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TitleCharacteristics of discontinuous permafrost based on ground temperature measurements and electrical resistivity tomography, southern Yukon, Canada
AuthorLewkowicz, A G; Etzelmuller, B; Smith, S LORCID logo
SourcePermafrost and Periglacial Processes 2011, 23 pages,
Alt SeriesEarth Sciences Sector, Contribution Series 20100083
Mediaon-line; digital; paper
File formatpdf
NTS105C; 105D; 115O
AreaDawson; Indian River; Wolfe Creek; Teslin; Whitehorse; Mayo Road; Johnson's Crossing
Lat/Long WENS-136.0000 -132.0000 61.0000 60.0000
Lat/Long WENS-140.0000 -138.0000 64.0000 63.0000
Subjectssurficial geology/geomorphology; geophysics; environmental geology; Nature and Environment; permafrost; freezing ground; ground ice; ground temperatures; electrical resistivity; resistivity; climate, arctic; climate; climatic fluctuations; Climate change
Illustrationslocation maps; tables; profiles; photographs
ProgramClimate Change Geoscience
Released2011 06 08
AbstractWarm permafrost conditions (mean temperatures of -3°C to -0.1°C) were investigated in detail at 13 valley and mountain sites in the sporadic (10 - 50%) and extensive (50 - 90%) discontinuous permafrost zones in the southern half of the Yukon (60°N to 64°N), using a combination of ground temperature monitoring, electrical resistivity tomography (ERT), frost table probing and coring. Sites were selected to cover a wide range of substrates, vegetation types and ground ice contents. ERT profiling in the spring imaged both deep seasonal frost and perennially frozen ground. Deep active layers measured by probing at the end of summer were also detectable by ERT. Where ground temperatures indicated that the base of permafrost was at a depth of less than 25 m, vertical transitions in apparent resistivity were more sharply defined in coarse materials than in fine-grained deposits, probably because of differences in unfrozen moisture contents at temperatures just below 0°C. Apparent resistivity values related to excess ice fraction and ground temperatures were similar to those previously obtained in Mongolia and Iceland, but generally lower than in ice-rich rock glaciers in European studies. The observations revealed the complexity of site conditions where permafrost is discontinuous and the utility of ERT, in combination with other methods, to investigate permafrost thickness, spatial extent and ice content for infrastructure planning or climate change studies.

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