Articles | Volume 4, issue 1
https://doi.org/10.5194/esurf-4-25-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esurf-4-25-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
18 Jan 2016
Research article |
| 18 Jan 2016
Network response to disturbances in large sand-bed braided rivers
F. Schuurman
CORRESPONDING AUTHOR
Faculty of Geosciences, Department of Physical Geography, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, the Netherlands
Department of Rivers, Deltas and Coasts, Royal HaskoningDHV, Amersfoort, the Netherlands
M. G. Kleinhans
Faculty of Geosciences, Department of Physical Geography, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, the Netherlands
H. Middelkoop
Faculty of Geosciences, Department of Physical Geography, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, the Netherlands
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Cited
23 citations as recorded by crossref.
- Interaction between the braided bar and adjacent channel during flood: a case study of a sand-bed braided river, Brahmaputra–Jamuna . Shampa & M. Ali 10.1007/s40899-018-0269-x
- Morphodynamic processes in a large gravel-bed braided channel in response to runoff change: a case study in the Source Region of Yangtze River H. Lu et al. 10.1007/s12517-022-09641-y
- Chaos in a simple model of a delta network G. Salter et al. 10.1073/pnas.2010416117
- Sedimentary Characteristics and Internal Architecture of a Sandy Braided River: Insights from a Numerical Model Y. Guo et al. 10.3390/w15234119
- Channel Migration of the Meandering River Fan: A Case Study of the Okavango Delta X. Yan et al. 10.3390/w13233319
- Characterizing braided rivers in two nested watersheds in the Source Region of the Yangtze River on the Qinghai-Tibet Plateau Z. Li et al. 10.1016/j.geomorph.2019.106945
- Development of a numerical model for braided river morphology and vegetation evolution with application to the Lower Waitaki River (Aotearoa – New Zealand) G. Stecca et al. 10.1016/j.advwatres.2022.104236
- Effects of Shoal Margin Collapses on the Morphodynamics of a Sandy Estuary W. van Dijk et al. 10.1029/2018JF004763
- Channel bar development, braiding and bankline migration of the Brahmaputra-Jamuna river, Bangladesh through RS and GIS techniques M. Rashid & M. Habib 10.1080/15715124.2022.2118281
- Main Flow Migration in the Middle Yangtze River Influenced by Cascade Reservoirs: Characteristics, Controlling Factors, Trends, and Ecological Impact H. Ge & L. Zhu 10.3390/land12050975
- The mechanism of barrier river reaches in the middle and lower Yangtze River X. You et al. 10.1007/s11442-017-1433-1
- Architectural Model of a Dryland Gravel Braided River, based on 3D UAV Oblique Photogrammetric Data: A Case Study of West Dalongkou River in Eastern Xinjiang, China S. YIN et al. 10.1111/1755-6724.14967
- Let's get connected: A new graph theory‐based approach and toolbox for understanding braided river morphodynamics G. Connor‐Streich et al. 10.1002/wat2.1296
- Conceptual model for the formation of bedforms along subglacial meltwater corridors (SMCs) by variable ice‐water‐bed interactions J. Vérité et al. 10.1002/esp.5725
- Response of braiding channel morphodynamics to peak discharge changes in the Upper Yellow River F. Schuurman et al. 10.1002/esp.4344
- Sedimentary characteristics of sandy braided river deposits and factors controlling their deposition: A case study of the lower Shihezi Formation in the northern ordos basin, China X. Tan et al. 10.1016/j.geoen.2023.211932
- Bar dynamics in a sandy braided river: Insights from sediment numerical simulations K. Zhang et al. 10.1016/j.sedgeo.2019.105557
- The barrier river reach identification and classification in the Middle Yangtze River J. Tang et al. 10.1007/s11707-018-0689-9
- Alluvial connectivity in multi‐channel networks in rivers and estuaries W. Sonke et al. 10.1002/esp.5261
- Geomorphology Processes of Channel Planform Migration on Meandering Rivers Z. LIN et al. 10.1111/1755-6724.13223
- The role of floodplain width and alluvial bar growth as a precursor for the formation of anabranching rivers S. Morón et al. 10.1016/j.geomorph.2016.10.026
- The Fate of Bars in Braided Rivers S. Alpheus & E. Hajek 10.2110/001c.117787
- Large‐scale modelling of highly braided and laterally confined reach of a sand‐bed river K. Han et al. 10.1002/esp.5568
23 citations as recorded by crossref.
