Determining ice-jam stage frequency distributions of an ungauged river reach using dendrogeomorphological data

Author:

Lubiniecki Teagan12,Lindenschmidt Karl-Erich2,Laroque Colin P.1,Rokaya Prabin23

Affiliation:

1. Mistik Askiwin Dendrochronology Laboratory, 5C74, Agriculture Building University of Saskatchewan, Saskatoon, Canada

2. Global Institute for Water Security, School of Environment and Sustainability, University of Saskatchewan, Saskatoon, Canada

3. Watershed Resilience and Transboundary Waters, Alberta Environment and Protected Areas, Calgary, Canada

Funder

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

Publisher

Informa UK Limited

Reference30 articles.

1. Beltaos, S., ed. 1995. River ice jams. Highlands Ranch, CO: Water Resources Publications, LLC.

2. Impacts of recurring ice jams on channel geometry and geomorphology in a small high-boreal watershed

3. Characterization of microplastics and anthropogenic fibers in surface waters of the North Saskatchewan River, Alberta, Canada

4. Dahl T. Gibson S. and Webber J. B. 2017. Using dendrochronology to identify historic ice jams. In: Proc. CGU HS committee on river ice processes and the environment 19th workshop on the hydraulics of ice-covered rivers Whitehorse . Alberta CA: Committee on River Ice Processes and the Environment.

5. Ice-Jam Flood Risk Assessment and Hazard Mapping under Future Climate

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