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Published byLaura Lawrence Modified over 9 years ago
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Mark Bennett, USGS Study funded Cooperatively with Newport News Waterworks
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Presentation derived primarily from study entitled: “ Simulated Changes in Salinity in the York and Chickahominy Rivers as a Result of Projected Sea- Level Rise in the Chesapeake Bay” Karen C. Rice, Mark R. Bennett, and Jian Shen
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Peninsula Water Supply NN Waterworks - Chickahominy River, five reservoirs, & desalted groundwater (62 mgd) Williamsburg – one reservoir; interconnections JCC & York County: groundwater; interconnections Regional sharing Agreements
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Chickahominy River Primary source of fresh water to the region Limited source during droughts due to low flows and salinity Tidal barrier dam designed/installed in 1940’s
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Warming impacts on surface water quality Warming impacts on surface water quality Drought Intensity and frequency changes Demand Patterns (including population shifts and seasonal peaking changes) Sea Level Rise, Storm Surge, Salinity Gradients
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Sea Level Trends
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Scenarios to Consider
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Normal and drought flow conditions in York and Chickahominy River Low, Median, and High Sea-level Rise Scenarios 1. 20 th Century rate = 3-4 mm/year; 30-40 cm by 2100 2. 2oth Century rate + 2 mm/year acceleration; up to 50 cm by 2100 3. 20th Century rate + 7 mm/year acceleration; up to 100 cm by 2100
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Large Domain Model of the Chesapeake Bay
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Chickahominy Model Results Model development, testing and calibration by VIMS and USGS Adapted Chesapeake Bay model and river models (HEM-3D)
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Salinity Excursions Chickahominy River (@ Walkers Dam)
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Calibration Results Chickahominy Model Results
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Surface salinity at Walkers Dam on the Chickahominy River 3 documented historical events 30 cm rise increases duration slightly, increases concentration significantly Chickahominy Model Results
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Higher sea-level conditions increase number of excursions during lower flow periods ( 7-8 events !) Chickahominy Model Results
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October 2005 flow conditions (“normal dry season/year”) Chickahominy Model Results
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October 2002 flow conditions (Severe Drought) Chickahominy Model Results
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Nested Grid Model of York River Estuary
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York River – Surface Salinity
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York River Model Results York River Model Results October 2005 flow conditions (“normal dry season/year”)
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York River Model Results October 2002 flow conditions (severe drought)
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Sea-Level rise will impact the freshwater-salt water – brackish water gradients in the York River and Chickahominy River. Changes will be most notable during low flows and in areas with a lower volume of flow What are the potential implications for habitat?
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Questions ? http://pubs.usgs.gov/of/2011/1191/ Quality. Reliability. Community.
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