. An analysis of results of a high-resolution world ocean circulation model. Oceanography. SON I20E I30E I40E '50E *- 1/2 DEG BOBU5T DIAGNOSTIC "UN, 3 YR BEST cwtoi« iMiinvAt . i n f lELO hin SCALE FACICfl . 1 99 HELD HA» 2 oe MM 75E.*5 75NI 1121 25NI CASCA 2001 ITERATION 100001 PAnAiiri orrAM rtiMAtr uoon ipocui maif of core »opio ocean configuration no. } POTENTIAL TEMPERATURE LEVEL ' 70E 1 10E MOE ISOE I60E I 70E SON -f. 1 1 1 , 1 L 50N. I20E I30E I40E ISOE A- 1/2 OEG POBUST DIAGNOSTIC THERM I 99 FIELD HIN ? I60E CONIOUH SCALE FACTOR i m FIELD MAX


. An analysis of results of a high-resolution world ocean circulation model. Oceanography. SON I20E I30E I40E '50E *- 1/2 DEG BOBU5T DIAGNOSTIC "UN, 3 YR BEST cwtoi« iMiinvAt . i n f lELO hin SCALE FACICfl . 1 99 HELD HA» 2 oe MM 75E.*5 75NI 1121 25NI CASCA 2001 ITERATION 100001 PAnAiiri orrAM rtiMAtr uoon ipocui maif of core »opio ocean configuration no. } POTENTIAL TEMPERATURE LEVEL ' 70E 1 10E MOE ISOE I60E I 70E SON -f. 1 1 1 , 1 L 50N. I20E I30E I40E ISOE A- 1/2 OEG POBUST DIAGNOSTIC THERM I 99 FIELD HIN ? I60E CONIOUH SCALE FACTOR i m FIELD MAX <68 MSI 2SNI Figure Potential temperature in °C at m depth in the Kuroshio Current region (a) for experiment 3 and (b) for experiment 4. 109. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Barton, Wesley Monterey, California: U. S. Naval Postgraduate School


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