Articles | Volume 6, issue 3
https://doi.org/10.5194/esurf-6-723-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-6-723-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
31 Aug 2018
Research article |
| 31 Aug 2018
| 31 Aug 2018
Late Holocene channel pattern change from laterally stable to meandering – a palaeohydrological reconstruction
Soil Geography and Landscape Group, Wageningen University &
Research, Wageningen, P.O. Box 47, 6700AA, the Netherlands
Maarten G. Kleinhans
Department of Physical Geography, Utrecht University, Utrecht, P.O. Box 80125, 3508TC, the Netherlands
Bart Makaske
Soil Geography and Landscape Group, Wageningen University &
Research, Wageningen, P.O. Box 47, 6700AA, the Netherlands
Wim Z. Hoek
Department of Physical Geography, Utrecht University, Utrecht, P.O. Box 80125, 3508TC, the Netherlands
Cindy Quik
Soil Geography and Landscape Group, Wageningen University &
Research, Wageningen, P.O. Box 47, 6700AA, the Netherlands
Jakob Wallinga
Soil Geography and Landscape Group, Wageningen University &
Research, Wageningen, P.O. Box 47, 6700AA, the Netherlands
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Total article views: 3,094 (including HTML, PDF, and XML)
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Cited
15 citations as recorded by crossref.
- Self‐constraining of low‐energy rivers explains low channel mobility and tortuous planforms J. Candel et al. 10.1002/dep2.112
- Anthropogenic drivers for exceptionally large meander formation during the Late Holocene C. Quik et al. 10.1016/j.ancene.2020.100263
- Readjustments of a sinuous river during the last 6000 years in northwestern Europe (Cher River, France): from an active meandering river to a stable river course under human forcing A. Vayssière et al. 10.1016/j.geomorph.2020.107395
- Sensitivity of a meandering lowland river to intensive landscape management: Lateral migration rates before and after watershed-scale agricultural development B. Rhoads et al. 10.1016/j.ancene.2024.100429
- Predicting river channel pattern based on stream power, bed material and bank strength J. Candel et al. 10.1177/0309133320948831
- Sediment preservation and accretion rates of fluvial meander-belt deposits: variations with temporal scale and river size N. Yan et al. 10.1144/SP540-2022-142
- Late‐Holocene counterpoint deposition in the Lower Rhine River L. Boterman et al. 10.1111/sed.13180
- Conditions to Preserve the Sedimentary Record of Channel Planforms in Temperate Rivers of the Northern Hemisphere M. Słowik et al. 10.1029/2021JF006188
- Changes in floodplain geo-ecology in the Belgian loess belt during the first millennium AD N. Broothaerts et al. 10.1017/njg.2021.9
- Geomorphic responses of fluvial systems to climate change: A habitat perspective K. Juracek & F. Fitzpatrick 10.1002/rra.3938
- Planform architecture, meander evolution and grain‐size variability of a deltaic channel belt in the Rhine‐Meuse delta, The Netherlands T. Winkels et al. 10.1111/sed.13022
- The evolution of meandering and anabranching rivers in postglacial and loess landscapes of Europe M. Słowik 10.1177/09596836221131712
- The fluvial architecture of buried floodplain sediments of the Weiße Elster River (Germany) revealed by a novel method combination of drill cores with two‐dimensional and spatially resolved geophysical measurements H. von Suchodoletz et al. 10.1002/esp.5296
- Was the termination of the Jizera River meandering during the Late Holocene caused by anthropogenic or climatic forcing? J. Elznicová et al. 10.1002/esp.5509
- Reconstructing lateral migration rates in meandering systems – a novel Bayesian approach combining optically stimulated luminescence (OSL) dating and historical maps C. Quik & J. Wallinga 10.5194/esurf-6-705-2018
13 citations as recorded by crossref.
- Self‐constraining of low‐energy rivers explains low channel mobility and tortuous planforms J. Candel et al. 10.1002/dep2.112
- Anthropogenic drivers for exceptionally large meander formation during the Late Holocene C. Quik et al. 10.1016/j.ancene.2020.100263
- Readjustments of a sinuous river during the last 6000 years in northwestern Europe (Cher River, France): from an active meandering river to a stable river course under human forcing A. Vayssière et al. 10.1016/j.geomorph.2020.107395
- Sensitivity of a meandering lowland river to intensive landscape management: Lateral migration rates before and after watershed-scale agricultural development B. Rhoads et al. 10.1016/j.ancene.2024.100429
- Predicting river channel pattern based on stream power, bed material and bank strength J. Candel et al. 10.1177/0309133320948831
- Sediment preservation and accretion rates of fluvial meander-belt deposits: variations with temporal scale and river size N. Yan et al. 10.1144/SP540-2022-142
- Late‐Holocene counterpoint deposition in the Lower Rhine River L. Boterman et al. 10.1111/sed.13180
- Conditions to Preserve the Sedimentary Record of Channel Planforms in Temperate Rivers of the Northern Hemisphere M. Słowik et al. 10.1029/2021JF006188
- Changes in floodplain geo-ecology in the Belgian loess belt during the first millennium AD N. Broothaerts et al. 10.1017/njg.2021.9
- Geomorphic responses of fluvial systems to climate change: A habitat perspective K. Juracek & F. Fitzpatrick 10.1002/rra.3938
- Planform architecture, meander evolution and grain‐size variability of a deltaic channel belt in the Rhine‐Meuse delta, The Netherlands T. Winkels et al. 10.1111/sed.13022
- The evolution of meandering and anabranching rivers in postglacial and loess landscapes of Europe M. Słowik 10.1177/09596836221131712
- The fluvial architecture of buried floodplain sediments of the Weiße Elster River (Germany) revealed by a novel method combination of drill cores with two‐dimensional and spatially resolved geophysical measurements H. von Suchodoletz et al. 10.1002/esp.5296
2 citations as recorded by crossref.
- Was the termination of the Jizera River meandering during the Late Holocene caused by anthropogenic or climatic forcing? J. Elznicová et al. 10.1002/esp.5509
- Reconstructing lateral migration rates in meandering systems – a novel Bayesian approach combining optically stimulated luminescence (OSL) dating and historical maps C. Quik & J. Wallinga 10.5194/esurf-6-705-2018
Discussed (final revised paper)
Latest update: 17 Apr 2024
Short summary
In this study we show how the Overijsselse Vecht river changed from a laterally stable to a meandering river ca. 500 years ago. We developed a methodology to reconstruct the historical discharge and found that the change in river style was caused by an increase in peak discharges. This increase was likely caused by the Little Ice Age and land use changes in the catchment (peat reclamation and exploitation). This study shows how river style changes as a result of discharge regime changes.
In this study we show how the Overijsselse Vecht river changed from a laterally stable to a...
