Articles | Volume 4, issue 1
https://doi.org/10.5194/esurf-4-273-2016
© 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-4-273-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Geometry of meandering and braided gravel-bed threads from the Bayanbulak Grassland, Tianshan, P. R. China
François Métivier
CORRESPONDING AUTHOR
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS – UMR7154, 1 rue Jussieu, 75238 Paris CEDEX 05, France
Olivier Devauchelle
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS – UMR7154, 1 rue Jussieu, 75238 Paris CEDEX 05, France
Hugo Chauvet
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS – UMR7154, 1 rue Jussieu, 75238 Paris CEDEX 05, France
Eric Lajeunesse
Institut de physique du globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS – UMR7154, 1 rue Jussieu, 75238 Paris CEDEX 05, France
Patrick Meunier
Département de Géologie, CNRS – UMR8538, Ecole Normale Supérieure, 24 rue Lhomond, 75005 Paris, France
Koen Blanckaert
Research center for Eco-environmental sciences, Chinese Academy of sciences, Beijing, P. R. China
Peter Ashmore
Department of Geography, Social Science Centre Rm 2322, Western University, London, Ontario, Canada
Zhi Zhang
The States Key laboratory of Cryospheric Science, Cold and Arid Region Environmental and Engineering and Research Institute, Chinese Academy of Sciences, 260 Donggang west road, Lanzhou, China
Yuting Fan
Xinjiang Institute of Ecology and geography, Chinese Academy of Sciences, Urumqi, P. R. China
Youcun Liu
Key Laboratory of Water Environment and Resource, Tianjin Normal University, 393 Binshui west road, Tianjin 300387, China
Zhibao Dong
The States Key laboratory of Cryospheric Science, Cold and Arid Region Environmental and Engineering and Research Institute, Chinese Academy of Sciences, 260 Donggang west road, Lanzhou, China
Baisheng Ye
The States Key laboratory of Cryospheric Science, Cold and Arid Region Environmental and Engineering and Research Institute, Chinese Academy of Sciences, 260 Donggang west road, Lanzhou, China
deceased
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Cited
20 citations as recorded by crossref.
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- Momentum transfer across an open-channel, turbulent flow P. Popović et al. 10.1017/jfm.2023.1098
- 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
- Reconstructing subsurface sandbody connectivity from temporal evolution of surface networks E. Steel et al. 10.1111/bre.12668
- Morphological Model for Erosion Prediction of India’s Largest Braided River Using MIKE 21C Model K. Pareta 10.3389/esss.2024.10075
- Managing erosion and deposition to stabilize a silt-laden river X. Wu et al. 10.1016/j.scitotenv.2023.163444
- Coupling threshold theory and satellite-derived channel width to estimate the formative discharge of Himalayan foreland rivers K. Gaurav et al. 10.5194/esurf-9-47-2021
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- Predicting stable alluvial channel profiles using emotional artificial neural networks A. Gholami et al. 10.1016/j.asoc.2019.03.003
- 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
- Investigation of a Gravel-Bed River’s Pattern Changes: Insights from Satellite Images D. Termini 10.3390/app11052103
- Estimating Snow Depth Using Multi-Source Data Fusion Based on the D-InSAR Method and 3DVAR Fusion Algorithm Y. Liu et al. 10.3390/rs9111195
- Differential Bank Migration Limits the Lifespan and Width of Braided Channel Threads A. Chadwick et al. 10.1029/2021WR031236
- Evidence of, and a proposed explanation for, bimodal transport states in alluvial rivers K. Dunne & D. Jerolmack 10.5194/esurf-6-583-2018
- Soil bacteria mediate organic carbon stability during alpine wetland biogeomorphic succession in the arid region of Central Asia Y. Hu et al. 10.1007/s11104-023-06405-9
- Laboratory rivers adjust their shape to sediment transport A. Abramian et al. 10.1103/PhysRevE.102.053101
- Laboratory rivers: Lacey's law, threshold theory, and channel stability F. Métivier et al. 10.5194/esurf-5-187-2017
- Threshold constraints on the size, shape and stability of alluvial rivers C. Phillips et al. 10.1038/s43017-022-00282-z
- A single width–discharge regime relationship for individual threads of braided and meandering rivers from the Himalayan Foreland K. Gaurav et al. 10.1016/j.geomorph.2017.07.004
19 citations as recorded by crossref.
- Analyzing bank profile shape of alluvial stable channels using robust optimization and evolutionary ANFIS methods A. Gholami et al. 10.1007/s13201-019-0928-6
- Momentum transfer across an open-channel, turbulent flow P. Popović et al. 10.1017/jfm.2023.1098
- 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
- Reconstructing subsurface sandbody connectivity from temporal evolution of surface networks E. Steel et al. 10.1111/bre.12668
- Morphological Model for Erosion Prediction of India’s Largest Braided River Using MIKE 21C Model K. Pareta 10.3389/esss.2024.10075
- Managing erosion and deposition to stabilize a silt-laden river X. Wu et al. 10.1016/j.scitotenv.2023.163444
- Coupling threshold theory and satellite-derived channel width to estimate the formative discharge of Himalayan foreland rivers K. Gaurav et al. 10.5194/esurf-9-47-2021
- Confluence simulations based on dynamic channel parameters in the grasslands lacking historical measurements M. Li et al. 10.1016/j.jhydrol.2023.130425
- Uncertainty analysis of intelligent model of hybrid genetic algorithm and particle swarm optimization with ANFIS to predict threshold bank profile shape based on digital laser approach sensing A. Gholami et al. 10.1016/j.measurement.2018.02.070
- Predicting stable alluvial channel profiles using emotional artificial neural networks A. Gholami et al. 10.1016/j.asoc.2019.03.003
- 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
- Investigation of a Gravel-Bed River’s Pattern Changes: Insights from Satellite Images D. Termini 10.3390/app11052103
- Estimating Snow Depth Using Multi-Source Data Fusion Based on the D-InSAR Method and 3DVAR Fusion Algorithm Y. Liu et al. 10.3390/rs9111195
- Differential Bank Migration Limits the Lifespan and Width of Braided Channel Threads A. Chadwick et al. 10.1029/2021WR031236
- Evidence of, and a proposed explanation for, bimodal transport states in alluvial rivers K. Dunne & D. Jerolmack 10.5194/esurf-6-583-2018
- Soil bacteria mediate organic carbon stability during alpine wetland biogeomorphic succession in the arid region of Central Asia Y. Hu et al. 10.1007/s11104-023-06405-9
- Laboratory rivers adjust their shape to sediment transport A. Abramian et al. 10.1103/PhysRevE.102.053101
- Laboratory rivers: Lacey's law, threshold theory, and channel stability F. Métivier et al. 10.5194/esurf-5-187-2017
- Threshold constraints on the size, shape and stability of alluvial rivers C. Phillips et al. 10.1038/s43017-022-00282-z
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Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
In meandering rivers, flow and sediments are carried in a single thread whereas in braided rivers they are carried through numerous threads. The geometry of single-thread follows scaling relationships with discharge. The most famous of these, "Lacey's law", states that a river's width scales with the square root of its discharge. We here show that threads from braided rivers also accord with Lacey's law, and that the geometry of meandering and braided threads cannot be differenciated.
In meandering rivers, flow and sediments are carried in a single thread whereas in braided...