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A Synthesis of Three Decades of Eco-Hydrological Research at Scotty Creek, NWT, Canada
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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...
A Tale of Two Roads: Consequences of Peat Conditions and Construction Practices on Peatland Effects, Reclaimability, and Best Practice Development
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This talk explores what needs to inform road construction decisions, including evaluating where roads should be built and what practices should be used based on peat conditions.
Comparison of Site Preparation and Revegetation Strategies within a Sphagnum-Dominated Peatland Following Removal of an Oil Well Pad
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
COSIA In-Situ Oil Sands Shared Practices for Working in and Around Wetlands
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This report compiles a toolbox of shared practices currently in use by COSIA companies, or which have been used but were found to be unsuccessful.
Cross-Scale Controls on Carbon Emissions from Boreal Forest Megafires
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Greater Variation in Boreal Plant Community Composition and Community-level Traits at Local Than Regional Scale
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Questions Rapid climate change in northern latitudes is expected to influence plant functional traits of the whole community (community-level traits) through species compositional changes and/or trait...
Groundwater in Peat and Peatlands
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Peatlands are wetlands with soil comprised of undecomposed remains of plants that accumulate in such a way that both responds to and controls the flux and storage of surface water and groundwater, as...
Increasing Contributions of Peatlands to Boreal Evapotranspiration in a Warming Climate
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The response of evapotranspiration (ET) to warming is of critical importance to the water and carbon cycle of the boreal biome, a mosaic of land cover types dominated by forests and peatlands. The...
On the Use of Mulching to Mitigate Permafrost Thaw due to Linear Disturbances in Sub-Arctic Peatlands
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The presence or absence of permafrost strongly influences the hydrology and ecology of northern watersheds. Resource exploration activities are currently having profound effects on hydrological and...
Paleolimnological Assessment of Past Hydro-ecological Variation at a Shallow Hardwater Lake in the Athabasca Oil Sands Region Before Potential Onset of Industrial Development
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Effective environmental monitoring requires knowledge of inherent natural variation. In the absence of pre-development monitoring of aquatic ecosystems, paleolimnological approaches have been...
Planning for Wetland Function and Reclamation Success in Road Design
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This research poster describes an overview of technical methods, peat properties and considerations, and development outcomes for linear feature (road) construction planning and development. Presented...
Spatial and Temporal Variation in Forest Transpiration Across a Forested Boreal Peatland Complex
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Transpiration is a globally important component of evapotranspiration. Careful upscaling of transpiration from point measurements is thus crucial for quantifying water and energy fluxes. In spatially...
Spatial Variation in Nutrient Dynamics Among Five Different Peatland Types in the Alberta Oil Sands Region
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Wetlands are found extensively throughout the Western Boreal Plain, a region under pressure because of disturbance by the oil and gas industries. To understand how wetland systems may respond to...
Temperature, Moisture and Freeze–thaw Controls on CO2 Production in Soil Incubations From Northern Peatlands
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Peat accumulation in high latitude wetlands represents a natural long-term carbon sink, resulting from the cumulative excess of growing season net ecosystem production over non-growing season (NGS)...
The Biophysical Climate Mitigation Potential of Boreal Peatlands During the Growing Season
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Peatlands and forests cover large areas of the boreal biome and are critical for global climate regulation. They also regulate regional climate through heat and water vapour exchange with the...
The Hydrology of Interconnected Bog Complexes in Discontinuous Permafrost Terrains
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In the zone of discontinuous permafrost, the cycling and storage of water within and between wetlands is poorly understood. The presence of intermittent permafrost bodies tends to impede and re-direct...