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Published byAmie Hensley Modified over 8 years ago
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Modeling the Washington Coastal Ocean Focus on estuary-shelf connections Parker MacCready, Dave Sutherland, Neil Banas University of Washington ePOPf September 2010, Portland
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MoSSea: Modeling the Salish Sea faculty.washington.edu/dsuth/MoSSea Realistic hindcasts ROMS v.3 Tides TPXO 7.1 Rivers (16): USGS Wind & Heat Flux: MM5 Ocean OBC: Global NCOM
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Annual Cycle
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Annual-mean Exchange Flow in the Salish Sea
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Nested sub-model of Admiralty Inlet
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Comparison: Monthly CTD Casts
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Comparison: Low-passed velocity
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Comparison: Mooring T & S SHELFHOOD CANAL
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Comparison: Seaglider GH Line
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RISE Ecosystem Modeling: Neil Banas “NPZD” 4-box system N = nitrate P = phytoplankton Z = (micro)zooplakton D = detritus
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RISE Ecosystem model-data comparisons
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Conclusions Exchange flow pulls coastal nitrate into estuaries Exchange flow provides buoyancy to the shelf (=> new pathways) Modeling estuaries requires high resolution Modeling the shelf and open ocean requires boundary conditions (wind & ocean) Both require data, especially ecosystem rates
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LINKS Many papers available at: http://faculty.washington.edu/pmacc/publicatio ns.htm MoSSea: http://faculty.washington.edu/dsuth/MoSSea/in dex.html
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