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John Wilkin wilkin@marine.rutgers.edu

ROMS surface temperature and velocity for 2001-Jul-23 (day 20 of 60-day simulation). Model grid resolution is 1 km. Velocity vectors are plotted for every 4 th grid point. The full domain is shown Initial conditions are from climatology.

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John Wilkin wilkin@marine.rutgers.edu

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  1. ROMS surface temperature and velocity for 2001-Jul-23 (day 20 of 60-day simulation).Model grid resolution is 1 km. Velocity vectors are plotted for every 4th grid point. The full domain is shown Initial conditions are from climatology. Configuration details:Fairall et al. bulk formulae with model SST and observed Tair, qair, Qsw, Qlw (met mooring obs assumed uniform throughout model domain). Open boundaries are climatology plus tides (7 major harmonics from ADCIRC model) John Wilkin wilkin@marine.rutgers.edu

  2. Comparison of ROMS and CTD section between SECNAV and ASIMET moorings (2001-Jul-23) ROMS configuration: Air-sea fluxes: Fairall et al. bulk formulae with model SST and observed Tair, qair, Qsw, Qlw (met mooring obs assumed uniform throughout model domain). Open boundaries are climatology plus tides John Wilkin wilkin@marine.rutgers.edu

  3. Comparison of ROMS surface height with C-BLAST 2001 pressure gauge data ROMS observed

  4. ROMS subsurface temperature at ASIT mooring location, CBLAST 2001 Air-sea fluxes: Fairall et al. bulk formulae with model SST and observed marine boundary layer Tair, qair, Qsw, Qlw from MVCO and mooring (assumed uniform throughout model domain). Open boundary condition: Climatological T,S; tides

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