study, it is suggested that scenarios calling for massive release of methane in the near future from degrading permafrost are questionable.

Received 11 January 2007; accepted 11 April 2007; published 10 May 2007.

Citation: Delisle, G. (2007), Near-surface permafrost degradation: How severe during the 21st century?, Geophys. Res. Lett., 34, L09503, doi:10.1029/2007GL029323.

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