Computation of Super High-Resolution Global Ocean Model using Earth Simulator

  • Kim, Dong-Hoon (Central Research Institute of Electric Power Industry (CRIEPI)) ;
  • Norikazu Nakashiki (Central Research Institute of Electric Power Industry (CRIEPI) ;
  • Yoshikatsu Yoshida (Central Research Institute of Electric Power Industry (CRIEPI) ;
  • Takaki Tsubono (Central Research Institute of Electric Power Industry (CRIEPI) ;
  • Frank O. Bryan (Mational Center for Atmospheric Research (NCAR) ;
  • Richard D.Smith (Los Alamos National Laboratory (LANL) ;
  • Mathew E. Maltrud (Los Alamos National Laboratory (LANL) ;
  • Matthew W. Hecht (Los Alamos National Laboratory (LANL) ;
  • Julie L. McClean (Naval Postgraduate School)
  • Published : 2003.08.01

Abstract

The need fur higher grid resolution in climate models is often discussed (e.g. McAvaney et al.,2001) because a number of important oceanic processes are not resolved by the current generation of coupled models, e.g., boundary currents, mesoscale eddy fluxes, sill through flows. McClean et al., (1997) and Bryan and Smith (1998) have compared simulated mesoscale variability in simulations at several eddy-resolving resolutions to TOPEX/Poseidon and similar data. (omitted)

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