Abstract Analysis of the δD and δ18O composition of ice is commonly used to provide insight
into the origin of ice bodies. However, studies have questioned the use of the co‐isotope …

There remains a lack of understanding of environmental isotopes and their use; students
and practitioners typically find the concepts of isotope concentrations and partitioning to be …

Retrogressive thaw slumps (RTSs) are spectacular landforms that occur due to the thawing
of ice-rich permafrost or melting of massive ground ice, often in hillslope terrain. RTSs occur …

Patterns of coastal erosion in the Arctic differ dramatically from those coasts in more
temperate environments. Thick sea ice and shore-fast ice limit wave-based erosional …

Ice‐cored permafrost landscapes are highly sensitive to disturbance and have the potential
to undergo dramatic geomorphic transformations in response to climate change. The …

Climate change is increasing the frequency and intensity of thermokarst, but the influences
of regional climate and physiography remain poorly understood. Retrogressive thaw …

Retrogressive thaw slumps are one of the most active geomorphic features in permafrost
terrain. This study investigated the distribution and growth of thaw slumps in the Richardson …

Climate change is increasing the frequency and intensity of thermokarst, and accelerating
the delivery of terrestrial organic material from previously sequestered sources to aquatic …

The climatic and geomorphic factors affecting retrogressive thaw slump initiation and activity
on the Aklavik Plateau (Richardson Mountains, NWT) were examined using historical air …

Permafrost thaw in the Arctic enables the biogeochemical transformation of vast stores of
organic carbon into carbon dioxide (CO2). This CO2 release has significant implications for …