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Coastal Impacts, Adaptation, and Vulnerabilities - Climate ...

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126 <strong>Coastal</strong> <strong>Impacts</strong>, <strong>Adaptation</strong>, <strong>and</strong> <strong>Vulnerabilities</strong>another 2.7 million acres between 1950 <strong>and</strong> 1980. With development, the Bay has losthalf of the forested shorelines, over half of the wetl<strong>and</strong>s, about 80 percent of underwatergrasses, <strong>and</strong> more than 98 percent of the oysters. The result has been a general decline inthe health of the Bay.Several states in the watershed have made a voluntary pledge to “Save the Bay” bycreating a blueprint for restoring the Bay’s health. On May 12, 2009, President Obamasigned the Chesapeake Bay Protection <strong>and</strong> Restoration Executive Order (Executive Order13508) to “protect <strong>and</strong> restore the health, heritage, natural resources, <strong>and</strong> social <strong>and</strong>economic value of the Nation’s largest estuarine ecosystem <strong>and</strong> the natural sustainabilityof its watershed.” The restoration of the water quality <strong>and</strong> aquatic ecosystems inthe Bay has proven to be difficult <strong>and</strong> will only become more complex with the addedimpacts of climate change.The selection of the Bay as a case study in this chapter of the NCA was based on severalfactors. Managing the Bay requires coordination among several states, making it atruly regional effort spanning a large geographic area. The Bay is a nationally importantresource that is in critical condition; a significant regulatory commitment has been madeto this area <strong>and</strong> substantial monitoring efforts are underway to support its restoration.Although future climate conditions are likely to be warmer, the magnitude <strong>and</strong> rateof warming over the 21st century is uncertain. The location of the Bay is also interestingfrom a precipitation st<strong>and</strong>point, with considerable uncertainty surrounding futureconditions; in other words, the area could be wetter or drier. Given the enormity of theBay <strong>and</strong> the issues it faces, this case study focuses more narrowly on the climate changeimpacts <strong>and</strong> adaptation measures relevant to managing water quality <strong>and</strong> aquatic ecosystemsin Maryl<strong>and</strong>, Pennsylvania, <strong>and</strong> Virginia.The following sections provide an overview of the climate impacts anticipated to occurin the Bay (Section 2), a snapshot of a set of plausible climate futures (Section 3), <strong>and</strong>,finally, an overview of state-level adaptation planning across the Bay (Section 4).2: <strong>Climate</strong> Change <strong>Impacts</strong> on Water Quality <strong>and</strong> EquaticEcosystems for the Chesapeake Bay2.1 Changes in Physical <strong>Climate</strong>A high level overview of the projected changes in the Bay’s physical climate is shownin Table A-1. These changes, along with related changes in streamflow, are discussed inmore detail below.Temperature changes are relative to the 1971-2000 average, with results shown forboth the lower B2 <strong>and</strong> higher A2 emission scenarios, averaged from seven climate models(Najjar et al., 2009). Ranges represent the multi-model mean ±1 st<strong>and</strong>ard deviation.For the earlier periods of 2010 to 2039 <strong>and</strong> 2040 to 2069, only the A2 are shown, becausethe differences between the multi-model averages for the two scenarios are lessthan 0.2°C. These scenarios were examined by Najjar et al. (2009) because they bracketthe range of emissions from the IPCC Third Assessment Report (Nakićenović & Swart,2000). Sea-level changes are relative to 1990. End-of-century projections are from Najjaret al. (2010), which is based on the statistical model presented in Rahmstorf (2007). The

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