IMPACTS OF FUTURE STORMINESS ALONG THE CASTLE NECK BARRIER AND ADJACENT TIDAL INLET SYSTEMS IN THE MERRIMACK EMBAYMENT, MA
In light of these future changes, we have analyzed historical shoreline changes along Castle Neck, one of the five barrier islands in the Merrimack Embayment. Likewise, we are documenting channel switching and bar migrations at the updrift Plum Island Sound Inlet. These data allow us to assess the impact of storms on the formation/removal of sand deposits and shoals along the beach and within Plum Island Sound Inlet. During the past 25 years, growth of a large protuberance and sequestration of sand along the mid-Castle Neck shoreline have resulted in a 600 m retreat of the southern spit-end of the barrier. More than a million cubic meters of the sand eroded from the spit washed into Essex Bay causing channel migrations and shoaling and building large sand shoals. At the same time, increased wave energy is impacting valuable shellfish beds and wetlands.
We are using remote sensing, hydrodynamic modeling, and grain size trends, to predict the formation and migration of shoals within Essex Bay. Collectively, these studies are aiding in the prediction of how sand will be exchanged among barrier island – tidal inlet reservoirs during a future period of climate change. Our research will help answer questions concerning barrier island shoreline management, inlet channel dredging programs, and beach nourishment practices.