. 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 VOLUME STREAM FUNCTION LEVEL 0 10E 20E 30E 40E 50E 60E 70E 0 - 20S- 40S - v \. ** »** \ *""?- (jB ?.-?._—? *'" 60S -20S -40S 60S 40E 50E 0 10E 20E 30E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL = *14 FIELD MIN = SCALE FACTOR = FIELD MAX = 60E 70E *14 ) *15 ) Figure Horizontal volume transport in Sv( = 10J-^ cmJ s "&
. 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 VOLUME STREAM FUNCTION LEVEL 0 10E 20E 30E 40E 50E 60E 70E 0 - 20S- 40S - v \. ** »** \ *""?- (jB ?.-?._—? *'" 60S -20S -40S 60S 40E 50E 0 10E 20E 30E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL = *14 FIELD MIN = SCALE FACTOR = FIELD MAX = 60E 70E *14 ) *15 ) Figure Horizontal volume transport in Sv( = 10J-^ cmJ s ""•*?) in the Agulhas Current region for experiment 1. 69. 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
