The islands of the Canadian Arctic, known as the Canadian Arctic Archipelago (CAA), contain the largest area of glacierized terrain outside of the ice sheets...
Previous studies reported that Good Friday Glacier had been actively surging in the 1950-60s, 1990s and again in 2000-15. Based on observations of terminus...
Landsat 7 and RADARSAT-1/RADARSAT-2 satellite images are used to produce the most comprehensive record of glacier motion in the Canadian High Arctic to date...
Speckle-tracking of historically acquired ALOS PALSAR and RADARSAT-2 datasets are used to determine the dynamics of major glaciers and ice masses in western...
Speckle tracking of ALOS PALSAR fine beam data from 2007-2011 is used to determine the surface motion of the major ice masses of Baffin and Bylot Islands in...
Over the last two decades, Trinity, Wykeham, Ekblaw, and Cadogan glaciers have retreated and been identified as the primary sources of iceberg flux from Prince...
Speckle tracking of repeat RADARSAT-2 fine-beam imagery acquired over 24 day periods in March 2009 allowed the creation of updated surface motion maps for the...
Recent studies indicate an increase in glacier mass loss from the Canadian Arctic Archipelago as a result of warmer summer air temperatures. However, no...
Feature tracking of approximately annually separated Landsat-7 ETM+ imagery acquired from 1999 to 2010 and speckle tracking of 24-day separated RADARSAT-2...
The basal topography of most of the glaciers that drain the ice caps of the Canadian Arctic Archipelago is largely unknown. To measure the basal topography,...
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