. 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 90E 1 ON 0- 10S- 20S - 30S 40S. """ '^A T 90E 100E 110E 120E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL = *M FIELD M[N SCALE FACTOR = FIELD MAX 1 30E -20S -30S 40S 140E +15 1124 . 50E. ) 1121 .) Figure 1 7 3 Horizontal volume transport in Sv(=10J-'1 cmJ s"1) in the western Australia region for exp
. 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 90E 1 ON 0- 10S- 20S - 30S 40S. """ '^A T 90E 100E 110E 120E A- ROBUST DIAGNOSTIC RUN CONTOUR INTERVAL = *M FIELD M[N SCALE FACTOR = FIELD MAX 1 30E -20S -30S 40S 140E +15 1124 . 50E. ) 1121 .) Figure 1 7 3 Horizontal volume transport in Sv(=10J-'1 cmJ s"1) in the western Australia region for experiment 1. 71. 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
