Global Ocean Prediction Using HYCOM

• Main Authors: Metzger, E. J., Hurlburt, Harley E., Wallcraft, Alan J., Cummings, James A., Chassignet, Eric P., Smedstad, Ole M.
• Other Authors: NAVAL RESEARCH LAB STENNIS SPACE CENTER MS OCEANOGRAPHY DIV
• Format: Text
• Language: English
• Published: 2006
• Subjects: Meteorology; Physical and Dynamic Oceanography; Computer Programming and Software; *OCEAN CURRENTS; *FORECASTING; *COORDINATES; *VERTICAL ORIENTATION; *HYBRID SYSTEMS; *OCEAN MODELS; *MARINE CLIMATOLOGY; VELOCITY; COMPUTERIZED SIMULATION; DATA PROCESSING; EDDIES(FLUID MECHANICS); SATELLITE METEOROLOGY; DEEP WATER; SURFACE TEMPERATURE; SALINITY; MIXED LAYER(MARINE); SHALLOW WATER; BATHYMETRY; MARINE ATMOSPHERES; PREDICTIONS; GLOBAL; SYMPOSIA; COASTAL REGIONS; *GLOBAL OCEAN PREDICTION; VERTICAL COORDINATES; NOWCASTING; ECMWF(EUROPEAN CENTER FOR MEDIUM-RANGE WEATHER FORECASTS); SSH(SEA SURFACE HEIGHT); WIND FORCING; THERMAL FORCING; STRATIFIED OCEAN; MIXED OCEAN; SHALLOW OCEAN; PE0601153N; WU738677065; North Atlantic
• Online Access: http://www.dtic.mil/docs/citations/ADA470731; http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA470731

One important aspect of ocean model design is the choice of the vertical coordinate system. Traditional ocean models use a single coordinate type to represent the vertical, but model comparison exercises performed in Europe (DYnamics of North Atlantic MOdels (DYNAMO)) and in the United States (Data Assimilation and Model Evaluation Experiment (DAMEE)) have shown that none of the three main vertical coordinates presently in use (depth [z-levels], density [isopycnal layers], or terrain-following [sigma-levels]) can by itself be optimal everywhere in the ocean. The HYbrid Coordinate Ocean Model (HYCOM) (Bleck, 2002) is configured to combine all three of these vertical coordinate types. It is isopycnal in the open, stratified ocean, but uses the layered continuity equation to make a dynamically smooth transition to a terrain-following coordinate in shallow coastal regions, and to z-level coordinates in the mixed layer and/or unstratified seas. The hybrid coordinate extends the geographic range of applicability of traditional isopycnic coordinate circulation models toward shallow coastal seas and unstratified parts of the world ocean. It maintains the significant advantages of an isopycnal model in stratified regions while allowing more vertical resolution near the surface and in shallow coastal areas, hence providing a better representation of the upper ocean physics. HYCOM is designed to provide a major advance over the existing operational global ocean prediction systems, since it overcomes design limitations of the present systems as well as limitations in vertical and horizontal resolution. The result should be a more streamlined system with improved performance and an extended range of applicability (e.g., the present systems are seriously limited in shallow water and in handling the transition from deep to shallow water). Presented at the High Performance Computing Modernization Program (HPCMP) Users Group Conference held in Denver, CO, on 26-29 Jun 2006. Pub. in the Proceedings of the High Performance Computing Modernization Program (HPCMP) Users Group Conference, p271-274, 2006. Prepared in cooperation with The Center for Ocean-Atmospheric Prediction Studies, Florida State University, Tallahassee, FL, and Planning Systems, Inc., Slidell, LA.