Physics
Scientific paper
May 2007
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007georl..3409503d&link_type=abstract
Geophysical Research Letters, Volume 34, Issue 9, CiteID L09503
Physics
15
Cryosphere: Permafrost (0475), Cryosphere: Active Layer, Cryosphere: Thermal Regime, Global Change: Cryospheric Change (0776), Global Change: Impacts Of Global Change (1225)
Scientific paper
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.
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