Articles | Volume 6, issue 3
https://doi.org/10.5194/esurf-6-723-2018
https://doi.org/10.5194/esurf-6-723-2018
Research article
 | 
31 Aug 2018
Research article |  | 31 Aug 2018

Late Holocene channel pattern change from laterally stable to meandering – a palaeohydrological reconstruction

Jasper H. J. Candel, Maarten G. Kleinhans, Bart Makaske, Wim Z. Hoek, Cindy Quik, and Jakob Wallinga

Related authors

Faded landscape: unravelling peat initiation and lateral expansion at one of northwest Europe's largest bog remnants
Cindy Quik, Ype van der Velde, Jasper H. J. Candel, Luc Steinbuch, Roy van Beek, and Jakob Wallinga
Biogeosciences, 20, 695–718, https://doi.org/10.5194/bg-20-695-2023,https://doi.org/10.5194/bg-20-695-2023, 2023
Short summary
Soil lacquer peel do-it-yourself: simply capturing beauty
Cathelijne R. Stoof, Jasper H. J. Candel, Laszlo A. G. M. van der Wal, and Gert Peek
SOIL, 5, 159–175, https://doi.org/10.5194/soil-5-159-2019,https://doi.org/10.5194/soil-5-159-2019, 2019
Short summary

Related subject area

Physical: Geomorphology (including all aspects of fluvial, coastal, aeolian, hillslope and glacial geomorphology)
Dimensionless argument: a narrow grain size range near 2 mm plays a special role in river sediment transport and morphodynamics
Gary Parker, Chenge An, Michael P. Lamb, Marcelo H. Garcia, Elizabeth H. Dingle, and Jeremy G. Venditti
Earth Surf. Dynam., 12, 367–380, https://doi.org/10.5194/esurf-12-367-2024,https://doi.org/10.5194/esurf-12-367-2024, 2024
Short summary
Path length and sediment transport estimation from DEMs of difference: a signal processing approach
Lindsay Marie Capito, Enrico Pandrin, Walter Bertoldi, Nicola Surian, and Simone Bizzi
Earth Surf. Dynam., 12, 321–345, https://doi.org/10.5194/esurf-12-321-2024,https://doi.org/10.5194/esurf-12-321-2024, 2024
Short summary
Influence of cohesive clay on wave–current ripple dynamics captured in a 3D phase diagram
Xuxu Wu, Jonathan Malarkey, Roberto Fernández, Jaco H. Baas, Ellen Pollard, and Daniel R. Parsons
Earth Surf. Dynam., 12, 231–247, https://doi.org/10.5194/esurf-12-231-2024,https://doi.org/10.5194/esurf-12-231-2024, 2024
Short summary
Statistical characterization of erosion and sediment transport mechanics in shallow tidal environments – Part 1: Erosion dynamics
Andrea D'Alpaos, Davide Tognin, Laura Tommasini, Luigi D'Alpaos, Andrea Rinaldo, and Luca Carniello
Earth Surf. Dynam., 12, 181–199, https://doi.org/10.5194/esurf-12-181-2024,https://doi.org/10.5194/esurf-12-181-2024, 2024
Short summary
Statistical characterization of erosion and sediment transport mechanics in shallow tidal environments – Part 2: Suspended sediment dynamics
Davide Tognin, Andrea D'Alpaos, Luigi D'Alpaos, Andrea Rinaldo, and Luca Carniello
Earth Surf. Dynam., 12, 201–218, https://doi.org/10.5194/esurf-12-201-2024,https://doi.org/10.5194/esurf-12-201-2024, 2024
Short summary

Cited articles

Agrawal, Y., McCave, I., and Riley, J.: Laser diffraction size analysis, Principles, methods, and application of particle size analysis, Cambridge University Press, New York, 119–128, 1991. 
Allen, J. R. L.: The sedimentation and palaeogeography of the Old Red Sandstone of Anglesey, north Wales, P. Yorks. Geol. Soc., 35, 139–185, 1965. 
Archer, D.: Land of Singing Waters-rivers and great floods of Northumbria, Spredden Press, 1992. 
Baden, W. and Eggelsmann, R.: Der Wasserkreislauf eines nordwestdeutschen Hochmoores, The water balance of a high moor in northwest Germany, Schriftenreihe des Kuratoriums fur Kulturbauwesen, 12, 156 pp., 1964. 
Baird, A. J., Eades, P. A., and Surridge, B. W.: The hydraulic structure of a raised bog and its implications for ecohydrological modelling of bog development, Ecohydrology, 1, 289–298, 2008. 
Download
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.