1. Predicting Characteristic Length Scales of Barrier Island Segmentation in Microtidal Environments.
- Author
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Palermo, R. V., Ashton, A. D., Nepf, H., Kule, M., and Swanson, T.
- Subjects
ARCHIPELAGOES ,SEDIMENT transport ,COASTAL ecology ,FISHERIES ,GEOSPATIAL data ,BARRIER islands - Abstract
Segmented barrier islands can be found in regions with small tidal ranges. In contrast to tidally dominated barriers, where inlet dynamics are thought to control island length scales, the controls on barrier island length scales in wave‐dominated environments have not been quantified. These microtidal barriers typically have a curved shoreline, suggesting the influence of wave‐driven alongshore sediment transport. Microtidal barriers are also typically hydrodynamically isolated from one another, as weak tidal flows limit interactions between adjoining barriers. To better understand the controls on and scales of barrier segmentation in the relative absence of tides, here we develop a theoretical framework to estimate the alongshore length scales at which a barrier will either breach or heal following a disturbance in the barrier morphology. The non‐dimensional framework compares the timescales of overwash (advective) and alongshore sediment transport (diffusive) processes along barrier island chains. We then apply this framework to modern barrier islands in the microtidal Gulf of Mexico using wave hindcast data and the lengths, widths, heights, and lagoon depths measured from remotely sensed geospatial data and topobathymetric data. We find that most of these barriers are currently longer than their critical length scale, often as a result of coastal restoration efforts. Our critical length scale analysis suggests that most of the Gulf of Mexico barriers are vulnerable to segmentation despite coastal restoration efforts intended to protect fisheries and the mainland coasts. Plain Language Summary: Barrier islands provide valuable protection for mainland communities, marine fisheries, and coastal ecology. Restoration efforts are frequently enacted to preserve barrier islands, particularly after storm‐induced breaches segment a barrier into two or more shorter islands. Stable barrier island length scales have been predicted in environments with large tides, where barriers are separated by inlets; however, the characteristic stable length of barriers has not been quantified for environments with small tidal ranges. In these micro‐tidal environments, barriers are primarily shaped by two mechanisms of sediment transport: (a) overwash, which moves sediment from the nearshore environment on top of and behind barriers and (b) wave‐driven alongshore sediment transport, which smooths the shoreline. Here, we present a theoretical framework to evaluate the ability of barrier islands to heal when breached, based on a comparison of timescales for barrier rollover by overwash and shoreline smoothing through alongshore sediment transport. We then apply this analysis to barrier islands in the Gulf of Mexico, finding that many of these barriers are overly long, which suggests that they are vulnerable to segmentation despite (or perhaps due to) coastal restoration. Key Points: We assess the vulnerability of micro‐tidal barriers to segmentation by comparing the timescales of island rollover and alongshore diffusionThe comparison defines a critical length scale over which barriers should be vulnerable to segmenting into smaller islandsMany Gulf of Mexico islands are longer than predicted critical length scales—these long islands tend to be anthropogenically modified [ABSTRACT FROM AUTHOR]
- Published
- 2024
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