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Coastal Resource Guide Pleasant Bay and ... - Town to Chatham

Coastal Resource Guide Pleasant Bay and ... - Town to Chatham

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<strong>Coastal</strong> <strong>Resource</strong> <strong>Guide</strong> for <strong>Pleasant</strong> <strong>Bay</strong> <strong>and</strong> <strong>Chatham</strong> Harboraccount for sea level rise. FEMA FIRM maps do not account foranticipated sea level rise, <strong>and</strong> are frequently based on decadesold flood studies. <strong>Pleasant</strong> <strong>Bay</strong> communities will need <strong>to</strong> developadditional <strong>to</strong>ols <strong>to</strong> help them plan for future flooding <strong>and</strong>conduct risk assessments for public <strong>and</strong> private infrastructure <strong>and</strong>natural resources. The continued study <strong>and</strong> moni<strong>to</strong>ring of localtidal regimes within the <strong>Pleasant</strong> <strong>Bay</strong> system is essential for thedevelopment of future flood hazard mapping <strong>and</strong> risk assessment.Other <strong>to</strong>ols, including airborne Light Detection <strong>and</strong> Ranging(LIDAR) used <strong>to</strong> delineate coastal <strong>to</strong>pography (i.e., l<strong>and</strong> elevation)with high precision; accurate bay-wide bathymetry maps <strong>and</strong>sophisticated dynamic computer models will also be necessary forthe development of predictive flood hazard data.While all floodplains will continue <strong>to</strong> be affected by coastalflooding, areas most vulnerable <strong>to</strong> coastal flooding are locatedwithin the FEMA mapped flood zones closest <strong>to</strong> the two inlets.Over time, future flood hazards will be better unders<strong>to</strong>od for allareas of the <strong>Pleasant</strong> <strong>Bay</strong> system, <strong>and</strong> communities can develop<strong>and</strong> implement appropriate hazard management measures.6.2.2 Shoreline Change from Erosion <strong>and</strong> Sea LevelRise<strong>Coastal</strong> erosion is another response <strong>to</strong> increased tidal ranges, risingsea level <strong>and</strong> increased s<strong>to</strong>rm frequency <strong>and</strong> severity. Erosion is aprocess that provides sediments <strong>to</strong> adjacent dunes, beaches <strong>and</strong>marshes within the lit<strong>to</strong>ral system. Erosion is a process that occursin nature. However, the natural rate or pattern of erosion maybe influenced by coastal armoring or other human activity thatinterferes with the natural movement of sediments. The rate ofsea level rise also may expedite the process of erosion.A fuller picture of the effects of SLR in <strong>Pleasant</strong> <strong>Bay</strong> <strong>and</strong> <strong>Chatham</strong>Harbor would require further data collection <strong>and</strong> analysis. In thefuture, this degree of detailed analysis may be warranted <strong>to</strong> guidelocal planning <strong>and</strong> management responses. At this time thereare general strategies for preparing for sea level rise that could beconsidered. These include:• Acquiring coastal property <strong>to</strong> protect access, reduce property<strong>and</strong> infrastructure damage <strong>and</strong> improve the functioning ofcoastal processes;• Relocating vulnerable infrastructure;• Removing unnecessary, dangerous or damaging coastalarmoring;• Developing improved regulations <strong>to</strong> protect coastal systems <strong>and</strong>beaches;• Encouraging l<strong>and</strong>owners <strong>to</strong> obtain conservation easements forunarmored bluffs that provide sediment <strong>to</strong> down drift beaches(Theiler, 2009).Some areas of <strong>Pleasant</strong> <strong>Bay</strong> <strong>and</strong> <strong>Chatham</strong> Harbor, particularlyin the vicinity of the 1987 <strong>and</strong> 2007 inlets, have experiencedsignificant erosion. The areas currently experiencing the mosterosion are located on the east facing <strong>Chatham</strong> shorelineopposite the 2007 inlet, as well as most other unarmored eastfacing properties throughout the <strong>Bay</strong>. The primary managementresponse <strong>to</strong> coastal erosion has been an increase in coastal erosioncontrol structures though out the <strong>Bay</strong> (see Section 5). Many <strong>to</strong>wnl<strong>and</strong>ings have lost significant areas of beach over recent years.Some of <strong>Chatham</strong>’s <strong>to</strong>wn l<strong>and</strong>ings, such as Scatteree <strong>and</strong> StrongIsl<strong>and</strong> Road, have required regular s<strong>and</strong> nourishment as a resul<strong>to</strong>f erosion. Much of Jacknife Beach in <strong>Chatham</strong> has been lost <strong>to</strong>erosion, <strong>and</strong> the parking lot experiences frequent flooding.Sea Level Rise (SLR) will continue <strong>to</strong> be a fac<strong>to</strong>r in shoreline changecaused by flooding <strong>and</strong> s<strong>to</strong>rm surges as well as coastal erosion.The effects of rising sea level can be magnified by human actionssuch as coastal armoring. Recent reports suggest that sea level willrise by approximately one meter by 2100. This degree of change,coupled with increased potential for s<strong>to</strong>rm surge, would beexpected <strong>to</strong> have significant effects such as loss of coastal habitats<strong>and</strong> resources, increased coastal erosion, loss of recreationalresources such as beaches <strong>and</strong> marshes, salt-water intrusion in<strong>to</strong>wells <strong>and</strong> septic systems, elevated s<strong>to</strong>rm surge levels, <strong>and</strong> morefrequent coastal inundation (Theiler, 2009).22<strong>Pleasant</strong> <strong>Bay</strong> Alliance 2011

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