Canadian Arctic Research
Summer sea ice off the coast of Devon Island, Nunavut, Canada.
Canadian Arctic Research
Landsat 7 ETM+ satellite image of the south-east Devon Island Ice Cap, Devon Island, Nunavut, Canada. The darker ice is the result of accumulated impurities at the surface.
Canadian Arctic Research
An ice cave or englacial melt channel. This ice cave was formed by meltwater flowing within the glacier ice. Belcher Glacier, Devon Island, Nunavut, Canada.
Canadian Arctic Research
Canadian researcher Brad Danielson maintaining a time-lapse camera overlooking the Belcher Glacier, Devon Island, Nunavut, Canada. Monitoring the ice that breaks off from the glacier helps the researchers constrain how much ice is calving into the ocean.
Canadian Arctic Research
MODIS satellite true color image of the Canadian Arctic Archipelago.
Canadian Arctic Research
Ice channel or supraglacial melt channel. This was formed by meltwater flowing along the surface of the glacier. Belcher Glacier, Devon Island, Nunavut, Canada.
Canadian Arctic Research
Ice lake or supraglacial lake. Surface melt water can pond on the surface of the glacier forming large lakes that can drain catastrophically. Belcher Glacier, Devon Island, Nunavut, Canada.
Canadian Arctic Research
MODIS satellite true color image of the Canadian Arctic Archipelago.
Canadian Arctic Research
Canadian researcher maintaining one of several weather station on the Devon Island, Nunavut, Canada. The researchers camp can be seen in the foreground. Monitoring the meteorological conditions over the ice cap helps researchers to determine glacier responses to changes in climate.
Canadian Arctic Research
Landsat 7 ETM+ satellite image of eastern Bylot Isalnd, Nunavut, Canada.
Canadian Arctic Research
Areal view of the Sverdrup Glacier, a river of ice that flows from the interior of the Devon Island Ice Cap into the ocean. Nunavut, Canada. Flow stripes are clearly visible on the surface of the glacier.
