. An analysis of results of a high-resolution world ocean circulation model. Oceanography. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our WOOI O OCFAN NO 7 L> VELOCITY LEVEL I I40E 1S0E I60E I 70E f80 I 70«r. I40C ISOE I60E A- ROBUST DIAGNOSTIC RUN CLNIUH INItHVAL • 5 00 SCALE FACTOR 1 00 FIlLO «IN FIELD MAI -12 0 1151 00E 15 00SI Figure (a) Meridional and (b) zona


. An analysis of results of a high-resolution world ocean circulation model. Oceanography. I40E 1S0E IfcOE A- ROBUST DIAGNOSTIC RUN LOMIUUH INItHVAL • 5 00 FltLO niN . -39 •» IVfi *t -W Dtfbl SCALE FACTOR . 1 00 FIELD M»» « iwwe «8 00si CASCA 1001 ITCRATION 10001 PAAAJ I Fl OrFAN CI IMATT UOflFI (POCMI Our WOOI O OCFAN NO 7 L> VELOCITY LEVEL I I40E 1S0E I60E I 70E f80 I 70«r. I40C ISOE I60E A- ROBUST DIAGNOSTIC RUN CLNIUH INItHVAL • 5 00 SCALE FACTOR 1 00 FIlLO «IN FIELD MAI -12 0 1151 00E 15 00SI Figure (a) Meridional and (b) zonal velocity in cm s~l at m depth in the East Australian Current region for experiment 1. 63. 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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