Breach Evolution - Coastal System Change at Fire Island, New York
In 2012, during Hurricane Sandy, a breach formed in the Otis Pike High Dune Wilderness Area on Fire Island, NY.
Breach Evolution at Fire Island
Breaches in barrier islands play an important role in long-term island resilience by transferring sediment to the bay side of islands, which is one of the ways that barriers keep up with sea level rise. Breaches are also important for bay and barrier island ecosystem function, wherein tide and storm-driven flows flush bay water, increase salinity, dilute contaminants, and provide otherwise unavailable migration pathways for fish and other biota. In 2012, during Hurricane Sandy, a breach formed in the Otis Pike Fire Island High Dune Wilderness Area on Fire Island, NY. The breach changes are being monitored with collaborators at USACE, NPS, and SUNY-Stonybrook using a variety of observational techniques including single-beam bathymetry, aerial lidar, GPS elevations, and aerial imagery.
From the time of its formation through the winter of 2015, the dominant change to the breach geomorphology was the recurring formation of a spit on the western side of the breach. The material forming the spit was eroded from the western ocean side of the barrier beach and transported northward along the western shoreline into the bay. Once formed, the spit restricted tidal flow exchange through the western flood shoal and correlated to a northeast-southwest orientation of the main breach channel.
USGS breach morphology observations have been used to develop a hydrodynamic and geomorphic numerical model, with collaborators at Deltares, which produces accurate hindcasts of the water levels in Great South Bay and breach evolution. The model results are being used to evaluate the relative importance of various hydrodynamic forcings responsible for breach growth and stability.
Below are other science projects associated with this project.
Coastal System Change at Fire Island, New York
Back-barrier and Estuarine - Coastal System Change at Fire Island, New York
Oceanside Beaches and Dunes - Coastal System Change at Fire Island, New York
Open Ocean/Marine - Coastal System Change at Fire Island, New York
Nearshore - Coastal System Change at Fire Island, New York
Below are publications associated with this project.
Morphologic evolution of the wilderness area breach at Fire Island, New York—2012–15
Coastal bathymetry data collected in May 2015 from Fire Island, New York—Wilderness breach and shoreface
Bathymetry data collected in October 2014 from Fire Island, New York—The wilderness breach, shoreface, and bay
Coastal bathymetry data collected in June 2014 from Fire Island, New York—The wilderness breach and shoreface
The effects of geomorphic changes during Hurricane Sandy on water levels in Great South Bay
Bathymetry of the Wilderness breach at Fire Island, New York, June 2013
In 2012, during Hurricane Sandy, a breach formed in the Otis Pike High Dune Wilderness Area on Fire Island, NY.
Breach Evolution at Fire Island
Breaches in barrier islands play an important role in long-term island resilience by transferring sediment to the bay side of islands, which is one of the ways that barriers keep up with sea level rise. Breaches are also important for bay and barrier island ecosystem function, wherein tide and storm-driven flows flush bay water, increase salinity, dilute contaminants, and provide otherwise unavailable migration pathways for fish and other biota. In 2012, during Hurricane Sandy, a breach formed in the Otis Pike Fire Island High Dune Wilderness Area on Fire Island, NY. The breach changes are being monitored with collaborators at USACE, NPS, and SUNY-Stonybrook using a variety of observational techniques including single-beam bathymetry, aerial lidar, GPS elevations, and aerial imagery.
From the time of its formation through the winter of 2015, the dominant change to the breach geomorphology was the recurring formation of a spit on the western side of the breach. The material forming the spit was eroded from the western ocean side of the barrier beach and transported northward along the western shoreline into the bay. Once formed, the spit restricted tidal flow exchange through the western flood shoal and correlated to a northeast-southwest orientation of the main breach channel.
USGS breach morphology observations have been used to develop a hydrodynamic and geomorphic numerical model, with collaborators at Deltares, which produces accurate hindcasts of the water levels in Great South Bay and breach evolution. The model results are being used to evaluate the relative importance of various hydrodynamic forcings responsible for breach growth and stability.
Below are other science projects associated with this project.
Coastal System Change at Fire Island, New York
Back-barrier and Estuarine - Coastal System Change at Fire Island, New York
Oceanside Beaches and Dunes - Coastal System Change at Fire Island, New York
Open Ocean/Marine - Coastal System Change at Fire Island, New York
Nearshore - Coastal System Change at Fire Island, New York
Below are publications associated with this project.