. An analysis of results of a high-resolution world ocean circulation model. Oceanography. t 90E IOOE I IOE 1 JOE • 3or A- 1/7 OFG ROHU^l niAGNOSlIC RUN, 3 TR OESI MOE CONTOUR INTERVAL • 1 00 FIELD WIN • -2 B3 1113 SHI SCALE FACTO* . 1 00 FIELO n»i • 0X1 CASEA 2001 llhWAIION I00OCI1 PARALLEL OCCAM CLIMATE UOOCL (POCUJ IIALf OCGACC >ORU) OCCAM C OMTtOuPA riON MO. 2 V VELOCITY I ATITIIOE 90C 100E 110E I JOE I 30E HOC. 90E IOOE I IOE I 20E 1 30E I40E I- 1/2 OtG HUHUST l)IA(,NOSIIC I Ht RM contcir intervn • i eg fieiohin. -2 38 1113 **f v t\\ SCALE
. An analysis of results of a high-resolution world ocean circulation model. Oceanography. t 90E IOOE I IOE 1 JOE • 3or A- 1/7 OFG ROHU^l niAGNOSlIC RUN, 3 TR OESI MOE CONTOUR INTERVAL • 1 00 FIELD WIN • -2 B3 1113 SHI SCALE FACTO* . 1 00 FIELO n»i • 0X1 CASEA 2001 llhWAIION I00OCI1 PARALLEL OCCAM CLIMATE UOOCL (POCUJ IIALf OCGACC >ORU) OCCAM C OMTtOuPA riON MO. 2 V VELOCITY I ATITIIOE 90C 100E 110E I JOE I 30E HOC. 90E IOOE I IOE I 20E 1 30E I40E I- 1/2 OtG HUHUST l)IA(,NOSIIC I Ht RM contcir intervn • i eg fieiohin. -2 38 1113 **f v t\\ SCALE fttlOR 1 80 FIELD rv>» 2.(4 1113 em Figure Zonal cross-section of meridional velocity in cm s"1 at °S latitude off of western Australia (a) for experiment 3 and (b) for experiment 4. 108. 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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