The shoreface of Fire Island was extensively modified by Hurricane Sandy and subsequent storms in the following winter months. The changes were evaluated using various morphometrics of the shoreface from four bathymetric surveys, one prior to Hurricane Sandy, and three over the course of twenty months following Sandy. The datasets show that the nearshore bar system moved offshore to deeper water depths following Hurricane Sandy with volume lost from the subaerial beach and surfzone. Following the offshore shift, the nearshore bar system increased in size, the trough deepened, and there has been gradual landward movement of the nearshore bar. The steepening of the upper shoreface, landward translation of the profile, and loss of sediment is ...
The ability of beaches and dunes to recover following an extreme storm is a primary control of barri...
Hurricane Hermine, 2016, impacted the coast of west-central Florida and generated high waves superim...
The response of a barrier island to an extreme storm depends in part on the surge elevation relative...
The shoreface of Fire Island was extensively modified by Hurricane Sandy and subsequent storms in th...
The U.S. Geological Survey (USGS) mounted a substantial effort in response to Hurricane Sandy includ...
Hurricane Sandy at Fire Island, New York presented unique challenges in the quantification of storm ...
Hurricane Sandy had an extensive impact on the beaches along the Atlantic coast. To quantify beach r...
Observed morphodynamic changes over multiple decades were coupled with storm-driven run-up character...
Hurricane Sandy caused record coastal flooding along the south shore of Long Island, NY, and led to ...
© The Author(s), 2015. This is the author's version of the work. It is posted here by permission of ...
This series of studies assesses spatial and temporal changes to the dune/beach system at Fire Island...
Behavior of coastal systems on time scales ranging from single storm events to years and decades is ...
This paper is not subject to U.S. copyright. The definitive version was published in Continental Sh...
KRATZMANN, M.G. and HAPKE, C.J., 2012. Quantifying anthropogenically driven morphologic changes on a...
Ivan, a strong Category 4 hurricane (downgraded to a Category 3 at landfall), caused widespread eros...
The ability of beaches and dunes to recover following an extreme storm is a primary control of barri...
Hurricane Hermine, 2016, impacted the coast of west-central Florida and generated high waves superim...
The response of a barrier island to an extreme storm depends in part on the surge elevation relative...
The shoreface of Fire Island was extensively modified by Hurricane Sandy and subsequent storms in th...
The U.S. Geological Survey (USGS) mounted a substantial effort in response to Hurricane Sandy includ...
Hurricane Sandy at Fire Island, New York presented unique challenges in the quantification of storm ...
Hurricane Sandy had an extensive impact on the beaches along the Atlantic coast. To quantify beach r...
Observed morphodynamic changes over multiple decades were coupled with storm-driven run-up character...
Hurricane Sandy caused record coastal flooding along the south shore of Long Island, NY, and led to ...
© The Author(s), 2015. This is the author's version of the work. It is posted here by permission of ...
This series of studies assesses spatial and temporal changes to the dune/beach system at Fire Island...
Behavior of coastal systems on time scales ranging from single storm events to years and decades is ...
This paper is not subject to U.S. copyright. The definitive version was published in Continental Sh...
KRATZMANN, M.G. and HAPKE, C.J., 2012. Quantifying anthropogenically driven morphologic changes on a...
Ivan, a strong Category 4 hurricane (downgraded to a Category 3 at landfall), caused widespread eros...
The ability of beaches and dunes to recover following an extreme storm is a primary control of barri...
Hurricane Hermine, 2016, impacted the coast of west-central Florida and generated high waves superim...
The response of a barrier island to an extreme storm depends in part on the surge elevation relative...