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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.

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Presentation on theme: "Under Development 2-way coupling between ocean and atmosphere circulation models – put the O in COAMPS Couple wave models with ocean and atmospheric circulation."— Presentation transcript:

1 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!

2 Distributed Integrated Ocean Prediction System Slides courtesy of Dean Wakeham DIOPS/SWAN Scientist Neptune Sciences, Inc.

3 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

4 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

5 Surf Object SURF 3.1 Nearshore Object REFDIF STWAVE SWAN Tidal Object PCTIDES Offshore Object Coarse Medium Fine WAM Atmosphere Object TEDS via METCAST DIOPS Data Flow Bathymetry Object TEDS DBDB-V Product Dissemination NIPRNET and/or SIPRNET Web Servers TEDS Product Servers Courtesy of Dean Wakeham

6 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

7 Surface Drift Dynamics Tides WindRiver inflow Wind Waves Stokes Drift ENVIR. FORCING OCEAN RESPONSE DRIFT RESPONSE Direct Windage Surface Heat Flux Wind Advected by Near-surface Currents Density Stratification Depth Dependent Currents Vertical Mixing Courtesy of Rich Signell (USGS / SACLANT)

8 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)

9 Littoral Turbidity Dynamics TidesWind Waves Steady barotropic/ baroclinic currents River inflow Oscillatory currents Sediment entrainment/transport Incident light Scattering and absorption ENVIR. FORCING OCEAN RESPONSE SEDIMENT RESPONSE OPTICAL RESPONSE (Keen, NRL) Courtesy of Rich Signell (USGS / SACLANT)


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