2012
DOI: 10.1007/s10584-012-0470-0
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Variability and change in the Canadian cryosphere

Abstract: During the International Polar Year (IPY), comprehensive observational research programs were undertaken to increase 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 f… Show more

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Cited by 92 publications
(67 citation statements)
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“…Arctic sea ice in Canada has also retreated in recent decades with strong negative trends in the Hudson and Baffin bays (Tivy et al, 2011;Derksen et al, 2012). Vessel transit within the Vessel Traffic Reporting Arctic Canada Traffic Zone (NORDREG) has been observed since 1990.…”
Section: A a Aliabadi Et Al: Air Quality Monitoring In The Arcticmentioning
confidence: 99%
“…Arctic sea ice in Canada has also retreated in recent decades with strong negative trends in the Hudson and Baffin bays (Tivy et al, 2011;Derksen et al, 2012). Vessel transit within the Vessel Traffic Reporting Arctic Canada Traffic Zone (NORDREG) has been observed since 1990.…”
Section: A a Aliabadi Et Al: Air Quality Monitoring In The Arcticmentioning
confidence: 99%
“…In Arctic coastal regions, for example, climate change is already threatening the livelihoods of indigenous communities. The melting of permafrost and the withdrawal of sea ice in the Arctic directly threaten infrastructure, traditional lifestyles and human well-being in coastal communities, cause increasing coastal erosion, and have adverse effects on sensitive coastal habitats [46], [47], [48].…”
Section: Challenges In Securing Blue Wealthmentioning
confidence: 99%
“…In a rapidly changing climate IPCC, 2013;Lenaerts et al, 2013;Woo and Young, 2014), with each of the last 3 decades being successively warmer than any preceding decade (Derksen et al, 2012) and as a result of complex energy exchanges between atmosphere, ocean, and land, the Arctic cryosphere is possibly transitioning towards a new state. As a major feature of the Arctic landscape, lakes, through their ice cover phenology (timing of ice formation, onset of melt, and end of break-up), are a key indicator of climatic changes (Heron and Woo, 1994;Duguay et al, 2006;Williamson et al, 2008) that the high-latitude environment is experiencing.…”
Section: Introductionmentioning
confidence: 99%