Journal
JOURNAL OF GLACIOLOGY
Volume 60, Issue 220, Pages 262-276Publisher
INT GLACIOL SOC
DOI: 10.3189/2014JoG13J091
Keywords
glacier mass balance; glaciological instruments and methods; remote sensing
Funding
- Canadian Foundation for Climate and Atmospheric Sciences (CFCAS)
- Canada Foundation for Innovation
- British Columbia Knowledge Development Fund
- UNBC
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We estimate the glacier mass balance of a 9.5 km(2) mountain glacier using three approaches for balance years 2009, 2010 and 2011. The photogrammetric, GPS and glaciological methods yielded sampling densities of 100, 5 and 2 points km(-2), with measurement precisions of +/- 0.40, +/- 0.10 and +/- 0.10 m w.e. respectively. Our glaciological measurements likely include a positive bias, due to omission of internal and basal mass balance, and uncertainty in determining the interface between snow and firn with a probe (+/- 0.10 m w.e.). Measurements from our photogrammetric method include a negative bias introduced by the manual operator and our temperature index model used to correct for different dates of imaging (0.15 m w.e.), whereas GPS measurements avoid these biases. The photogrammetric and GPS methods are suitable for estimating glacier-wide annual mass balance, and thus provide a valuable measure that complements the glaciological method. These approaches, however, cannot be used to estimate mass balance at a point or mass-balance profiles without a detailed understanding of the vertical component of ice velocity.
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