Climate Change and Chesapeake Bay Habitats

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Climate Change and Chesapeake Bay Habitats Donna Marie Bilkovic STAC Chesapeake Bay Forage Base Workshop 12 November 2014 http://www.chesapeake.org/stac/ Virginia Institute of Marine Science www.ccrm.vims.edu donnab@vims.edu

Existing coastal wetlands Chesapeake Bay NON-TIDAL COASTAL WETLANDS State Coastal (ha) % VA 260,627 64 MD 136,558 90 Havens, regional assessment TIDAL FRESHWATER WETLANDS State (ha) Delaware 823 Maryland 10,345 Virginia 16,000 North Carolina 1,200 South Carolina 26,115 Georgia 19,040 After: Mitsch & Gosselink 2000 from Baldwin et al. 2012 Total Bay Coastal Wetlands ~~595,000 ha BRACKISH & SALT MARSH Salt Marsh 27,438 Brackish marsh 123,651 SAV (2012) ~ 19,500 ha

Two principal drivers of bay habitat persistence, human use and climate, are constantly changing Human Use Climate Change

Climate Change can affect coastal wetlands through multiple ways Temperatures can change plant growth and assemblages Storms can physically remove SAV beds and marsh plants Changing weather patterns can affect local salinity Runoff can add to turbidity and nutrient levels Sea level rise can increase water depth & reduce available habitat Shoreline protection can prevent landward migration

Climate Projections for Chesapeake Bay Sea Level Rise Surface Water Temperature Boon 2012 SE VA Average Rate is 4.42 mm/yr & accelerating (~3.4 mm/yr baywide) SE VA is likely to see a 2 3 ft rise by 2050 Both mean and max annual temps have increased by more than 1 C (1.8 F) over the past 5-6 decades Seasonal warming occurring ~3 weeks earlier than in the 1960s Expected increase of 2 6 C by 2100 Sources: Pyke et al. 2008. Climate change and the Chesapeake Bay, CBP STAC Report. Austin 2002, AFS Symposium 32. Boon 2012. Evidence of sea level acceleration at US and Canadian tide stations, Atlantic Coast, North America. JCR 28.6

Tidal wetlands and Sea level rise Geomorphic settings of mid-atlantic tidal wetlands Conversion of tidal wetlands to open water Geomorphic settings have differing hydrodynamics, sediment sources, & vegetative communities Wetland response to sea level rise expected to vary with geomorphic setting CCSP 2009: Cahoon et al. 2009; data source: Reed et al., 2008; map source: Titus et al., 2008

The Problem with Shoreline Hardening Habitat loss & fragmentation forest, wetlands (Peterson and Lowe 2009; Dugan et al 2011) Sediment supply & transport altered, increased scouring, turbidity (Bozek and Burdick 2005, NRC 2007) Increase in invasive spp (Chambers et al 1999) Decrease fish & benthos, marsh bird diversity, terrapin presence (Peterson et al 2000, Chapman 2003, King et al 2005, Bilkovic et al 2006, Seitz et al 2006, Bilkovic & Roggero 2008, Morley et al 2012, Isdell et al in press) Prevents natural migration of habitats with SLR Evidence of Low Thresholds (e.g. >5% riprap no increase in SAV (Patrick et al 2014) Map source: D. Bilkovic Chesapeake Bay 18% of tidal shoreline hardened VA: 11% MD: 28% 32% riparian land developed ~5 km 2 of artificial substrate introduced (intertidal impacted)

Coastal Development: Status and Future Trends Current shoreline hardening Bulkhead/Riprap Future shore protection Map source: D.M. Bilkovic Only ~7% of coastal lands set aside for conservation Almost 45% of the land expected to be developed Map source: Titus et al. 2009

Tidal Marshes SLR & barriers to migration Tidal marshes in the meso-polyhaline reaches at highest risk due to land development & SLR Nearly 40% of Virginia marshes are vulnerable to SLR due to adjacent development Bilkovic et al. 2009 Vulnerability of shallow tidal water habitats in Virginia to climate change. http://ccrm.vims.edu/research/climate_change/index.html

Continuum of shoreline protection approaches Estuarine & coastal shorelines Minimally-Moderately altered Highly altered Created marsh Eastern Shore: The Virginia Coast Reserve Oyster-sill Bulkhead Tabbs Creek, VA Marsh-sill Riprap Revetment Breakwater-beach 3-6% 13-18%

Nekton assemblages & productivity in living shorelines depend on availability of suitable habitat Nekton assemblages less diverse at armored shorelines than natural marshes & nekton utilization increases when armored shorelines are converted to living shorelines (diversity & density) Assumed energy transfer to higher trophic levels not yet verified o The role that living shorelines may play as fish and shellfish nursery habitat has not yet been measured. We need to demonstrate enhanced growth and protection from predation compared to other habitats Persistent aquatic environment seaward from marsh edge may be essential o Sediment accretion landward of living shoreline structures may limit suitable habitat over time Davis et al 2008; Hardaway et al 2007, Seitz et al. 2006, Bilkovic & Roggero 2008, Bilkovic & Mitchell 2013

Ribbed Mussels and Marshes Mussel Distribution Ecosystem Engineers Filter water Accrete sediment, Stabilize shore Promote marsh plant growth Enhance nutrient dynamics Important Prey item York River ~200 Million Mussels Oysters Living shorelineslower mussel density salinity preferences (~8-30)

Submerged Aquatic Vegetation ~ 20 SAV species are commonly found throughout Chesapeake Bay SAV communities can be grouped by salinity tolerances Zostera marina eelgrass (Polyhaline) Ruppia maritima widgeongrass (Meso)

Map source: Ken Moore Stresses related to climate change that affect eelgrass survival include: Increased frequency and duration of high summer water temps, > 30 C (86 F) -Massive baywide decline observed during 2005 from >30 C Increased rainfall = runoff of sediments and nutrients = light availability Light requirements of eelgrass increase with increasing temps Increased storm intensity and frequency Increased water level/shl hardening = declines in habitat area BUT, CO2 with warmer waters may increase high temp tolerance leading to enriched growth, shoot survival and propagation (Tom Arnold, Dickerson; Richard Zimmerman, ODU)

Recommendations and Research Needs More detailed data on sediment processes & Shallow water bathymetry Bilkovic Landscape-level influences on bay habitat resilience - Better understanding of the extent that landscape setting moderates habitat connectivity, functionality, and species distribution Fragmentation patterns of marshes Dispersed wetlands (yellow) tend to occur in areas of developed land use Align implementation & monitoring of habitat restoration activities with living resource objectives. Thank You! donnab@vims.edu