. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASTA 1001 UFRATION 1O0O1 p»o»ULCL OCEAN CLIMATC UOOCL ONE OEGRCC WORLD OCCAN CONFIGURATION MO. I POTENTIAL TEMPERATURE IATITUOF 90E 100E HOE I JOE I 30E i«OE i i i i 90E IOOE I IOE Bonus i oiacnosmc run contfir inifpvul i i en SCALE FACTOR 1. i99 ««e 3>e aii MM »l CASFA 1001 ITERATION 10001 PARALLEL OCEAM CLIMATE UOOCL (POCWI nw OCGREE RORL0 OCEAN CONOG. iJOPr NO. 2 POTENTIAL TEMPERATURE LATITUDE 90E IOOE llOE I JOE I JOE i*0E. Please note that these images are extracted
. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASTA 1001 UFRATION 1O0O1 p»o»ULCL OCEAN CLIMATC UOOCL ONE OEGRCC WORLD OCCAN CONFIGURATION MO. I POTENTIAL TEMPERATURE IATITUOF 90E 100E HOE I JOE I 30E i«OE i i i i 90E IOOE I IOE Bonus i oiacnosmc run contfir inifpvul i i en SCALE FACTOR 1. i99 ««e 3>e aii MM »l CASFA 1001 ITERATION 10001 PARALLEL OCEAM CLIMATE UOOCL (POCWI nw OCGREE RORL0 OCEAN CONOG. iJOPr NO. 2 POTENTIAL TEMPERATURE LATITUDE 90E IOOE llOE I JOE I JOE i*0E. 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: ., bookcentury1900, bookcollectionamerican, booksubjectoceanography
