. An analysis of results of a high-resolution world ocean circulation model. Oceanography. LATITUDE (DEGREES a. LJ Q d 25 50 75 100 135 185 260 360 510 710 985 1335 1750 2200 2750 3300 3850 4400 4800 5200 755 TTTTTTn 30S imiimiiiiiiiiiiiiiiiiiiiiijiiiiuiutbj lllllllllllllll 1111111H11111111\ I Illllllll. 65N llllllllllllllll Figure Indian-Pacific meridional volume transport in units of 10?LX craJ s"L for experiment 1 (positive values clockwise; negative values counterclockwise). 87. Please note that these images are extracted from scanned page images that may have been digitall
. An analysis of results of a high-resolution world ocean circulation model. Oceanography. LATITUDE (DEGREES a. LJ Q d 25 50 75 100 135 185 260 360 510 710 985 1335 1750 2200 2750 3300 3850 4400 4800 5200 755 TTTTTTn 30S imiimiiiiiiiiiiiiiiiiiiiiijiiiiuiutbj lllllllllllllll 1111111H11111111\ I Illllllll. 65N llllllllllllllll Figure Indian-Pacific meridional volume transport in units of 10?LX craJ s"L for experiment 1 (positive values clockwise; negative values counterclockwise). 87. 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
