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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3 Modeling and Analysis Subsystem {SWG3.3 Chair, Chris Mooers/RSMAS-UM} In the next five years, produce operationally, real-time model-based analyses and forecasts (with generalized error bars and by downscaling from National Backbone basin-scale or global models) of fields of basic physical variables for the SECOORA domain as needed for a variety of societal applications, including R&D. In the next five years, produce operationally, real-time model-based analyses and forecasts (with generalized error bars and by downscaling from National Backbone basin-scale or global models) of fields of basic physical variables for the SECOORA domain as needed for a variety of societal applications, including R&D.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.1 Product Identification A few quasi-operational, real-time, 3D nowcast/forecast systems (w/o data assimilation) for coastal ocean circulation presently exist in the SECOORA domain that estimate sea surface height, temperature, salinity, and current fields, plus Lagrangian particle trajectories.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.1 {CONTINUED} These models have a horizontal resolution of a few km, a vertical resolution of ca. 4% of the depth, and a time resolution of a few minutes. They are driven by tidal models, numerical weather predictions, realistic bottom topogrpahy, and operational basin-scale or global models for open boundary conditons. They are designed to predict oceanic fronts, eddies, meandering jets, coastal upwelling/downwelling events, mixing events, etc. These models have a horizontal resolution of a few km, a vertical resolution of ca. 4% of the depth, and a time resolution of a few minutes. They are driven by tidal models, numerical weather predictions, realistic bottom topogrpahy, and operational basin-scale or global models for open boundary conditons. They are designed to predict oceanic fronts, eddies, meandering jets, coastal upwelling/downwelling events, mixing events, etc.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.1. {CONTINUED} There are also a few 2D numerical models that are used intermittently (viz., during severe storm passsges) to estimate sea surface heights (water levels), depth- averaged currents, tides, waves, and coastal inundation.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.2 Gap Analysis In the next five years, there is a need to conduct additional model-observation comparisons to extend the data base of generalized error bars for a large suite of metrics. There is a need to introduce data assimilation capabilities to the modeling efforts. In the next five years, there is a need to conduct additional model-observation comparisons to extend the data base of generalized error bars for a large suite of metrics. There is a need to introduce data assimilation capabilities to the modeling efforts.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.2 {CONTINUED} “Forecasters” need to be identified: NWS/WFOs, Ocean Prediction Center/NCEP/NWS, USCG SAROPS, et al. The “value-added industry” needs to be fostered. CONOPS is missing. “Forecasters” need to be identified: NWS/WFOs, Ocean Prediction Center/NCEP/NWS, USCG SAROPS, et al. The “value-added industry” needs to be fostered. CONOPS is missing.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.2 {CONTINUED} Observing System Experiments (OSEs) and Observing System Simulation Experiments (OSSEs) should be conducted to aid observing subsystem designs. Sub-regional (including estuarine and coastal lagoon) nowcast/forecast systems should be nested in domain-wide models. Ecosystem and sediment transport models should be introduced operationally. Observing System Experiments (OSEs) and Observing System Simulation Experiments (OSSEs) should be conducted to aid observing subsystem designs. Sub-regional (including estuarine and coastal lagoon) nowcast/forecast systems should be nested in domain-wide models. Ecosystem and sediment transport models should be introduced operationally.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.3 Operational Continuity Redundant, distributed telecommunication and computational facilities are needed to ensure a storm-hardened, robust system. The observing system needs to provide adequate observations for data assimilation and validation/verification. A CONOPS is needed to link RCOOS and National Backbone operations. Redundant, distributed telecommunication and computational facilities are needed to ensure a storm-hardened, robust system. The observing system needs to provide adequate observations for data assimilation and validation/verification. A CONOPS is needed to link RCOOS and National Backbone operations.
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The SouthEast Coastal Ocean Observing SECOORA Meeting Regional Association (SECOORA) June 11-12, 2007 3.3.4 User Satisfaction Regular reviews of product adequacy need to be conducted with various user groups on a regional basis. There will also be a need to communicate with users on a national scale, including coordination with the National Backbone and the value-added industry. “Users” should range from researchers to forecasters, from super users to end users. Regular reviews of product adequacy need to be conducted with various user groups on a regional basis. There will also be a need to communicate with users on a national scale, including coordination with the National Backbone and the value-added industry. “Users” should range from researchers to forecasters, from super users to end users.
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