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Observations of barrier island length explained using an exploratory morphodynamic model
Author(s) -
Roos Pieter C.,
Schuttelaars Henk M.,
Brouwer Ronald L.
Publication year - 2013
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/grl.50843
Subject(s) - inlet , barrier island , geology , oceanography , tidal range , structural basin , range (aeronautics) , geomorphology , estuary , engineering , shore , aerospace engineering
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).