Results
From most borehole sites we now have continuous measurements of air and ground temperatures, as well as snow cover conditions since August 2008.
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Example of air and ground temperatures from Juvvass BH1 (1861 m a.s.l.). This site reveals an active layer of ~1.5 m. Note that the winter wave goes deeper during the 2008-2009 winter than the 2009-2010 winter although winter air temperatures are lower the second winter. The explanation is the thicker snow cover during the 2009-2010 winter, thereby isolating the ground surface from the low air temperature.
Published Nov. 23, 2010 12:24 PM
- Last modified Feb. 3, 2011 4:12 PM