Advances in River Ice Research

A special issue of Glacies (ISSN 2813-8740).

Deadline for manuscript submissions: 30 June 2027 | Viewed by 1548

Editor


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Guest Editor
Department of Civil and Environmental Engineering, Clarkson University, Potsdam, NY 13699-5710, USA
Interests: river ice; river hydraulics; sediment transport; ice jam and flooding; mathematical modeling; freeze up; frazil and anchor ice
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Special Issue Information

Dear Colleagues,

In cold-region water resources management, river ice is a critical factor—its evolution from freeze-up to breakup and its impacts on channel morphology and water quality involve thermal and mechanical processes that are not typically the focus of traditional river hydraulics and hydrology. The impact of climate change has posed new research challenges, including the need to understand channel morphology in permafrost regions, flow and sediment transport in response to changing glacial conditions, outburst floods from the moraine dams of glacial lakes (GLOFs), and the decline of freshwater resources associated with glacier retreat. This Special Issue will explore all aspects of river ice hydraulics and hydrology, how river ice impacts the environment and ecology, and how climate change affects river ice processes.

Prof. Dr. Hung Tao Shen
Guest Editor

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Keywords

  • river ice
  • frazil and anchor ice
  • freeze-up
  • breakup
  • ice jam and flooding
  • sediment transport and channel morphology
  • environmental and ecological effects
  • climate change effects
  • mathematical modeling
  • river ice in Arctic and Subarctic regions
  • GLOFs

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Published Papers (1 paper)

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Research

16 pages, 7107 KB  
Article
Modelling and Evaluating the Sensitivity of River Ice Thickness in the Mackenzie River Basin to a Changing Climate
by Yonas B. Dibike, Ethan James, Laurent de Rham and Daniel L. Peters
Glacies 2026, 3(3), 11; https://doi.org/10.3390/glacies3030011 - 12 Aug 2026
Viewed by 202
Abstract
Climate change is altering river-ice regimes across northern basins, with important implications for river hydraulics, infrastructure and flood hazards. In this study, river-ice thickness was simulated at 59 hydrometric stations across the Mackenzie River Basin (MRB) for the period 1980–2024 using a thermodynamically [...] Read more.
Climate change is altering river-ice regimes across northern basins, with important implications for river hydraulics, infrastructure and flood hazards. In this study, river-ice thickness was simulated at 59 hydrometric stations across the Mackenzie River Basin (MRB) for the period 1980–2024 using a thermodynamically based Stefan ice-growth model driven by daily mean air temperature from the Canadian Surface Reanalysis (CaSR). Cumulative freezing degree-days (CFDD) were derived from 10 km gridded air temperature fields, and site-specific Stefan coefficients (α) were calibrated using measured average ice thickness data from the updated Canadian River Ice Database (CRID). The model reproduced observed river-ice thickness with good accuracy, achieving a median coefficient of determination (R2) of 0.96 across all stations. Basin-wide analysis revealed statistically significant warming in annual and seasonal air temperatures, averaging 0.37 °C decade−1, accompanied by widespread declines in CFDD. These climatic changes translated into widespread reductions in simulated annual maximum river-ice thickness, averaging 1.1 cm decade−1, together with a shift toward earlier peak ice thickness. Sensitivity analyses with uniform air-temperature increases of +1 to +3 °C further indicated average reductions in maximum river-ice thickness of up to 10 cm. Overall, the results demonstrate that the Stefan ice-growth model provides a robust and computationally efficient framework for basin-scale assessment of river-ice thickness and show that river ice across the MRB is already responding to climate warming, with continued thinning expected under projected future warming scenarios. Full article
(This article belongs to the Special Issue Advances in River Ice Research)
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