. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 100t ITERATION 1000 1 PARALLEL OCEAN CLIUAIE UOOEL (POCU) ONE OEGPEE HORLO OCCAM CONFIGURATION NO 2 VOLUME STREAM FUNCTION LEVEL 90E IO0E t IOE I JOE I 30E I40E ION. 90E 100E I IOE I JOE »_ pnnii^T « 1121 CASEA 2001 ITERATION 50001 PARALLEL OCEAN CIXATE >J00EL (POCMT HALF OEGRCE WOULD OCEAN CONFIGURATION NO. J VOLUME STREAM FUNCTION LEVEL ?»0E IOOE I IOE I JOE I 30E I «0E. Please note that these images are extracted from scanned page images that may have been digit
. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 100t ITERATION 1000 1 PARALLEL OCEAN CLIUAIE UOOEL (POCU) ONE OEGPEE HORLO OCCAM CONFIGURATION NO 2 VOLUME STREAM FUNCTION LEVEL 90E IO0E t IOE I JOE I 30E I40E ION. 90E 100E I IOE I JOE »_ pnnii^T « 1121 CASEA 2001 ITERATION 50001 PARALLEL OCEAN CIXATE >J00EL (POCMT HALF OEGRCE WOULD OCEAN CONFIGURATION NO. J VOLUME STREAM FUNCTION LEVEL ?»0E IOOE I IOE I JOE I 30E 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
Size: 1659px × 1506px
Photo credit: © Library Book Collection / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookcollectionamerican, booksubjectoceanography
