Regime shifts in a D3D schematized Scheldt model: recent progress
M.A. de Lucas Pardo (Deltares)
Y. Dijkstra (Deltares)
D.S. Van Maren (TU Delft - Environmental Fluid Mechanics, Deltares)
Julia Vroom (Deltares)
T. van Kessel (Deltares)
J.C. Winterwerp (TU Delft - Environmental Fluid Mechanics, Deltares)
More Info
expand_more
Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.
Abstract
The Ems and Loire evolved into hyper-turbid estuaries in the course of the 20th
century. Winterwerp et al. (2013 a, b) argued that narrowing and deepening of these
rivers induced a regime shift towards these hyper-turbid conditions. This regime
shift was presumed to be driven by a positive feed-back between tidal
amplification, tidal asymmetry and sediment-induced drag reduction. As also the
Sea Scheldt was/is subject to narrowing and deepening, Winterwerp et al. reasoned
that also this river may be at risk to become hyper-turbid.