Principal Investigator:Tank, Suzanne E Licensed Year(s):
2017
2016 Summary:
The objective of this study is to determine the effect of fire on water quality within the southern NWT landscape. The research team will work across the Taiga Plains and Taiga Shield ecoregions. Differences in landscape between these regions will affect the catchment response to fire. The team will also target catchments with variable permafrost extent, and wetland/lake coverage.
The research ...
Principal Investigator:Spence, Christopher Licensed Year(s):
2017
2016201220112010200920082007 Summary:
It is the objective of this research to determine the water cycle processes acting in watersheds that could affect the streamflow response and water chemistry of Taiga Shield streams.
The proposed work will take place within a research basin framework. The proposed watershed, the upper reaches of Baker Creek, is a typical Canadian Shield stream that drains 150 km2 into Great Slave Lake. There ...
Principal Investigator:Bond, Matthew J Licensed Year(s):
2016
Summary:
The objective of this research is to determine whether permafrost thaw in the Canadian north is resulting in the release of historic radionuclides to surface waters. The results of this study will be incorporated into a larger model of radionuclide fate and transport in the Canadian north.
Field work will involve sampling surface water (triplicate 500 mL samples), groundwater seepage (triplicat...
Principal Investigator:Charette, Matthew Licensed Year(s):
2016
Summary:
The objectives are to measure a suite of trace elements and isotopes (TEIs) in the active layer and permanently frozen layer of permafrost cores sampled near the Mackenzie River, and to compare these concentrations to those observed in submarine groundwater discharge and Mackenzie River discharge in order to determine whether permafrost-associated TEIs are being transported to the coastal Arctic. ...
Principal Investigator:Quinton, William L. Licensed Year(s):
2016
20152014201320122011201020092008200720062005200420032001 Summary:
Understanding the integrated eco-hydrological behaviour of ecosystems in the context of thawing permafrost is a major challenge. To meet this, the research team will measure the present surface and near-surface water supplies and their inter-annual variability assuming a condition of no permafrost thaw. The team will also develop new knowledge on the eco-hydrology of the major ecosystems (i.e. bog...
Principal Investigator:Quinlan, Roberto Licensed Year(s):2017
2016
201520142013 Summary:
This study will examine the effects of permafrost and flooding on the ecological structure and carbon exchange of contrasting lakes in the Mackenzie River Delta. Permafrost thaw in lake catchments may cause increased transport of organic carbon and dissolved nutrients to lakes with effects on the hydrology and water chemistry of lake environments. Patterned ground marked by ice-wedge polygons is f...
Principal Investigator:Laurent, Cyrielle C Licensed Year(s):
2015
Summary:
The short term objectives for this project are to:
- Assess permafrost as a possible origin of mercury contamination;
- Measure mercury content in permafrost samples;
- Engage the community to exchange traditional and scientific knowledge to better understand relationships between country food, water quality, and permafrost degradation from a contamination perspective; and
- Use traditional la...
Principal Investigator:Lacelle, Denis Licensed Year(s):
2015
Summary:
Thaw slumps are one of the most dramatic thermokarst features in permafrost regions. The number of thaw slumps on Banks Island has more than tripled in recent decades and it is likely that this change is altering terrestrial and aquatic ecosystems. This multidisciplinary research project investigates the short- (1960s-present day) and long-term (Medieval Warm Period to today) impacts of permafrost...
Principal Investigator:Wookey, Philip A Licensed Year(s):
2014
2013 Summary:
This research aims to understand what factors affect 1) the amount of carbon stored in tundra soils, and 2) the conversion of this soil carbon into greenhouse gases (carbon dioxide and methane). In particular, the research team wants to understand how hydrology (which is the distribution and movement of water in soils and streams) might affect the carbon cycle under future global warming. This inc...
Principal Investigator:Beilman, David W Licensed Year(s):
2013
Summary:
The research team seek to understand carbon dynamics during warm climate intervals in the Arctic: the Holocene Thermal Maximum (HTM) the warmest pre-industrial interval ranging in timing from 10 ka (thousands of years before present) with maximum seasonality to 6 ka with reduced seasonality, and the Medieval Climate Anomaly (MCA) at ~1 ka with similar seasonality as today. By studying peat cores f...