Shore-based monitoring of flow dynamics in a steep bedrock canyon river

The pace of landscape evolution is set by bedrock erosion in canyons. This phenomenon occurs by various geological processes including plucking of bedrock blocks and abrasion by saltating bedload and suspended load in highly turbulent flows. For a better understanding of the river flow characteristi...

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Main Authors: Ansari Saber, Rennie Colin D., Venditti Jeremy G., Kwoll Eva, Fairweather Kirsti
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20184006025
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author Ansari Saber
Rennie Colin D.
Venditti Jeremy G.
Kwoll Eva
Fairweather Kirsti
author_facet Ansari Saber
Rennie Colin D.
Venditti Jeremy G.
Kwoll Eva
Fairweather Kirsti
author_sort Ansari Saber
collection DOAJ
description The pace of landscape evolution is set by bedrock erosion in canyons. This phenomenon occurs by various geological processes including plucking of bedrock blocks and abrasion by saltating bedload and suspended load in highly turbulent flows. For a better understanding of the river flow characteristics in bedrock rivers, a comprehensive study of flow dynamics was undertaken in Black Canyon in the Fraser River, British Columbia. We used shore-based video imagery of the river to study surface flow dynamics. The shore-based monitoring system consisted of a Campbell Scientific camera mounted at the top of the canyon walls. We monitored the water surface boils due to upwelling and determined river surface flow velocities from the shore-based imagery. Automatic detection of the upwelling surface boils leads to a better understanding of the secondary circulation patterns and flow structures in this large steep river bedrock canyon. The data collection and analytical procedures developed in this research are cost-effective tools for remotely determining flow dynamics, which can be applied to other rivers.
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spelling doaj.art-738565634fe542348dd628cfe01857b92022-12-21T20:01:40ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01400602510.1051/e3sconf/20184006025e3sconf_riverflow2018_06025Shore-based monitoring of flow dynamics in a steep bedrock canyon riverAnsari SaberRennie Colin D.Venditti Jeremy G.Kwoll EvaFairweather KirstiThe pace of landscape evolution is set by bedrock erosion in canyons. This phenomenon occurs by various geological processes including plucking of bedrock blocks and abrasion by saltating bedload and suspended load in highly turbulent flows. For a better understanding of the river flow characteristics in bedrock rivers, a comprehensive study of flow dynamics was undertaken in Black Canyon in the Fraser River, British Columbia. We used shore-based video imagery of the river to study surface flow dynamics. The shore-based monitoring system consisted of a Campbell Scientific camera mounted at the top of the canyon walls. We monitored the water surface boils due to upwelling and determined river surface flow velocities from the shore-based imagery. Automatic detection of the upwelling surface boils leads to a better understanding of the secondary circulation patterns and flow structures in this large steep river bedrock canyon. The data collection and analytical procedures developed in this research are cost-effective tools for remotely determining flow dynamics, which can be applied to other rivers.https://doi.org/10.1051/e3sconf/20184006025
spellingShingle Ansari Saber
Rennie Colin D.
Venditti Jeremy G.
Kwoll Eva
Fairweather Kirsti
Shore-based monitoring of flow dynamics in a steep bedrock canyon river
E3S Web of Conferences
title Shore-based monitoring of flow dynamics in a steep bedrock canyon river
title_full Shore-based monitoring of flow dynamics in a steep bedrock canyon river
title_fullStr Shore-based monitoring of flow dynamics in a steep bedrock canyon river
title_full_unstemmed Shore-based monitoring of flow dynamics in a steep bedrock canyon river
title_short Shore-based monitoring of flow dynamics in a steep bedrock canyon river
title_sort shore based monitoring of flow dynamics in a steep bedrock canyon river
url https://doi.org/10.1051/e3sconf/20184006025
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AT vendittijeremyg shorebasedmonitoringofflowdynamicsinasteepbedrockcanyonriver
AT kwolleva shorebasedmonitoringofflowdynamicsinasteepbedrockcanyonriver
AT fairweatherkirsti shorebasedmonitoringofflowdynamicsinasteepbedrockcanyonriver