|Title||Variability and change in the Canadian Cryosphere
|Author||Derksen, C; Smith, S L; Sharp, M; Howell, S; Mueller, D; Copland, L; Gautier, Y; Fletcher, C; Walker, A|
|Source||Program and abstracts, International Polar Year (IPY) 2012 conference; by IPY 2012 Committee; 2012 p. 1|
|Alt Series||Earth Sciences Sector, Contribution Series 20110193|
|Meeting||International Polar Year (IPY) 2012 Conference - From Knowledge to Action; Montréal; CA; April 22-27, 2012|
|Province||British Columbia; Alberta; Saskatchewan; Manitoba; Ontario; Quebec; New Brunswick; Nova Scotia; Prince Edward Island; Newfoundland and Labrador; Northwest Territories; Yukon; Nunavut; Canada|
|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||environmental geology; surficial geology/geomorphology; Nature and Environment; climate effects; climate, arctic; climatic fluctuations; ground temperatures; temperature; permafrost|
|Program||Climate Change Geoscience|
|Abstract||Through its influence on the surface energy balance of the Earth, and on moisture and gas (including greenhouse gas) fluxes within the Earth system, the polar cryosphere plays an important role in
Arctic and global climate, ocean circulation, and freshwater hydrological systems. During the International Polar Year, Canadian cryospheric scientists conducted comprehensive observational research programs aimed at increasing our understanding of
the Canadian polar cryosphere response to a changing climate. Cryospheric components considered were snow, permafrost, sea ice, freshwater ice, glaciers and ice shelves. Enhancement of conventional observing systems and retrieval algorithms for
satellite measurements facilitated development of a snapshot of current cryospheric conditions, providing a baseline against which future change can be assessed. Key findings include that:|
1. a consistent response to warming air temperatures
at the surface and in the lower troposphere is evident through the analysis of longer-term cryospheric data sets. The pan-Arctic, pan-cryosphere response to spring temperature anomalies underscore the close relationship between the cryosphere and
surface air temperatures over the Arctic region in June when albedo feedback potential is at a maximum.
2. the IPY period marked an acceleration of trends observed over the previous decades including warming permafrost, reduction in snow cover
extent and duration, reduction in summer sea ice extent, increased mass loss from glaciers, and thinning and break-up of the remaining Canadian ice shelves. These changes illustrate both a reduction in the spatial extent and mass of the cryosphere
(such as sea ice area/volume and negative glacier mass balance) as well as an increase in the temporal persistence of melt related parameters.
3. the strength of the snow-albedo feedback (SAF), as determined from a suite of global climate model
simulations, is an excellent predictor of SAF strength under climate change. Model simulations also projected an earlier lake ice break-up date by up to 25 days, with a reduction in mean ice thickness of up to 40 cm.
4. the observed changes in the
cryosphere have important implications for human activity including the vulnerability of northern residents and their traditional lifestyles, access to northern regions for natural resource development, and the integrity of northern
Sustained efforts to comprehensively observe all elements of the cryosphere are necessary to understand the response to a changing global climate system, understand how these changes will affect terrestrial and marine
ecosystems, and reduce the vulnerability of northern residents and northern development to climate-induced uncertainty.