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TitleMass balance of the Devon (NW), Meighen, and South Melville ice caps, Queen Elizabeth Islands for the 2012-2013 balance year
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorBurgess, D OORCID logo
SourceGeological Survey of Canada, Open File 7692, 2014, 26 pages, https://doi.org/10.4095/295443 Open Access logo Open Access
LinksAmerican Meteorological Society
LinksWorld Glacier Monitoring Service
Image
Year2014
PublisherNatural Resources Canada
Documentopen file
Lang.English
Mediaon-line; digital
RelatedThis publication is related to the following publications
File formatpdf
ProvinceNorthwest Territories; Nunavut
NTS48G; 48H; 58G; 58H; 68G; 68H; 78G; 78H; 88G; 88H; 49; 59; 69; 79; 89; 560; 340
AreaDevon Island; Melville Island; Meighen Island; Queen Elizabeth Islands
Lat/Long WENS-120.0000 -80.0000 84.0000 75.0000
Subjectssurficial geology/geomorphology; Nature and Environment; icefields; glaciers; ice thickness
Illustrationslocation maps
ProgramClimate Change Geoscience Essential Climate Variable Monitoring
Released2014 10 21
AbstractIn-situ glacier mass balance surveys were conducted across the Devon, Meighen, and South Melville ice caps in the Canadian high Arctic by Natural Resources Canada during spring, 2014. Survey results indicate positive net balance values for the Devon (NW) and Meighen ice caps (+2 and +17 cm w.e. respectively), while the South Melville ice cap experienced slightly negative mass balance (-18 cm w.e.). Results from these glacier surveys are indicative of relatively cool conditions that prevailed across this region during the summer of 2013. Associated water equivalent volume change for the Devon (NW), Meighen, and South Melville ice caps in 2012-2013 was 0.04, 0.01, and -0.009 Gt respectively resulted in a net negative contribution to global sea-level rise from these 3 sites for the 2012-2013 balance year.
Summary(Plain Language Summary, not published)
The Canadian high Arctic holds the single largest mass of ice outside of the Greenland and Antarctic ice sheets. Knowledge of annual glacier mass balance (ie. the difference between input[snow] and output[melt] for any given year) in this region thus provides a robust indicator of climate change, and facilitates assessments of contributions to regional and global sea-level from Canadian glaciers and ice caps. This report presents a summary of results from the 2014 glacier mass balance surveys (representing the 2012-2013 balance year) conducted by NRCan on the Devon, Melville South, and Meighen ice caps. Overall, glacier mass balance in the Queen Elizabeth Islands for 2012-2013 indicated a negative contribution to global sea-level rise reflecting relatively cool conditions that prevailed across this region during the summer of 2013.
GEOSCAN ID295443

 
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