. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 0 iot ?oe 30E . pobiist diagnostic sun coniow iNtEBvut - e lew-n fieio nin SCALE FACTOR • 9 1B8E-M FIELD MAX 60E •e » 296E-I5I9 5»SI CASEA 200t ITERATION 50001 PARALLEL OCEAN Cl*A*rE MOOEL (POCUI MAir OCGBCE »OPL0 OCEAM COMFIGUPATIOH MO. 2 VOLUME STREAM FUNCTION LEVEL 0 IOE 20E 30E «0E SOE »OE 70E -^7". Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illu


. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 0 iot ?oe 30E . pobiist diagnostic sun coniow iNtEBvut - e lew-n fieio nin SCALE FACTOR • 9 1B8E-M FIELD MAX 60E •e » 296E-I5I9 5»SI CASEA 200t ITERATION 50001 PARALLEL OCEAN Cl*A*rE MOOEL (POCUI MAir OCGBCE »OPL0 OCEAM COMFIGUPATIOH MO. 2 VOLUME STREAM FUNCTION LEVEL 0 IOE 20E 30E «0E SOE »OE 70E -^7". 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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Keywords: ., book, bookcentury1900, bookleafnumber124, booksubjectoceanography