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groundwater dischargesnowmelt
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2 record(s) found in the location "Inuvialuit Settlement Region" (multi-year projects are grouped):
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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 Trail Valley Creek site will be accessed by Twin Otter, helicopter and snowmobile, while the Havikpak Creek site will be accessed by foot and snowmobile. We plan to have a small field crew at each site to measure the amount of snow on the ground in the middle of April, and to again return to measure snowmelt and the streamflow in mid to late May. Actual timing of the spring melt trip will depe...
Licensed Year(s): 2005 2004 2003 2002 2001 2000 1999 1998 1997 1996 1995 1994 1993 1992 1990
Summary: The Trail Valley Creek site will be accessed by Twin Otter, helicopter and snowmobile, while the Havikpak Creek site will be accessed by foot and snowmobile. We plan to have a small field crew at each site to measure the amount of snow on the ground in the middle of April, and to again return to measure snowmelt and the streamflow in mid to late May. Actual timing of the spring melt trip will depe...
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...
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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