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View article: Multi-scale water balance analysis of a thawing boreal peatland complex near the southern permafrost limit in northwestern Canada
Multi-scale water balance analysis of a thawing boreal peatland complex near the southern permafrost limit in northwestern Canada Open
Permafrost thaw profoundly changes landscapes in the Arctic-boreal region, affecting ecosystem composition, structure, function and services and their hydrological controls. The water balance provides insights into water movement and distr…
View article: Fire, drought and permafrost thaw: interactive effects on dissolved organic carbon, mercury, and nutrients in peatland-rich watersheds of boreal western Canada.  
Fire, drought and permafrost thaw: interactive effects on dissolved organic carbon, mercury, and nutrients in peatland-rich watersheds of boreal western Canada.   Open
Permafrost thaw, wildfires, and increased amplitude of floods and droughts are all aspects of climate change that risk affecting the downstream mobilization of dissolved organic carbon (DOC), the neurotoxin methylmercury (MeHg), and variou…
View article: Multi-scale water balance analysis of a thawing boreal peatland complex near the southern permafrost limit in western Canada
Multi-scale water balance analysis of a thawing boreal peatland complex near the southern permafrost limit in western Canada Open
Permafrost thaw profoundly changes landscapes in the Arctic-boreal region, affecting ecosystem composition, structure, function and services and their hydrological controls. The water balance provides insights into water movement and distr…
View article: Detecting Forest‐Wetland Changes in Northwestern Canada's Discontinuous Permafrost Region Using Landsat Trend Analysis
Detecting Forest‐Wetland Changes in Northwestern Canada's Discontinuous Permafrost Region Using Landsat Trend Analysis Open
Rapid circumpolar warming has led to accelerated permafrost thaw that has induced extensive landscape change in northwestern Canada. In northwestern Canada's discontinuous permafrost zone, forest‐dominated peatland landscapes, which were l…
View article: Watershed hydrology mediates the recovery of an arsenic impacted subarctic landscape
Watershed hydrology mediates the recovery of an arsenic impacted subarctic landscape Open
A holistic understanding of the chemical recovery of lakes from arsenic (As) pollution requires consideration of within-lake biogeochemical cycling of As and processes occurring in the surrounding catchment. This study used a watershed mas…
View article: Thaw-induced impacts on land and water in discontinuous permafrost: A review of the Taiga Plains and Taiga Shield, northwestern Canada
Thaw-induced impacts on land and water in discontinuous permafrost: A review of the Taiga Plains and Taiga Shield, northwestern Canada Open
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View article: Heterogenous runoff trends in peatland-dominated basins throughout the circumpolar North
Heterogenous runoff trends in peatland-dominated basins throughout the circumpolar North Open
The hydrological implications of discontinuous permafrost thaw in peatland-dominated basins are not well understood. While there is evidence suggesting that permafrost-thaw-driven land cover change increases annual runoff and the runoff ra…
View article: Long-term climate-influenced land cover change in discontinuous permafrost peatland complexes
Long-term climate-influenced land cover change in discontinuous permafrost peatland complexes Open
The discontinuous permafrost zone is undergoing rapid transformation as a result of unprecedented permafrost thaw brought on by circumpolar climate warming. Rapid warming over recent decades has significantly decreased the area underlain b…
View article: The trajectory of landcover change in peatland complexes with discontinuous permafrost, northwestern Canada
The trajectory of landcover change in peatland complexes with discontinuous permafrost, northwestern Canada Open
The discontinuous permafrost zone is undergoing rapid transformation as a result of unprecedented permafrost thaw brought on by circumpolar climate warming. Rapid climate warming over recent decades has significantly decreased the area und…
View article: Pore-scale controls on hydrological and geochemical processes in peat: Implications on interacting processes
Pore-scale controls on hydrological and geochemical processes in peat: Implications on interacting processes Open
Peatlands are wetlands that provide important ecosystem services including carbon sequestration and water storage that respond to hydrological, biological, and biogeochemical processes. These processes are strongly influenced by the comple…
View article: A thawing boreal peat landscape along the southern limit of permafrost presently is carbon neutral
A thawing boreal peat landscape along the southern limit of permafrost presently is carbon neutral Open
<p>Along the southern limit of permafrost in northwestern Canada rising air temperatures have caused widespread land cover changes at unprecedented rates. A prominent change includes thermokarst wetland expansion at the expense of bl…
View article: Hydrometeorological measurements in peatland‐dominated, discontinuous permafrost at Scotty Creek, Northwest Territories, Canada
Hydrometeorological measurements in peatland‐dominated, discontinuous permafrost at Scotty Creek, Northwest Territories, Canada Open
The discontinuous permafrost region of northwestern Canada is experiencing rapid warming resulting in dramatic land cover change from forested peatland permafrost terrain to treeless wetlands. Extensive research has been conducted througho…
View article: A synthesis of three decades of hydrological research at Scotty Creek, NWT, Canada
A synthesis of three decades of hydrological research at Scotty Creek, NWT, Canada Open
Scotty Creek, Northwest Territories (NWT), Canada, has been the focus of hydrological research for nearly three decades. Over this period, field and modelling studies have generated new insights into the thermal and physical mechanisms gov…
View article: Permafrost thaw induced drying of wetlands at Scotty Creek, NWT, Canada
Permafrost thaw induced drying of wetlands at Scotty Creek, NWT, Canada Open
Northwestern Canada is one of the most rapidly warming regions on Earth. The scale and rapidity of recently observed warming-induced changes throughout this region indicate that it is particularly sensitive to climate warming and capable o…
View article: A Synthesis of Three Decades of Eco-Hydrological Research at Scotty Creek, NWT, Canada
A Synthesis of Three Decades of Eco-Hydrological Research at Scotty Creek, NWT, Canada Open
Scotty Creek, Northwest Territories (NWT), Canada, has been the focus of eco-hydrological research for nearly three decades. Over this period, field and modelling studies have generated new insights into the thermal and physical mechanisms…
View article: Hydrometric measurements in peatland-dominated, discontinuous permafrost at Scotty Creek, Northwest Territories, Canada – Changing Cold Regions Network (CCRN) Special Observation and Analysis Period (SOAP)
Hydrometric measurements in peatland-dominated, discontinuous permafrost at Scotty Creek, Northwest Territories, Canada – Changing Cold Regions Network (CCRN) Special Observation and Analysis Period (SOAP) Open
The discontinuous permafrost region of northwestern Canada is experiencing rapid warming resulting in dramatic land cover change from forested permafrost terrain to treeless wetlands. Extensive research has been conducted throughout this r…
View article: Permafrost thaw induced changes to runoff generation and hydrologic connectivity in low-relief, discontinuous permafrost terrains
Permafrost thaw induced changes to runoff generation and hydrologic connectivity in low-relief, discontinuous permafrost terrains Open
Recent climate warming in northwestern Canada is occurring at an unprecedented rate in recorded history and has resulted in the widespread thaw of permafrost. Where present, permafrost exerts a significant control on local hydrology, and d…