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Balancing Between Predation Risk and Food by Boreal Breeding Ducks
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Wetlands belong to the globally most threatened habitats, and organisms depending on them are of conservation concern. Wetland destruction and quality loss may affect negatively also boreal breeding...
Caribou and Reindeer Migrations in the Changing Arctic
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Caribou and reindeer, Rangifer tarandus, are the most numerous and socio-ecologically important terrestrial species in the Arctic. Their migrations are directly and indirectly affected by the seasonal...
Continental Synchrony and Local Responses: Climatic Effects on Spatiotemporal Patterns of Calving in a Social Ungulate
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Warming temperatures and advancing spring are affecting annual snow and ice cycles, as well as plant phenology, across the Arctic and boreal regions. These changes may be linked to observed population...
Critical Summer Foraging Tradeoffs in a Subarctic Ungulate
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Summer diets are crucial for large herbivores in the subarctic and are affected by weather, harassment from insects and a variety of environmental changes linked to climate. Yet, understanding...
Decreased Carbon Accumulation Feedback Driven by Climate‐Induced Drying of Two Southern Boreal Bogs over Recent Centuries
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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...
Dissipation of Bromacil in Humic Luvic Gleysols in Northwestern Alberta
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Dissipation of bromacil in Humic Luvic Gleysols amended with cow manure was evaluated at two sites in northwestern Alberta from 1984 to 1987
Effect of Pipeline Construction on Soil Compaction in Alberta
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No clear relationships emerged between soil Orders, zones, or soil parent materials and the effect of pipeline construction on soil compaction. Soil moisture conditions appear to be more important.
Effect of Pipeline Construction on Soil Strengths of Soil Horizons in Alberta: 1990 Final Report
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At each of the fifteen 1989 study areas and at each of the eight 1988 study areas soil strength was monitored using a cone penetrometer in 15 cm depth increments to a depth of 52.5 cm.
Environmental Spaces for Palsas and Peat Plateaus are Disappearing at a Circumpolar Scale
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The anthropogenic climate change threatens northern permafrost environments. This compromises the existence of permafrost landforms, such as palsas and peat plateaus, which have been assessed to be...
Impacts of Overstripping Topsoil on Native Rangelands in Southeastern Alberta: A Literature Review
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Available information indicates that overstripping and subsequent replacement of topsoil can produce horizon characteristics similar to plow depth characteristics resulting from cultivation
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...
Increasing Fire Frequency and Severity Will Increase Habitat Loss for a Boreal Forest Indicator Species
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Climate change will lead to more frequent and more severe fires in some areas of boreal forests, affecting the distribution and availability of late-successional forest communities. These forest...
Intra- and Interspecific Variation in Spectral Properties of Dominant Sphagnum Moss Species in Boreal Peatlands
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Boreal peatlands store ~25 % of global soil organic carbon and host many endangered species; however, they face degradation due to climate change and anthropogenic drainage. In boreal peatlands...
Minimal Disturbance Pipeline Construction Procedures in Peatland Areas
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TransCanada presents an account of pipeline construction methods implemented in the boreal regions of Alberta.