Measurements of thaw front depth, surface organic layer thickness, soil moisture content and water table depth in Old Crow Flats, Yukon, Canada

Kevin Turner1, Samuel Gagnon2,3, Michelle Pearce1, Danielle Chiasson2,3, Pascale Roy-Léveillée2,3, Brent Thorne1.
1Brock University
2Université Laval
3Centre d'études nordiques

Abstract

Between June 2017 and September 2022, fieldwork was conducted in Old Crow Flats, Yukon (Canada) to study thermokarst lake and drained basin dynamics and hydrological connections in the flats. As part of this work, measurements of thaw front depth, thickness of the surface organic layer, soil water content and water table depth were made at 17 sites. Thaw front depths were made by probing soils to refusal with a rod. The thickness of the organic layer was measured by digging holes until the mineral layer was visible, and the depth to the water table was noted in that same hole. Water content was recorded with the HydroSense II Handheld Soil Moisture Sensor.

Data citation

Turner, K., Gagnon, S., Pearce, M., Chiasson, D., Roy-Léveillée, P., Thorne, B. 2023. Measurements of thaw front depth, surface organic layer thickness, soil moisture content and water table depth in Old Crow Flats, Yukon, Canada, v. 1.0. Nordicana D115, doi: 10.5885/45819CE-C45A35328D1E48A4.

Location map

Key references

  • Roy-Léveillée, Pascale, and C. R. Burn. “Old Crow Flats: Thermokarst Lakes in the Forest–Tundra Transition.” In Landscapes and Landforms of Western Canada, edited by Olav Slaymaker, 267–76. World Geomorphological Landscapes. Cham: Springer International Publishing, 2017.
    DOI: https://doi.org/10.1007/978-3-319-44595-3_19
  • Turner, Kevin W., Michelle D. Pearce, and Daniel D. Hughes. “Detailed Characterization and Monitoring of a Retrogressive Thaw Slump from Remotely Piloted Aircraft Systems and Identifying Associated Influence on Carbon and Nitrogen Export.” Remote Sensing 13, no. 2 (2021): 171.
    DOI: https://doi.org/10.3390/rs13020171
  • MacDonald, Lauren A., Kevin W. Turner, Ian McDonald, Mitchell L. Kay, Roland I. Hall, and Brent B. Wolfe. “Isotopic Evidence of Increasing Water Abundance and Lake Hydrological Change in Old Crow Flats, Yukon, Canada.” Environmental Research Letters 16, no. 12 (November 2021): 124024.
    DOI: https://doi.org/10.1088/1748-9326/ac3533

Contributors

Gray, Luke Brock University Charlie, Caleb Old Crow community member Nagwan, Clifton Old Crow community member Kyikavichik, Robert Old Crow community member

Acknowledgements

We thank Polar Knowledge Canada, the Natural Sciences and Engineering Research Council of Canada, and NASA's Arctic-Boreal Vulnerability Experiment (ABoVE) for their support. We are also grateful to the village of Old Crow, its inhabitants and the Vuntut Gwitchin First Nation for welcoming us and supporting our research.

Version history

You can request an older version by contacting nordicana@cen.ulaval.ca

Measurement sites

Site Latitude Longitude Altitude (m)
Plot 1 67.90957 -139.69718 299.542 More info
Plot 2 67.90002 -139.7335 298.422 More info
Plot 3 67.90036 -139.73568 298.587 More info
Plot 5 67.84151 -139.75759 271.152 More info
Plot 4 67.84081 -139.75571 272.319 More info
Plot 6 67.8415 -139.76108 274.99 More info
OCFF 67.91003 -139.69711 299 More info
OCFE1 67.93187 -139.44582 308 More info
OCFJD2 67.92082 -139.47784 303 More info
OCF55 67.84261 -139.76259 275 More info
OCF55T 67.84113 -139.7579 281 More info
OCFJD2V 67.92082 -139.47784 303 More info
PR2CT 67.91811 -139.40752 306 More info
PR2CM 67.92067 -139.43088 303 More info
PR2SD 67.92477 -139.37485 304 More info
PR3M 67.92916 -139.34833 303 More info
PR3C 67.92632 -139.35396 305 More info

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