Erosion potential of dynamic ice breakup in Lower Athabasca River. Part I; Field measurements and initial quantification

Highlights •Can dynamic ice breakup in lower Athabasca River generate large erosional forces? •Two-season field study furnishes unique spatiotemporal variations of water level. •Calculated local water surface slopes attain extreme values. •Initial estimates of peak bed shear stress exceed all previously known values. •Extreme erosive capacity manifested in bank and bed scour.

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Lauks Vērtība
Short Name of Publication https://www.sciencedirect.com/science/article/pii/S0165232X17301970
Deliverable Type Science Article
Program Catagory Aquatics
Program Type OSM
Autors Beltaos, S., Carter, T., Rowsell, R., and DePalma, S.G.S.
Periodical Title Cold Regions Science and Technology
Year of Publication 2018
Publishing Organization Watershed Hydrology and Ecology Research Division, Environment and Climate Change Canada
Month of Publication 5
Periodical Volumes 149
Page Range 16-28
Digital Object Identifier (DOI) 10.1016/j.coldregions.2018.01.013
Online ISBN/ISSN 1872-7441
Print ISBN/ISSN 0165-232X
Recomended Citation Beltaos, S., Carter, T., Rowsell, R., & DePalma, S. G. S. (2018). Erosion potential of dynamic ice breakup in Lower Athabasca River. Part I: Field measurements and initial quantification. Cold Regions Science and Technology, 149, 16–28. doi:10.1016/j.coldregions.2018.01.013
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