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Paleoecological techniques are used to investigate how Canadian High Arctic wetlands responded to a mid-twentieth century increase in growing degree days.
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The continental shelf of the Canadian Beaufort Sea is investigated to see if it is causing decomposition of relict offshore subsea permafrost and gas hydrates.
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Research on how soil and air temperature is affected by snow.
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Active layer thickness data paired with Landsat data were used to quantify the impacts of changing permafrost conditions on vegetation productivity in the NWT.
