Geography & Environment Publications

Document Type

Article

Publication Date

10-12-2018

Volume

44

Issue

3

Journal

Earth Surface Processes and Landforms

First Page

752

Last Page

765

URL with Digital Object Identifier

https://doi.org/10.1002/esp.4528

Abstract

Planimetric change was measured on daily hydrographs over two meltwater seasons using time-lapse images of the proglacial, gravel, braided, Sunwapta River, Canada. Significant planimetric change occurred on 10-15 days per year. Area of planimetric change correlated with peak and total daily meltwater hydrograph discharge. A clear threshold discharge can be identified below which no planform activity occurs, an intermediate range over which change occurs conditionally, and a peak flow range at which significant change always occurs. Field conditions were reproduced in a physical model in a laboratory flume. Photogrammetric DEMs of bed morphology and measurements of bedload output were made for each hydrograph experimental run. The physical model results for planimetric change had a threshold discharge for change, and trend with discharge, similar to the field data. The model data also show that planimetric change correlates strongly with volumes of erosion/deposition measured from successive DEMs, and with bedload transport rate. The relation between planimetric change and topographic change is also apparent from previous cross-section surveys at the field site. The results highlight the planimetric dynamics of braiding rivers in relation to discharge forcing, and the relationship between planimetric change, morphological change, and bedload transport in braided rivers. This also points to the potential use of measurements of planimetric change from time-lapse imagery as a low-cost method for high-frequency monitoring for braiding dynamics and also a surrogate for bedload transport measurement.

Notes

"This is the peer reviewed version of the following article: Middleton, L., Ashmore, P., Leduc, P. & Sjogren, S. (2019). Rates of planimetric change in a proglacial gravel-bed braided river: Field measurement and physical modeling. Earth Surface Processes and Landforms, 44(3), 752-765, which has been published in final form at https://doi.org/10.1002/esp.4528. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions."

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