The role of storm-driven seaward sediment flux in coastal barrier dynamics is an enduring puzzle
The role of storm-driven seaward sediment flux in coastal barrier dynamics is an enduring puzzle
Coastal barrier systems are low-lying environments that bear the brunt of storm impacts, with cumulative and complex consequences for barrier evolution. Most studies of barrier responses to storms examine what happens when water and sediment get driven landward across a barrier from its ocean side. Sherwood et al. (2023, https://doi.org/10.1029/2022jf006934) investigate the effects of overland flow and sediment transport forced across a barrier in the opposite direction—from its sheltered side, seaward. Using high-resolution imagery of a barrier island observed before and after a hurricane, Sherwood et al. (2023, https://doi.org/10.1029/2022jf006934) show that “outwash” flow across the barrier shifted several times more sediment by volume than is typically reported for beach and dune erosion from onshore forcing. Their findings are remarkable because they are not exceptional: a related survey of barriers along the Atlantic and Gulf Coasts of the USA observed patterns of outwash morphology essentially everywhere. Insights into outwash morphology open exciting questions regarding the overlooked role of storm-driven seaward sediment transport in barrier dynamics, with important implications for post-storm barrier recovery and barrier evolution over decades to centuries.
coastal barriers, cyclones, outwash, overwash, washout, washover
Lazarus, Eli D.
642a3cdb-0d25-48b1-8ab8-8d1d72daca6e
12 July 2023
Lazarus, Eli D.
642a3cdb-0d25-48b1-8ab8-8d1d72daca6e
Lazarus, Eli D.
(2023)
The role of storm-driven seaward sediment flux in coastal barrier dynamics is an enduring puzzle.
Journal of Geophysical Research: Earth Surface, 128 (7), [e2023JF007168].
(doi:10.1029/2023JF007168).
Abstract
Coastal barrier systems are low-lying environments that bear the brunt of storm impacts, with cumulative and complex consequences for barrier evolution. Most studies of barrier responses to storms examine what happens when water and sediment get driven landward across a barrier from its ocean side. Sherwood et al. (2023, https://doi.org/10.1029/2022jf006934) investigate the effects of overland flow and sediment transport forced across a barrier in the opposite direction—from its sheltered side, seaward. Using high-resolution imagery of a barrier island observed before and after a hurricane, Sherwood et al. (2023, https://doi.org/10.1029/2022jf006934) show that “outwash” flow across the barrier shifted several times more sediment by volume than is typically reported for beach and dune erosion from onshore forcing. Their findings are remarkable because they are not exceptional: a related survey of barriers along the Atlantic and Gulf Coasts of the USA observed patterns of outwash morphology essentially everywhere. Insights into outwash morphology open exciting questions regarding the overlooked role of storm-driven seaward sediment transport in barrier dynamics, with important implications for post-storm barrier recovery and barrier evolution over decades to centuries.
Text
JGR Earth Surface - 2023 - Lazarus - The Role of Storm‐Driven Seaward Sediment Flux in Coastal Barrier Dynamics Is an
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Accepted/In Press date: 30 June 2023
e-pub ahead of print date: 8 July 2023
Published date: 12 July 2023
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Funding Information:
My thanks to Ton Hoitink, Kristen Splinter, and Evan Goldstein for helpful discussions. Constructive comments from Jaap Nienhuis and two anonymous reviewers improved this Commentary. Figure 1 was created and kindly supplied by Christopher Sherwood, Jin‐Si Over, and the co‐authors of Sherwood et al. ( 2023 ). I am also grateful for support from the Leverhulme Trust (RPG‐2018‐282).
Publisher Copyright:
© 2023. The Authors.
Keywords:
coastal barriers, cyclones, outwash, overwash, washout, washover
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Local EPrints ID: 483820
URI: http://eprints.soton.ac.uk/id/eprint/483820
ISSN: 2169-9003
PURE UUID: fddef78d-6297-4e11-ab85-853a560edf88
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Date deposited: 06 Nov 2023 18:15
Last modified: 18 Mar 2024 03:38
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