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A global synthesis of the effectiveness of sedimentation-enhancing strategies for river deltas and estuaries

Jana R. Cox. et al. - 24/05/2022 - Rivers2Morrow
Global and Planetary Change

Modelling morphodynamic development in the presence of immobile sediment

Chavarrías, V., W. Ottevanger, K. Sloff & E. Mosselman - 10/05/2022
Geomorphology

The Jamuna–Brahmaputra River, Bangladesh

James L. Best, Philip J. Ashworth, Erik Mosselman, Maminul H. Sarker, Julie E. Roden - 09/05/2022
In A. Gupta (Ed.), Large Rivers: Geomorphology and Management (2nd ed., pp. 579-640). Wiley-Blackwell

The Dutch Rhine branches in the Anthropocene – Importance of events and seizing of opportunities

Erik Mosselman - 09/05/2022
Geomorphology, Vol.410

River Dune Dynamics During Low Flow

L. R. Lokin, J. J. Warmink, A. Bomers, S. J. M. H. Hulscher - 19/04/2022 - Rivers2Morrow
Geophysical Research Letters

River Dune Dynamics During Low Flows

L. R. Lokin, J. J. Warmink, A. Bomers, S. J. M. H. Hulscher - 14/04/2022 - Rivers2Morrow

Subsite Publication

River Dune Dynamics During Low Flows

L. R. Lokin, J. J. Warmink, A. Bomers, S. J. M. H. Hulscher - 14/04/2022 - Rivers2Morrow

Subsite Publicatie

Modelling strategies for low flow dune behaviour

13/04/2022 - Rivers2Morrow
A dune development model that may be used for predicting dunes must be able to simulate dune behaviour for both high and low flows well.

Subsite Abstract

Trends in de fluxen van zwevend sediment in het stroomgebied van de Rijn (1997-2014)

13/04/2022 - Rivers2Morrow
In this study, we aim to quantify the temporal and downstream changes in annual loads of suspended sediments in the Rhine river basin during the past decades to identify major sources and sinks of sediment.

Subsite Samenvatting

Massive morphological changes during the 2021 summer flood in the River Meuse

13/04/2022 - Rivers2Morrow
The objective of the study was to improve understanding of the morphological processes during extreme floods, by focusing on the Common Meuse. Here, the riverbed surface is composed of gravel and the longitudinal bed slope is five times steeper than the downstream canalized river.

Subsite Abstract