Titlebook: Barrier Dynamics and Response to Changing Climate; Laura J. Moore,A. Brad Murray Book 2018 Springer International Publishing AG 2018 Barri

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Drowned Barriers as Archives of Coastal-Response to Sea-Level Risereadily be deconstructed as they are not in operation simultaneously, nor present along all coasts. However, it is possible to recognize local conditions that make barriers vulnerable to overstepping. It is shown that barrier retreat through overstepping is enhanced by one or more of the following;

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Barrier Island and Estuary Co-evolution in Response to Holocene Climate and Sea-Level Change: Pamlicrodynamic models aid in understanding the magnitude of changes, and the impact on barrier morphology. Future changes to coastal systems may be anticipated based upon changes that have occurred in the past.

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Abrupt Increase in Washover Deposition Along a Transgressive Barrier Island During the Late Nineteene island was seaward of its present location and an open-water lagoon separated it from the mainland. Barrier-island transgression progressed mainly through overwash processes and saltmarsh replaced the lagoon by AD 1500. During the nineteenth century, the number and landward extent of washover depo

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Follets Island: A Case of Unprecedented Change and Transition from Rollover to Subaqueous Shoalsentennial timescales. Stratigraphic architecture reveals two prominent transgressive surfaces. A lower flooding surface separates red fluvial-deltaic clay from overlying bay mud and an upper erosional surface separates back-barrier deposits from overlying shoreface and foreshore deposits..Radiocarbo

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Geometric Constraints on Long-Term Barrier Migration: From Simple to Surprising which active sediment transport occurs). In the next simplest case, substrates composed partly of fine sediment (which is lost to the nearshore system when the substrate is eroded) cause a reduction of the slope of the migration trajectory, because more landward migration is required for each incre

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Shoreface Controls on Barrier Evolution and Shoreline Changetal change. Such shoreface evolution has implications for barrier evolution (and vice versa). In this chapter, we review (1) relations between shoreface and barrier form, (2) limits to knowledge on shoreface behavior and insights from depositional records from which systematic changes over time can

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Morphodynamics of Barrier Response to Sea-Level Rise. Even small perturbations to a barrier system traversing the shelf in dynamic equilibrium can kick-start an oscillating retreat. Looking alongshore, shoreline interconnectivity can have a significant effect on shoreline behavior across both space and time. Overall, our morphodynamic modeling result

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