. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITERATION 10001 PARALLEL OCEAN CLIMATE MODEL (POCM) ONE DEGREE WORLD OCEAN CONFIGURATION NO. 2 V VELOCITY LEVEL 1 0 0 -s 20S- 40S -. 60S 50E 1 1 1 1— 0 10E 20E 30E 40E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL = FIELD MIN = SCALE FACTOR = FIELD MAX = 20S -4-0S 60S 60E 121. 70E () 141 Figure Meridional velocity in cm s" *? at depth in the Agulhas Current region for experiment 1. 68. Please note that these images are extracted from sca
. An analysis of results of a high-resolution world ocean circulation model. Oceanography. CASEA 1001 ITERATION 10001 PARALLEL OCEAN CLIMATE MODEL (POCM) ONE DEGREE WORLD OCEAN CONFIGURATION NO. 2 V VELOCITY LEVEL 1 0 0 -s 20S- 40S -. 60S 50E 1 1 1 1— 0 10E 20E 30E 40E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL = FIELD MIN = SCALE FACTOR = FIELD MAX = 20S -4-0S 60S 60E 121. 70E () 141 Figure Meridional velocity in cm s" *? at depth in the Agulhas Current region for experiment 1. 68. 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
