aalto1 untyped-item.component.html
Small-Scale Riverbank Erosion Experiments in Freezing and Thawing Conditions
Loading...
Access rights
openAccess
CC BY
CC BY
Creative Commons license
Except where otherwised noted, this item's license is described as openAccess
publishedVersion
URL
Journal Title
Journal ISSN
Volume Title
A1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä
This publication is imported from Aalto University research portal.
View publication in the Research portal (opens in new window)
View/Open full text file from the Research portal (opens in new window)
View publication in the Research portal (opens in new window)
View/Open full text file from the Research portal (opens in new window)
Unless otherwise stated, all rights belong to the author. You may download, display and print this publication for Your own personal use. Commercial use is prohibited.
Date
Department
Major/Subject
Mcode
Degree programme
Language
en
Pages
37
Series
Water Resources Research, Volume 61, issue 7
Abstract
Climatic warming is projected to change the duration and intensity of frozen periods in polar regions, impacting hydrology and riverbank erosion. Herein we present a series of 125 laboratory flume experiments conducted in a novel cryolab morphology facility using a small-scale Friedkin channel. We assess the influence of discharge (flow velocity), water temperature, riverbank moisture content and temperature on riverbank erosion for varying air temperatures. The riverbank topography was quantified before and after each experiment and volumetric changes were calculated, using an array of images collected via a semi-automatic camera and structure from motion method. Videos were used to determine bank edge retreat during the experiments. Surface flow velocities were measured using particle tracking velocimetry method. An infrared thermal camera aided understanding the temperature variations across the riverbank. A non-linear relationship has been identified between volumetric erosion rate and air temperature, with the highest rates (at maximum up to 1.03 cm3/s) occurring at −5.2°C overnight air temperatures during highest tested discharge conditions. Erosion rates decrease when temperatures fall below or rise above −5.2°C, but increase again (at maximum up to 0.51 cm3/s) at +4.5°C. High moisture content slowed temperature propagation, caused by flowing water, through the riverbank. Erosion occurred as blocks in freezing conditions when the moisture content exceeded 18.9%, which further promoted thermo-erosional niche development, a phenomenon observed also in polar/arctic river systems. The non-linear dependency on air temperature highlights the importance of air temperature on erosion, with further implications for erosion with climate warming.
Description
Publisher Copyright: © 2025. The Author(s).
Other note
Citation
Lotsari, E S, de Vet, M G W, Murphy, B J, McLelland, S J & Parsons, D R 2025, 'Small-Scale Riverbank Erosion Experiments in Freezing and Thawing Conditions', Water Resources Research, vol. 61, no. 7, e2024WR037569. https://doi.org/10.1029/2024WR037569
