• Arctic and Sub-arctic Lowlands
• Trail Valley Creek
• Havikpak Creek
• Scotty Creek
• Baker Creek

11. Trail Valley Creek, NWT

Meteorological station at Trail Valley Creek (photo: Phil Marsh)

Location and Physical Characteristics

• Located at roughly 68°45'N, 133°30'W, Trail Valley Creek is 50 km north-northeast of Innuvik, NWT, and 80 km south of the Beaufort Sea, Arctic Ocean;
• The basin is 63 km² in area and is dominated by gently rolling hills and some deeply incised river valleys;
• Elevations range 50 m to 180 m above seal level and the terrain has a mean slope of 3° (maximum slope 30°);
• Located at the northern edge of the boreal forest - tundra ecotone, vegetation of dominant upland tundra areas consists mostly of grasses, lichens, and mosses. Moister hillslopes and valley bottoms support shrub tundra with vegetation ranging from 0.5 m to 3 m in height. There are sparse pockets of black spruce forest throughout the basin;
• Climate is characterized by short summers and long cold winters, with an 8-month snow-cover period.  Mean annual air temperature is about -10 °C and annual precipitation is about 266 mm (66% of which is snow);  
• Trail Valley Creek is in the continuous permafrost zone and active layer thickness ranges from 0.3 m to 0.8 m.     

History

• Trail Valley Creek has been a focal hydrological research basin since 1992, where the National Water Research Institute (NWRI) has operated a meteorological station since that time;
• The Water Survey of Canada (WSC) has operated a gauging station at the outlet of the basin since 1979;
• Trail Valley Creek represented an important research basin contributing to the objectives of the Mackenzie GEWEX Study (MAGS) and the IP3 Network.  

Current Science Focus and Instrumentation

• Long-term hydrological research in the Sub-Arctic to Arctic transition region (Taiga to Tundra ecoregions);
• Research is currently focused on the integrated dynamics and variability of vegetation, snow, energy balance, active layer depth, thermokarst, soil water storage, and runoff;
• Important insights are being developed on the expansion of shrub Tundra and its associated effects;
• Instrumentation consists of:
  • Meteorological stations in 3 main Tundra and tall shrub sites measuring soil temperature, soil moisture, air temperature, wind speed and direction, incoming/outgoing short- and long-wave radiation, precipitation, and eddy covariance flux measurement for key periods;
  • WSC streamflow measurement at the outlet of Trail Valley Creek;
  • Other more recent stations set up (e.g. flux station near lake in upper part of basin, WMO SPICE (Solid Precipitation Intercomparison Experiment) site in lower part of basin);
• Field observations including:
  • Distributed end-of-winter snow surveys, detailed snowpack monitoring (GEONOR snowfall measurement, snow pillow, Cosmic ray SWE measurement), ground-based and remote sensing (Lidar, Radar) methods for spatial variability of soil moisture, soil temperature, and SWE;   
• All meteorological towers to be upgraded for flux observations of water, energy, carbon, and to include 15 m deep well casings to allow installation of thermistors for monitoring of permafrost conditions.       

Other Resources and Further Information

• Data catalogue for Trail Valley Creek;
• The IP3 website (http://www.usask.ca/ip3/) contains some further information on Trail Valley Creek as well as a subset of available data;
• The Taiga Plains Research Network website (http://taigaplains.ca/) also contains some further information on the site and provides details about related projects across this northern region;
• Presentation on Trail Valley Creek and Havikpak Creek at CCRN's Targeted Process Studies Workshop, Hamilton, ON, September 12-13, 2013  

For further information contact:

Isolated stand of sparse black spruce forest within Trail Valley Creek (photo: Phil Marsh)