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14th Annual Woo Water Lecture
Event
Event Date and Time
November 28th, 2023 at 3:30pm EST to November 28th, 2023 at 4:30pm EST
Hamilton, ON
Contact
Organization
A Hydrogeological Landscape Framework to Identify Peatland Wildfire Smouldering Hot Sports
Resource
Northern peatlands are important global carbon stores, but there is concern that these boreal peat reserves are at risk due to increased fire frequency and severity as predicted by climate change...
A Hydrogeological Landscape Framework to Identify Peatland Wildfire Smouldering Hot Spots
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This study used a combination of field measurements and modelling to assess the vulnerability of peat to smouldering in the Utikuma Region Study Area, Alberta, Canada.
Advances in Wetland Hydrology: The Canadian Contribution Over 75 Years
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Wetlands are an integral part of the Canadian landscape, providing crucial ecohydrological services with globally significant benefits. Over the past 75 years, Canadian scientists have emerged as...
An Assessment of Sampling Designs Using SCR Analyses to Estimate Abundance of Boreal Caribou
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Abstract Accurately estimating abundance is a critical component of monitoring and recovery of rare and elusive species. Spatial capture–recapture (SCR) models are an increasingly popular method for...
Biting Flies and Activity of Caribou in the Boreal Forest
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Habitat loss has been implicated in the decline of forest-dwelling caribou ( Rangifer tarandus caribou), but it is unknown how biting insects, potentially important components of boreal forest habitat...
Controls on Plot-Scale Growing Season CO2 and CH4 Fluxes in Restored Peatlands: Do They Differ From Unrestored and Natural Sites?
Resource
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...
Deciduous Tree Species Classification Using Object-Based Analysis and Machine Learning with Unmanned Aerial Vehicle Multispectral Data
Resource
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...
Development of Genomic Resources for Cattails (Typha), a Globally Important Macrophyte Genus
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A critical knowledge gap in freshwater plant research is the lack of genetic tools necessary to answer fundamental questions about their demographic histories, adaptation and phylogenetic...
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
DNA Metabarcoding of Faecal Pellets Reveals High Consumption of Yew (Taxus spp.) by Caribou (Rangifer tarandus) in a Lichen-poor Environment
Resource
Woodland caribou ( Rangifer tarandus caribou) are threatened in Canada because of the drastic decline in population size caused primarily by human-induced landscape changes that decrease habitat and...
Does Connectivity Exist for Remnant Boreal Caribou (Rangifer tarandus caribou) Along the Lake Superior Coastal Range? Options for Landscape Restoration
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Study of whether animal movement can be discerned, using genetic population and relatedness analyses, within and beyond the Lake Superior Coastal Range.
Ecohydrology by Thinking Outside the Bog: Shifting Paradigms in an Era of Shifting Peatland Ecosystems
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Large shifts in vegetation distributions are occurring worldwide and at unprecedented rates. The most extreme of these regime shifts are expected to occur at ecosystem boundaries of both semi-arid and...
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.