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TitleNumerical model of the geothermal regime on the Beaufort Shelf, arctic Canada since the Last Interglacial
AuthorTaylor, A E; Dallimore, S R; Hill, P R; Issler, D R; Blasco, S; Wright, F
SourceJournal of Geophysical Research, Earth Surface vol. 118, no. 4, 2013 p. 2365-2379, (Open Access)
Alt SeriesNatural Resources Canada, Contribution Series 20182926
Mediapaper; on-line; digital
File formatpdf
ProgramPublic Safety Geoscience
ProgramClimate Change Geoscience
Released2013 11 14
AbstractA finite element geothermal model is developed for the outer Mackenzie Delta-Beaufort Sea shelf to predict permafrost evolution since the Last Interglacial ~130-116 kaBP(cal). The purpose is to reconcile sparse observations of the depth and extent of ice-bonded permafrost with sediment properties and the paleoenvironment. Sea level curves determine, as a function of time, areas of the shelf that were subaerially exposed, promoting permafrost aggradation, and areas that were submerged, promoting permafrost degradation. Assuming as a model starting point that a paleoclimate similar to today persisted through the Last Interglacial, permafrost subsequently aggrades in depth and advances seaward from the present shoreline to the shelf/slope bathymetric break by the Last Glacial Maximum (LGM) ~26 kaBP(cal). Modeled permafrost exhibits reduced growth in depth and seaward progression that correlate with early and middle Wisconsin stillstands in sea level. Following the LGM and rise in sea level, offshore permafrost degrades and permafrost base rises ~100 m to its present depth of ~600 m. The offshore limit of modeled ice-bonded permafrost lies at the ~95 m isobath, within 1 km of the bathymetric shelf/slope break. The model replicates features of offshore permafrost body observed seismically and demonstrates that warm outflow from the Mackenzie River depresses the upper surface of offshore permafrost by tens of meters to the 20 m isobath. Although Pleistocene permafrost predated the Wisconsinan, the model demonstrates that the paleoenvironment of the last 125,000 years is sufficient to develop the depth, seaward extent, and principal features of the permafrost body. 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.