Preprints
https://doi.org/10.5194/egusphere-2025-975
https://doi.org/10.5194/egusphere-2025-975
12 Mar 2025
 | 12 Mar 2025
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Interannual variability in air temperature and snow drive differences in ice formation and growth

Arash Rafat and Homa Kheyrollah Pour

Abstract. Recent warming of northern, high-latitude regions has raised alarms for the safe and efficient use of frozen lakes for winter transportation and recreation. This concern is significant in Canada’s Northwest Territories (NWT), where seasonally constructed roads over lakes, rivers, and land (winter roads) span thousands of kilometers and act as vital links to isolated communities and resource development projects. Current climate change and weather variability is altering the evolution of lake ice, challenging predictions of freeze-up, ice growth, and ice decay. The accurate simulation of ice evolution is imperative for safe and efficient planning, operation, and maintenance of winter roads under a changing climate and heightened weather variability. This is particularly significant in the early winter period when ice road planning and design is undertaken. Here, we investigate the effects of weather variability on ice formation, growth, and evolution in a small lake near Yellowknife, NWT, Canada. High-resolution measurements of air, snow, ice, and water temperatures were collected continuously from a floating research station between October and December in 2021, 2022, and 2023 and variability in ice evolution and weather examined. Combinations of above and below average snowfall and winter air temperatures resulted in variability of up to 17 days in freeze-up dates (FUD) and 8 days in freeze-up durations. End of December ice thicknesses (hi) varied up to 12 cm, while the duration between the FUD and hi=30 cm varied up to 10 days. hi were effectively simulated (RMSE=1.11–2.33 cm) using empirical relationships developed using cumulative freezing degree days (CFDD) and seasonally cumulative snowfall (ST), while snow-ice thicknesses simulated (RMSE=0.83–1.21 cm) using CFDD and daily snowfall. Developed relationships between air temperatures, snow, and ice thicknesses can be used for predicting minimum ice thicknesses required for commencing ice road construction, and to assist in the effective management of construction activities.

Competing interests: One of the authors is a member of the editorial board of The Cryosphere.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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Arash Rafat and Homa Kheyrollah Pour

Status: open (until 23 Apr 2025)

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Arash Rafat and Homa Kheyrollah Pour
Arash Rafat and Homa Kheyrollah Pour

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Short summary
Climate change in Canada’s Northwest Territories (NWT) is making lake ice less predictable, thereby affecting ice road safety for northern communities. In this study, observations of significant changes in ice formation and growth between Oct.–Dec. 2021–2023 in a small NWT lake are related to changes in local snowfall and air temperatures. Collected data was used to develop simple models that can be applied for ice road planning, construction, and design under future and current climate change.
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