Coupled evolution of rivers and floodplains
Coupled evolution of rivers and floodplains
River-floodplains are coupled systems in which the conveyance and cycling of sediment over centuries to millennia set the morphological and sedimentological boundary conditions that control fluvial processes over shorter time periods (e.g., years to decades). Although this is well known, understanding how such processes are coupled over short and long timescales remains a significant challenge. Moreover, fluvial geomorphology as a discipline has, arguably, focused more on the study of within-channel processes and dynamics, with less attention given to how river-floodplain interactions and feedbacks control the functioning of the wider river corridor (i.e., channel-belt). Growing concern over the potential impacts of 21st century environmental change (e.g., on river morphology, flood conveyance and floodplain ecosystems) highlights a pressing need to address this knowledge gap.
This study applies a physically-based morphodynamic model to investigate the coupled evolution of channel-floodplain systems. The model solves the shallow water equations for in-channel and overbank flows, together with equations representing fine and coarse sediment transport, channel migration and floodplain development. Simulations are run over time periods sufficient for the floodplain to be reworked (and hence reconstructed) by the model. Simulation results provide new insights into: (i) the relative importance of river gradient, sediment flux and bank erodibility as controls on channel migration rates; (ii) the factors that determine the mechanisms and frequency of channel cutoffs; (iii) the degree to which floodplain dynamics (e.g., floodplain reworking and construction) control both floodplain topography and river pattern; (iv) the relative importance of bedload versus suspended load in determining overall fluvial system behaviour; and (v) the challenges involved in simulating these effects using numerical models.
Nicholas, Andrew
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Aalto, Rolf
78fbaea1-c10c-44da-a6a1-6f0a1eeff388
Ashworth, Phil
4332f573-928f-408f-aa8f-816338ecad78
Best, Jim
e9955f54-34ef-42be-82f8-8a4e543b7093
Bruckner, Muriel
b14fccdf-9a6b-4394-b3e2-b08162e0db37
Gasparotto, Andrea
e47e07cd-358a-4ee2-a3bd-5ee836fa5f0e
Almeida, Renato Paes de
95bdbc13-2c4d-471d-a8f3-da1ba73cdf75
9 March 2024
Nicholas, Andrew
6406b349-a2c8-4dc6-9d13-6aa70154229a
Aalto, Rolf
78fbaea1-c10c-44da-a6a1-6f0a1eeff388
Ashworth, Phil
4332f573-928f-408f-aa8f-816338ecad78
Best, Jim
e9955f54-34ef-42be-82f8-8a4e543b7093
Bruckner, Muriel
b14fccdf-9a6b-4394-b3e2-b08162e0db37
Gasparotto, Andrea
e47e07cd-358a-4ee2-a3bd-5ee836fa5f0e
Almeida, Renato Paes de
95bdbc13-2c4d-471d-a8f3-da1ba73cdf75
Nicholas, Andrew, Aalto, Rolf, Ashworth, Phil, Best, Jim, Bruckner, Muriel, Gasparotto, Andrea and Almeida, Renato Paes de
(2024)
Coupled evolution of rivers and floodplains.
EGU General Assembly 2024, , Vienna, Austria.
14 Mar - 19 Apr 2024.
(doi:10.5194/egusphere-egu24-12515).
Record type:
Conference or Workshop Item
(Other)
Abstract
River-floodplains are coupled systems in which the conveyance and cycling of sediment over centuries to millennia set the morphological and sedimentological boundary conditions that control fluvial processes over shorter time periods (e.g., years to decades). Although this is well known, understanding how such processes are coupled over short and long timescales remains a significant challenge. Moreover, fluvial geomorphology as a discipline has, arguably, focused more on the study of within-channel processes and dynamics, with less attention given to how river-floodplain interactions and feedbacks control the functioning of the wider river corridor (i.e., channel-belt). Growing concern over the potential impacts of 21st century environmental change (e.g., on river morphology, flood conveyance and floodplain ecosystems) highlights a pressing need to address this knowledge gap.
This study applies a physically-based morphodynamic model to investigate the coupled evolution of channel-floodplain systems. The model solves the shallow water equations for in-channel and overbank flows, together with equations representing fine and coarse sediment transport, channel migration and floodplain development. Simulations are run over time periods sufficient for the floodplain to be reworked (and hence reconstructed) by the model. Simulation results provide new insights into: (i) the relative importance of river gradient, sediment flux and bank erodibility as controls on channel migration rates; (ii) the factors that determine the mechanisms and frequency of channel cutoffs; (iii) the degree to which floodplain dynamics (e.g., floodplain reworking and construction) control both floodplain topography and river pattern; (iv) the relative importance of bedload versus suspended load in determining overall fluvial system behaviour; and (v) the challenges involved in simulating these effects using numerical models.
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Published date: 9 March 2024
Venue - Dates:
EGU General Assembly 2024, , Vienna, Austria, 2024-03-14 - 2024-04-19
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Local EPrints ID: 494545
URI: http://eprints.soton.ac.uk/id/eprint/494545
PURE UUID: 556bdca2-9da8-46ef-aa55-f9a929bad68b
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Date deposited: 10 Oct 2024 16:39
Last modified: 11 Oct 2024 02:09
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Contributors
Author:
Andrew Nicholas
Author:
Rolf Aalto
Author:
Phil Ashworth
Author:
Jim Best
Author:
Muriel Bruckner
Author:
Andrea Gasparotto
Author:
Renato Paes de Almeida
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