Validation of the Basal Temperature of Snow (BTS) Method to Map Permafrost in Complex Mountainous Terrain, Ruby Range, Yukon Territory and Haines Summit, British Columbia

Validation of the Basal Temperature of Snow (BTS) Method to Map Permafrost in Complex Mountainous Terrain, Ruby Range, Yukon Territory and Haines Summit, British Columbia

121 pages· 2006· ISBN 9780494257487
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This study is the second attempt to use the Basal Temperature of Snow (BTS) method to map permafrost in mountainous regions of northwestern Canada. It differs from the first study which took place in Wolf Creek in terms of (1) the methodology used to evaluate BTS, (2) the strategy used to avoid spatial autocorrelation in residuals, and (3) the climatic regions investigated. Two study areas, part of the Ruby Range (61° 12' N, 138° 19' W) and Haines Summit (59° 37' N, 136° 27' W) were selected for BTS sampling based on differing climatic conditions and previous knowledge of permafrost elevations from active rock glaciers.

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