Blog

A study of thermal modeling parameters and their impact on modelled permafrost responses to climate warming

A study by Khatereh Roghangar and Jocelyn Hayley has assessed the effects of thermal modeling parameters on permafrost ground response to climate warming. They analyzed how variations in depth, water content, and soil type affect predictions of future active layer depths and settlement under various climate scenarios using the soil characteristics along Hudson Bay Railway corridor.

The results indicate that, for fine-grained soils, the depth of the model is a more significant parameter than for coarse-grained soils. The water content of all soil types is a critical factor in determining the time at which permafrost thaws and the depth at which the active layer is located, as higher water content leads to larger active layer changes and more settlement in most cases. These findings have important implications for infrastructure and land use management in the Arctic region.

Roghangar, K. and Hayley, J.L. (2024). A study of thermal modeling parameters and their impact on modelled permafrost responses to climate warming. Cold Regions Science and Technology, 221, 104155, DOI: 10.1016/j.coldregions.2024.104155.

Non-destructive multi-sensor core logging allows for rapid imaging and estimation of frozen bulk density and volumetric ice content in permafrost cores

Exciting research in the Permafrost ArChives Science Laboratory (PACS Lab) at the University of Alberta has demonstrated a novel application of multi-sensor core logging for analyzing permafrost cores.

Measurements of core physical properties are typically destructive and time intensive.

Non-destructive multi-sensor core logging (MSCL) can efficiently analyze permafrost samples and provide high-resolution insights without these problems. The  new technique allows rapid imaging, measurement of bulk density and estimation of ice content in permafrost cores. The team were able to visualize cryostructures and estimate frozen bulk density, magnetic susceptibility, and volumetric ice content.

The new technique is described in the paper published in The Cryosphere by Duane Froese’s lab: Pumple, J., Monteath, A., Harvey, J., Roustaei, M., Alvarez, A., Buchanan, C., and Froese, D.: Non-destructive multi-sensor core logging allows for rapid imaging and estimation of frozen bulk density and volumetric ice content in permafrost cores, The Cryosphere, 18, 489–503, https://doi.org/10.5194/tc-18-489-2024, 2024.

Transferring Cryosphere Knowledge between Mountains Globally: A Case Study of Western Canadian Mountains, the European Alps and the Scandes

Most mountain permafrost research has been focussed on the small area of the European alps. This leads to the question, can you transfer cryosphere knowledge from the Scandes and Alps to Canada?

Emilie Stewart-Jones, has now developed a method for comparing regional climates at a coarse scale to highlight similarities and differences. Her paper “Transferring Cryosphere Knowledge between Mountains Globally: A Case Study of Western Canadian Mountains, the European Alps and the Scandes” published in the Journal of Alpine Research in November can now answer the question of whether we can transfer our knowledge of permafrost in one region to another.