NWT RESEARCH DATABASE

Regions: Inuvialuit Settlement Region

Tags: physical sciences, permafrost, climate change, wedge ice

Objective(s): To understand the rate of ground warming in permafrost due to climate change and to measure the changes in ground surface characteristics that are occurring as a result.

Project Description: The objective of this research is to understand the rate of ground warming in permafrost due to climate change and to measure the changes in ground surface characteristics that are occurring as a result. In particular, the research team are interested in changes in ground temperature, in the depth of the active layer, and in subsidence of the ground. The team are also interested in measuring how quickly ice wedges are developing ponds and then melting out underneath, leading to degradation of tundra polygons. The project continues investigations in the western Arctic since 1987, and so an important objective is to keep some of the long-term records that the team have as continuous series, so that the conclusions are based on firm evidence. The methods primarily consist of: 1) drilling holes in the ground to depths of up to 15 m with a water jet drill and installing thermistor cables with data loggers to measure ground temperatures; 2) installing bench marks for repeated surveys to determine how much the ground is settling or moving laterally; 3) monitoring the depth of thaw in the ground; 4) measuring snow depths and snow densities; 5) measuring lake-ice thicknesses; and, 6) measuring the temperature in ponds and other water bodies. When the research team go to the field sites levelling surveys are made, the research team retrieve data loggers and down load them, samples are collected from soil pits, and holes are drilled to 3 or 4 m depth to collect samples from permafrost. Occasionally the research team make resistivity surveys of near-surface conditions. Close attention is also paid to changes in vegetation at the sites, and surveys of vegetation composition and abundance may be made. At Illisarvik the research team also place little shock loggers in the ground, which monitor miniearthquakes, because the team are interested in detecting when ice wedges crack. In 2015 wildlife cameras were placed at Illisarvik in front of a snow stake in order to see if snow accumulation can be monitored at the site. The research team will make an annual visit to a Hunters and Trappers Committee (HTC) meeting to present the work both in the delta and on the Yukon North Slope and to discuss suggestions as to what the HTC might consider a priority for research on permafrost. The team have a long-term monitoring program established with Aurora Research Institute (ARI) that involves their technicians going to a site near Inuvik and another in the delta to collect ground temperatures. From time to time the ARI asks the research team to give presentations in schools and communities, and we have been happy to do that. In the next 5 years the team plan to visit a HTC meeting once each year to present the work, ask for comments, and discuss any concerns. The team particularly hope to visit Aklavik because of research on the Yukon North Slope, in collaboration with Parks Canada, and on Herschel Island. The research team are also more than willing to answer any questions that arise from community members at other times. The fieldwork for this study will be conducted from April 12, 2018 to August 17, 2018.