Observations of barrier island length explained using an exploratory morphodynamic model

Journal article (2013)
Department
Delft Institute of Applied Mathematics (EEMCS) (TU Delft)
Copyright: © 2013 American Geophysical Union
DOI: https://doi.org/doi:10.1002/grl.50843
Stability Equilibrium Barrier coast Tidal flow Morphodynamic modeling Multiple inlet systems
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Published Date

20-08-2013

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Source:

Geophysical ResearchLetters, 40 (16), 2013

ISSN:

0094-8276

Faculty

Electrical Engineering, Mathematics and Computer Science

Department

Delft Institute of Applied Mathematics

Abstract

Barrier coasts display a chain of islands, separated by tidal inlets that connect a back-barrier basin to a sea or ocean. Observations show that barrier island length generally decreases for increasing tidal range and increasing basin area. However, this has neither been reproduced in model studies nor explained from the underlying physics. This is the aim of our study. Here we simulate barrier coast dynamics by combining a widely used empirical relationship for inlet dynamics with a process-based model of the tidal hydrodynamics. Our model results show stable inlet systems with more than one inlet open that support the observed qualitative relationships and fit in existing barrier coast classifications. To explain this, we identify a competition between a destabilizing mechanism (bottom friction in inlets, tending to reduce the number of open inlets) and a stabilizing one (spatially varying pressure gradients over the inlets, tending to keep the inlets open).