. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 1 r ^ r - LP cr UJ I 1 .5 UJ 1 .0 IS X 3 a. -1 .0 -1 .5 ^ CURVE A CURVE B CURVE C CURVE D Overturning Gyre Di ffus ive Total I _L -60 -40 -20 0 20 LATITUDE (DEGREES) 40 60 Figure Indian-Pacific meridional heat transport for experiment 1 (positive values northward; negative values southward). 83. 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 m


. An analysis of results of a high-resolution world ocean circulation model. Oceanography. 1 r ^ r - LP cr UJ I 1 .5 UJ 1 .0 IS X 3 a. -1 .0 -1 .5 ^ CURVE A CURVE B CURVE C CURVE D Overturning Gyre Di ffus ive Total I _L -60 -40 -20 0 20 LATITUDE (DEGREES) 40 60 Figure Indian-Pacific meridional heat transport for experiment 1 (positive values northward; negative values southward). 83. 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: ., book, bookcentury1900, bookleafnumber105, booksubjectoceanography