Process signatures in regional patterns of shoreline change on annual to decadal time scales
Process signatures in regional patterns of shoreline change on annual to decadal time scales
Gradients in wave-driven alongshore sediment transport influence the morphologies of sediment-covered coastlines on a range of spatial and temporal scales, affecting accretion and erosion patterns relevant to human development. Recent theoretical findings predict that a correlation between shoreline change and shoreline curvature results from patterns of alongshore sediment flux; the sign (positive or negative) of that correlation depends on whether high- or low-angle waves dominated the wave climate. Using lidar surveys of the northern North Carolina coast from 1996–2005 to document shoreline change and quantify alongshore patterns of erosion and deposition, we isolate these signals diagnostic of alongshore-transport processes. Our analyses show a persistent, significant negative correlation between shoreline-position change and shoreline curvature consistent with a low-angle-dominated incident wave climate over the last decade. At large spatial scales, convex-seaward promontories have eroded landward, while concave-seaward bays have aggraded seaward, resulting in an apparent diffusion of alongshore morphological features
L19402
Lazarus, Eli
642a3cdb-0d25-48b1-8ab8-8d1d72daca6e
Murray, A. Brad
dd93e4dd-ed6c-4cf5-89c6-e1f85cf8f61f
October 2007
Lazarus, Eli
642a3cdb-0d25-48b1-8ab8-8d1d72daca6e
Murray, A. Brad
dd93e4dd-ed6c-4cf5-89c6-e1f85cf8f61f
Lazarus, Eli and Murray, A. Brad
(2007)
Process signatures in regional patterns of shoreline change on annual to decadal time scales.
Geophysical Research Letters, 34 (19), .
(doi:10.1029/2007GL031047).
Abstract
Gradients in wave-driven alongshore sediment transport influence the morphologies of sediment-covered coastlines on a range of spatial and temporal scales, affecting accretion and erosion patterns relevant to human development. Recent theoretical findings predict that a correlation between shoreline change and shoreline curvature results from patterns of alongshore sediment flux; the sign (positive or negative) of that correlation depends on whether high- or low-angle waves dominated the wave climate. Using lidar surveys of the northern North Carolina coast from 1996–2005 to document shoreline change and quantify alongshore patterns of erosion and deposition, we isolate these signals diagnostic of alongshore-transport processes. Our analyses show a persistent, significant negative correlation between shoreline-position change and shoreline curvature consistent with a low-angle-dominated incident wave climate over the last decade. At large spatial scales, convex-seaward promontories have eroded landward, while concave-seaward bays have aggraded seaward, resulting in an apparent diffusion of alongshore morphological features
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Published date: October 2007
Organisations:
Earth Surface Dynamics
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Local EPrints ID: 400725
URI: http://eprints.soton.ac.uk/id/eprint/400725
ISSN: 0094-8276
PURE UUID: 8da2dfff-a40b-4d1b-91d3-a44d34fa0de9
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Date deposited: 23 Sep 2016 14:23
Last modified: 15 Mar 2024 03:57
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Author:
A. Brad Murray
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