- Interaction between the braided bar and adjacent channel during flood: a case study of a sand-bed braided river, Brahmaputra–Jamuna . Shampa & M. Ali 10.1007/s40899-018-0269-x
- Morphodynamic processes in a large gravel-bed braided channel in response to runoff change: a case study in the Source Region of Yangtze River H. Lu et al. 10.1007/s12517-022-09641-y
- Chaos in a simple model of a delta network G. Salter et al. 10.1073/pnas.2010416117
- Sedimentary Characteristics and Internal Architecture of a Sandy Braided River: Insights from a Numerical Model Y. Guo et al. 10.3390/w15234119
- Channel Migration of the Meandering River Fan: A Case Study of the Okavango Delta X. Yan et al. 10.3390/w13233319
- Characterizing braided rivers in two nested watersheds in the Source Region of the Yangtze River on the Qinghai-Tibet Plateau Z. Li et al. 10.1016/j.geomorph.2019.106945
- Development of a numerical model for braided river morphology and vegetation evolution with application to the Lower Waitaki River (Aotearoa – New Zealand) G. Stecca et al. 10.1016/j.advwatres.2022.104236
- Effects of Shoal Margin Collapses on the Morphodynamics of a Sandy Estuary W. van Dijk et al. 10.1029/2018JF004763
- Channel bar development, braiding and bankline migration of the Brahmaputra-Jamuna river, Bangladesh through RS and GIS techniques M. Rashid & M. Habib 10.1080/15715124.2022.2118281
- Main Flow Migration in the Middle Yangtze River Influenced by Cascade Reservoirs: Characteristics, Controlling Factors, Trends, and Ecological Impact H. Ge & L. Zhu 10.3390/land12050975
- The mechanism of barrier river reaches in the middle and lower Yangtze River X. You et al. 10.1007/s11442-017-1433-1
- Architectural Model of a Dryland Gravel Braided River, based on 3D UAV Oblique Photogrammetric Data: A Case Study of West Dalongkou River in Eastern Xinjiang, China S. YIN et al. 10.1111/1755-6724.14967
- Let's get connected: A new graph theory‐based approach and toolbox for understanding braided river morphodynamics G. Connor‐Streich et al. 10.1002/wat2.1296
- Conceptual model for the formation of bedforms along subglacial meltwater corridors (SMCs) by variable ice‐water‐bed interactions J. Vérité et al. 10.1002/esp.5725
- Response of braiding channel morphodynamics to peak discharge changes in the Upper Yellow River F. Schuurman et al. 10.1002/esp.4344
- Sedimentary characteristics of sandy braided river deposits and factors controlling their deposition: A case study of the lower Shihezi Formation in the northern ordos basin, China X. Tan et al. 10.1016/j.geoen.2023.211932
- Bar dynamics in a sandy braided river: Insights from sediment numerical simulations K. Zhang et al. 10.1016/j.sedgeo.2019.105557
- The barrier river reach identification and classification in the Middle Yangtze River J. Tang et al. 10.1007/s11707-018-0689-9
- Alluvial connectivity in multi‐channel networks in rivers and estuaries W. Sonke et al. 10.1002/esp.5261
- Geomorphology Processes of Channel Planform Migration on Meandering Rivers Z. LIN et al. 10.1111/1755-6724.13223
- The role of floodplain width and alluvial bar growth as a precursor for the formation of anabranching rivers S. Morón et al. 10.1016/j.geomorph.2016.10.026
- The Fate of Bars in Braided Rivers S. Alpheus & E. Hajek 10.2110/001c.117787
- Large‐scale modelling of highly braided and laterally confined reach of a sand‐bed river K. Han et al. 10.1002/esp.5568
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Latest update: 21 Nov 2024
Short summary
We studied the propagation of natural and human-induced perturbations in large braided sand-bed rivers using a physics-based 3-D model. The results show that the perturbations not only affect the local morphology but their effects amplify while propagating through the braided network. This occurs by destabilization of bifurcations in combination with reshaping of bars and branches. These results could have a major impact on the assessment of engineering measures in large braided sand-bed rivers.
We studied the propagation of natural and human-induced perturbations in large braided sand-bed...
