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Under Development. 2-way coupling between ocean and atmosphere circulation models – put the O in COAMPS Couple wave models with ocean and atmospheric circulation models Automate flow of data and model results from one model to another – DIOPS for waves
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Under Development • 2-way coupling between ocean and atmosphere circulation models – put the O in COAMPS • Couple wave models with ocean and atmospheric circulation models • Automate flow of data and model results from one model to another – DIOPS for waves • Integrate sediment transport models with coastal circulation models • And I haven’t even talked about ice modeling!
Distributed Integrated Ocean Prediction System Slides courtesy of Dean Wakeham DIOPS/SWAN Scientist Neptune Sciences, Inc.
Vision of DIOPS A distributed, forward deployed ocean wave and nearshore dynamics prediction software system, providing real-time, organic, relocateable wave prediction capability to operating forces. Courtesy of Dean Wakeham
COMPONENTS • WAve Model (WAM) • STeady-state WAVE Model (STWAVE) • Combined REFraction/DIFfraction Model (REF/DIF) • Navy Relocatable Tide/Surge Modeling System (PCTIDES) • Navy SURF 3.1 Courtesy of Dean Wakeham
DIOPS Data Flow Atmosphere Object TEDS via METCAST Offshore Object Nearshore Object Coarse Medium Fine WAM STWAVE Tidal Object SWAN PCTIDES Product Dissemination REFDIF NIPRNET and/or SIPRNET Web Servers TEDS Product Servers Bathymetry Object Surf Object TEDS DBDB-V SURF 3.1 Courtesy of Dean Wakeham
Project 01A-2:Littoral Turbidity and Surface Drift Modeling Richard P. Signell NATO/SACLANT Undersea Research Centre La Spezia, Italy Photo: NRL-SSC Photo: SACLANTCEN
Surface Drift Dynamics ENVIR. FORCING Wind River inflow Surface Heat Flux Wind Tides OCEAN RESPONSE Depth Dependent Currents Wind Waves Vertical Mixing Density Stratification DRIFT RESPONSE Stokes Drift Direct Windage Advected by Near-surface Currents Courtesy of Rich Signell (USGS / SACLANT)
Surface Drift Modeling • Coupled operational models for wind, waves and 3D currents now exist, and we can now build (and assess!) an operational surface drift model. • COAMPS, WAM/SWAN, and NCOM models GNOME (Generalized NOAA Oil Modeling Environment) • NAVO Persian Gulf Drift Forecast Courtesy of Rich Signell (USGS / SACLANT)
Littoral Turbidity Dynamics ENVIR. FORCING River inflow Wind Tides Waves Incident light OCEAN RESPONSE Oscillatory currents Steady barotropic/ baroclinic currents SEDIMENTRESPONSE Sediment entrainment/transport OPTICAL RESPONSE Scattering and absorption (Keen, NRL) Courtesy of Rich Signell (USGS / SACLANT)