Icing and aufeis in cold regions II: consequences and mitigation

Author:

Turcotte B.1ORCID,Dubnick A.1,McKillop R.2

Affiliation:

1. Climate Change Research, YukonU Research Centre, Yukon University, 500 University Drive, PO Box 2799, Whitehorse, Yukon Y1A 5K4, Canada

2. Palmer, 470 Granville Street, Suite 630, Vancouver, BC V6C 1V5, Canada

Abstract

The process of icing and the resulting layered ice masses, called aufeis, are caused by the freezing of overflow originating from groundwater or surface water. Aufeis can directly impact infrastructure and property, most commonly through winter ice formation and spring flooding within, against, and on the surface of hydraulic structures and transportation infrastructure. They also represent a safety concern for drivers. This geohazard often needs to be managed proactively and efficiently to mitigate associated risks. This paper provides an overview of the consequences of aufeis in northwestern Canada. A total of 50 existing and novel icing and aufeis mitigation approaches are described and classified. The context of applicability for each approach is identified, considering the source of water, the type of infrastructure, and its role in the formation of aufeis. Finally, future research avenues to support the development or improvement of aufeis risk reduction techniques are presented.

Funder

Transport Canada

ArcticNet North-by-North program

Publisher

Canadian Science Publishing

Subject

General Environmental Science,Civil and Structural Engineering

Reference27 articles.

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2. Mobilisation of heavy metals by deicing salts in a roadside environment

3. Calmels F., Doré G., Kong X., Roy L., Lemieux C., Horton B. 2016. Vulnerability of the north Alaska highway to permafrost thaw: design options and climate change adaptation. Northern Climate ExChange, Yukon Research Centre, Yukon College. 130p.

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1. Preface to the special issue on river ice and infrastructure;Canadian Journal of Civil Engineering;2024-02-01

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