|Title||The thermal state of permafrost in Canada - results from the International Polar Year|
|Author||Smith, S L; Lewkowicz, A G; Burn, C R; Allard, M; Throop, J L|
|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 20090436|
|Meeting||3rd European Conference on Permafrost (EUCOPIII); Longyearbyen Svalbard; NO; June 14-18, 2010|
|Province||British Columbia; Alberta; Saskatchewan; Manitoba; Ontario; Quebec; New Brunswick; Nova Scotia; Prince Edward Island; Newfoundland and Labrador; Northwest Territories; Yukon; Nunavut|
|NTS||1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 52; 53; 54; 55; 56; 57; 58; 59; 62; 63; 64; 65;
66; 67; 68; 69; 72; 73; 74; 75; 76; 77; 78; 79; 82; 83; 84; 85; 86; 87; 88; 89; 92; 93; 94; 95; 96; 97; 98; 99; 102; 103; 104; 105; 106; 107; 114O; 114P; 115; 116; 117; 120; 340; 560|
|Lat/Long WENS||-141.0000 -50.0000 90.0000 41.7500|
|Subjects||surficial geology/geomorphology; Nature and Environment; permafrost; ground ice; freezing ground; terrain types; terrain analysis; thermal analyses; ground temperatures|
|Program||Climate Change Geoscience, Earth Science for National Scale Characterization of Climate Change Impacts on Canada's Landmass|
|Abstract||The International Polar Year (IPY) provided the op-portunity for the Canadian permafrost community to conduct a coordinated program of permafrost obser-vations in order to define present permafrost
condi-tions and their spatial and temporal variability. Can-ada¿s contribution to the multinational Thermal State of Permafrost project examines the ongoing impacts of climate change on permafrost conditions.|
The Canadian permafrost monitoring
network cur-rently consists of about 170 sites, with almost half of these established during the IPY to address geo-graphical gaps such as the eastern Arctic and the mountains of the Yukon Territory. The measurement sites span a diverse range of
ecoclimatic and geo-logical conditions across northern Canada. An up-dated snapshot of the thermal state of permafrost was developed that indicates permafrost tempera-tures range from warmer than -2.5°C in the discon-tinuous zone to as cold as -15°C
in the continuous zone (Table 1).
Ground temperature records 20 to 30 years long, available for a number of sites, indicate that perma-frost was generally warmer during IPY than the av-erage ground temperature for the entire record. In concert
with regional air temperatures, permafrost has been warming across Canada for the past several decades with later warming occurring (since the early 1990s) in the eastern Arctic. Rates of perma-frost temperature increase are variable and are
gen-erally greater in colder permafrost north of treeline where the upper 15 m of permafrost has warmed by up to 0.1°C per year. Latent heat effects in the southern discontinuous zone dominate the perma-frost thermal regime close to 0°C and allow
perma-frost to persist for decades under a warming climate. Consequently, the spatial diversity of permafrost thermal conditions is decreasing over time.
The snapshot of permafrost thermal state generated by this project provides an improved
baseline against which change can be measured. Essential in-formation has been generated for improved assess-ments of climate change impacts and predictions of future conditions. The project has also provided in-formation that can be utilized for:
engineering de-sign of northern infrastructure; informed landuse planning decisions; development of adaptation strategies to deal with climate change.