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Alan E. Taylor, S. R. Dallimore, P. R. Hill, D. R. Issler, S. Blasco and F. Wright Numerical model of the geothermal regime on the Beaufort Shelf, arctic Canada since the Last Interglacial Journal of Geophysical Research: Earth Surface 118

Version of Record online: 14 NOV 2013 | DOI: 10.1002/2013JF002859

Key Points

  • Offshore permafrost is modeled considering geology, sea level and paleoclimate
  • Permafrost extends to the ~95 m isobath from modeling and geophysical evidence
  • Upper permafrost surface is depressed by the seasonal Mackenzie River outflow

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