4 record(s) found in the location "Inuvialuit Settlement Region" (multi-year projects are grouped):
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Impact of esturine cation exchange reactions on the true carbon export budget of the Mackenzie river.
Principal Investigator: Tipper, Edward
Licensed Year(s): 2022
Summary: This licence has been issued for the scientific research application No.5269. This project will determine the impact of cation exchange between minerals and surface waters and quantify the release from the exchange pool as fresh water enters the oceans. This will be achieved through careful sampling of suspended sediment and water from regions of fresh to saline waters of the Mackenzie River. ...


Long-term hydrological dynamics of Canada’s largest watershed: Climate controls on water quantity of the Mackenzie River Basin
Principal Investigator: Galloway, Jennifer
Licensed Year(s): 2020
Summary: This licence has been issued for the scientific research application No.4705. The Mackenzie River Basin (MRB) is one of the largest cold-water, intact boreal ecosystems in the world and has unique Earth-system’s processes associated with sea ice formation, global circulation of deep ocean currents, carbon storage, and biogeochemical cycling. This unique global resource is also critical for supp...


Snow Accumulation/Runoff in High Latitude Permafrost Basins
Principal Investigator: Marsh, Philip
Licensed Year(s): 2005 2004 2003 2002 2001 2000 1999 1998 1997 1996 1995 1994 1993 1992 1990
Summary: The primary objective of this project is to develop improved understanding of the fluxes of water and energy in northern regions, and to develop improved computer models of these processes. The Trail Valley Creek site will be accessed by helicopter and s...


Water Quality in the Richardson Mountain catchments
Principal Investigator: CLARK, Ian D.
Licensed Year(s): 1997
Summary: The objectives of this research are to study the chemistry of the groundwaters that flow into the Little Fish River near the Cache Creek overwintering hole. The role of carbonate rocks is important as there is a lot of subsurface flow in this rock type. The presence of the aufeis (winter icing) on Cache Creek is a sign of groundwater flow, and is one of the reasons that this site was chosen. We...


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