Item talk:Q239544
From geokb
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"name": "Change in morphology and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York between 2011 and 2014: Analysis of hurricane impact",
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"abstract": "Seafloor mapping investigations conducted on the lower shoreface and inner continental shelf offshore of Fire\r\nIsland, New York in 2011 and 2014, the period encompassing the impacts of Hurricanes Irene and Sandy,\r\nprovide an unprecedented perspective regarding regional inner continental shelf sediment dynamics during\r\nlarge storm events. Analyses of these studies demonstrate that storm-induced erosion and sediment transport\r\noccurred throughout the study area in water depths up to 30 m. Acoustic backscatter patterns were observed to\r\nmove from ~1 m to 450 m with a mean of 20 m and movement tended to decrease with increasing water depth.\r\nThese patterns indicate that both of the primary inner continental shelf sedimentary features in the study area,\r\nlinear sorted bedforms offshore of eastern Fire Island and shoreface-attached sand ridges offshore of central and\r\nwestern Fire island, migrated alongshore to the southwest. The migration of the sorted bedforms represents the\r\nmodification of an active ravinement surface and is thought to have liberated a significant volume of sediment.\r\nComparison of isopach maps of sediment thickness show that the volume of modern sediment composing the\r\nlower shoreface and shoreface-attached sand ridges decreased by ~2.8 \u00d7 106 m3 across the ~73 km2 of\r\ncommon seafloor mapped in both surveys. However, a similar analysis for the relatively calmer 15-yr period\r\nprior to 2011 revealed significant accretion. This allows speculation that the shoreface-attached sand ridges are\r\nmaintained over decadal timescales via sediment supplied through erosion of Pleistocene outwash and lower\r\nHolocene transgressive channel-fill deposits exposed on the inner continental shelf, but that the sand ridges also\r\nperiodically erode and move to the southwest during large storm events. Analyses show that significant storminduced\r\nerosion and sediment transport occurs far seaward of the 5 to 9 m depth of closure assumed for Fire\r\nIsland, where it is thought that an onshore-directed sediment flux from the inner continental shelf to the littoral\r\nsystem is required to balance the coastal sediment budget. It is also thought that the morphology of the\r\nshoreface-attached sand ridges controls the persistent shape of the adjacent shoreline through modification of\r\nincident waves. Thus, we suggest that the sediment dynamics of the inner continental shelf and both storminduced\r\nand anthropogenic modification of the field of shoreface-attached sand ridges be considered in future\r\ncoastal resiliency planning.",
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