. 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 U VELOCITY LEVEL 1 0 I OE 20E 30E 4-0E 50E 60E 70E 20S- -20S 40S- 60S. 0 10E 20E 30E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL * SCALE FACTOR = 1 .00 FIELD MIN = ) FIELD MAX = 103. Figure Zonal velocity in cm s"1 at m depth in the Agulhas Current region for experiment 1 67. Please note that these images are extracted from scanned page image
. 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 U VELOCITY LEVEL 1 0 I OE 20E 30E 4-0E 50E 60E 70E 20S- -20S 40S- 60S. 0 10E 20E 30E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL * SCALE FACTOR = 1 .00 FIELD MIN = ) FIELD MAX = 103. Figure Zonal velocity in cm s"1 at m depth in the Agulhas Current region for experiment 1 67. 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: ., bookc, bookcentury1900, bookleafnumber89, booksubjectoceanography
