|Title||Climate and permafrost relations across widely separated sites in northern Canada|
|Author||Throop, J; Smith, S L; Lewkowicz, A G|
|Source||Thermal state of frozen ground in a changing climate during the IPY, abstracts from the Third European Conference on Permafrost; by Mertes, J R (ed.); Christiansen, H H (ed.); Etzelmüller, B (ed.); 2010
|Alt Series||Earth Sciences Sector, Contribution Series 20090435|
|Meeting||3rd European Conference on Permafrost (EUCOPIII); Longyearbyen, Svalbard; NO; June 14-18, 2010|
|Province||Northwest Territories; Nunavut; Yukon|
|NTS||25; 26; 27; 35; 36; 37; 38; 39; 45; 46; 47; 48; 49; 55; 56; 57; 58; 59; 65; 66; 67; 68; 69; 75; 76; 77; 78; 79; 85; 86; 87; 88; 89; 95; 96; 97; 98; 99; 105; 116; 107; 115; 116; 117; 120; 340; 560|
|Lat/Long WENS||-141.0000 -60.0000 90.0000 60.0000|
|Subjects||surficial geology/geomorphology; environmental geology; Nature and Environment; permafrost; freezing ground; ground ice; ground temperatures; climate, arctic|
|Program||Climate Change Geoscience|
|Abstract||Permafrost zones extend across 50% of Canada's land area, with conditions varying from continuous through to isolated patches, along latitudinal and elevational gradients (Heginbottom et al., 1995). The
purpose of this study is to determine the spatially variable influence of climate on permafrost tempera-tures at nine widely separated thermal monitoring sites in northern Canada (Figure 1).|
The study sites encompass various environmental and
climatic conditions, and range from ice-rich sediment with mean annual temperatures just below 0°C in the sporadic discontinuous permafrost zone, to bedrock at temperatures close to -15°C in the con-tinuous permafrost zone. There are between one and
five boreholes at each site ranging in depth from 3 to 60 m.
A comparative analysis was conducted to assess the variability in climate-permafrost relationships across space. The local characteristics at each bore-hole were assessed using the
mean annual air and ground temperatures (MAAT and MAGT, respec-tively), freezing n-factor (nf), apparent thermal dif-fusivity (ATD), snow characteristics, and substrate.
A strong relationship exists between MAAT and MAGT across all of the
sites. The differences be-tween these two variables increase as MAAT in-creases. The strongest relationships were observed at Alert and Iqaluit, where the least amount of snow accumulates.
The sites with MAGTs close to 0°C are consid-ered warm
permafrost, and the sites below -2°C are considered cold permafrost. The ATD was at least an order of magnitude lower at the warm permafrost sites than the cold ones, and generally increased with increasing depth across all of the sites.
warm permafrost sites at Wrigley, Table Mountain, and Wolf Creek had the lowest values of nf, ranging between 0.21 and 0.44. Values of nf were highest at very cold or bedrock sites, Alert, Iqaluit, Sixty Mile, and Alpine Burwash, even though some of
these sites had significant amounts of snow. Al-though snow has a great influence on air-ground sur-face temperature relationships during the winter, the relationship is modulated by air temperatures, active layer thickness, and subsurface moisture.
The influence of vegetation and snow characteris-tics, substrate, and frozen and unfrozen moisture on the thermal link between air and permafrost tem-peratures is evident through the variations in annual temperature amplitude propagation.
MAAT is the primary determinant of permafrost temperatures across these study sites in northern Canada. Cold bedrock sites are more sensitive to changes in climate than the warm ice-rich perma-frost sites. The relationship between snow and nf
de-pends not only on MAAT and active layer thickness, but also on the substrate material and moisture con-tent, both frozen and unfrozen, at the site.