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The effect of geometry and bottom friction on local bed forms in a tidal embayment

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TLDR
In this paper, a 2DH idealized local morphodynamic model for a tidal channel was used to demonstrate that estuarine bars with typical length scales on the order of the tidal excursion length can develop as the result of a positive feedback between water motion, sediment transport and the sandy bottom.
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This article is published in Continental Shelf Research.The article was published on 2002-07-01 and is currently open access. It has received 75 citations till now. The article focuses on the topics: Length scale & Suspended load.

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Journal ArticleDOI

Morphodynamics of Tidal Inlet Systems

TL;DR: In this paper, the authors discuss the morphodynamics of different units that characterize a tidal inlet system: the overall system, the ebb-tidal delta, the tidal channels, channel networks, tidal bars and meanders, and finally the intertidal zone of tidal flats and salt marshes.
Journal ArticleDOI

Long‐term morphodynamic evolution of a tidal embayment using a two‐dimensional, process‐based model

TL;DR: In this paper, the authors investigated the long-term evolution of estuarine morphodynamics with special emphasis on the impact of pattern formation using a two-dimensional (2-D), numerical, process-based model.
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The Effect of Tidal Asymmetry and Temporal Settling Lag on Sediment Trapping in Tidal Estuaries

TL;DR: In this article, a 2DV model is developed to investigate the changes in relative roughness (friction) and mixing, resulting in fundamental changes in the char- acteristics of the horizontal (velocity) and vertical tides (sea surface elevation).
Journal ArticleDOI

Numerical modelling of shoal pattern formation in well-mixed elongated estuaries

TL;DR: In this article, the formation of channel and shoal patterns in a schematic estuary was investigated using a 2D depth-averaged numerical model based on a description of elementary flow and sediment transport processes.
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Long-term morphodynamic evolution and energy dissipation in a coastal plain, tidal embayment

TL;DR: In this paper, the authors investigated the interaction between different scales and spatial scales of the morphodynamic system in alluvial, coastal plain estuaries and the evolution of the estuarine morphodynamic evolution.
References
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Journal ArticleDOI

A morphodynamic model to simulate the seasonal closure of tidal inlets

TL;DR: A morphodynamic model capable of simulating the seasonal closure of inlets, which includes both longshore (LST) and cross-shore transport (CST) processes, was developed in this paper.
Book

The Morphodynamics of the Wadden Sea

TL;DR: In this paper, a comprehensive description of the geomorphological development and recent problems of the barrier islands from Texel to Fano is given for the first time, including 40 colour photographs and 393 figures, almost all previously unpublished.
Journal ArticleDOI

Morphodynamic modelling for a tidal inlet in the Wadden Sea

TL;DR: In this paper, a dynamic model for morphological development in a tidal inlet, Het Friesche Zeegat, in the Wadden Sea along the northern coast of the Netherlands, is set up to obtain a better understanding of the behaviour of the morphological system around tidal inlets.
Journal ArticleDOI

A model of morphological behaviour of tidal basins

TL;DR: In this paper, a semi-empirical model is presented to simulate the morphological behaviour of a tidal basin in response to a change in one or more of the extrinsic conditions.
Journal ArticleDOI

Initial formation of channels and shoals in a short tidal embayment

TL;DR: In this paper, it is demonstrated that bedforms in a short tidal embayment can develop due to a positive feedback between tidal currents, sediment transport and bedforms, and the stability of a constantly sloping equilibrium bottom profile is studied for various combinations of the model parameters.
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Q1. What are the contributions mentioned in the paper "The effect of geometry and bottom friction on local bed forms in a tidal embayment" ?

In the case that the width is much smaller than the tidal excursion length and non-linear bottom friction is used, there is good qualitative agreement with results from 3D models reported in literature which were applied to the same parameter regime.