. An analysis of results of a high-resolution world ocean circulation model. Oceanography. "i 1 r "i 1 r i 1 r in - 111 1 0 s> «- X .5 en t— i— <? 3 0 *—' h- <r o n - 5 en z «r CC i— -1 .0 i— <t hi T -1 b -2 0 -2 5 ? CURVE A CURVE B CURVE C CURVE D Overturning Gyre Diffus ive Total -60 -40 -20 0 LATITUDE (DEGREES) 20 40 60 Figure Atlantic meridional heat transport for experiment 1 (positive values northward negative values southward). 84. Please note that these images are extracted from scanned page images that may have been digitally enhanced for
. An analysis of results of a high-resolution world ocean circulation model. Oceanography. "i 1 r "i 1 r i 1 r in - 111 1 0 s> «- X .5 en t— i— <? 3 0 *—' h- <r o n - 5 en z «r CC i— -1 .0 i— <t hi T -1 b -2 0 -2 5 ? CURVE A CURVE B CURVE C CURVE D Overturning Gyre Diffus ive Total -60 -40 -20 0 LATITUDE (DEGREES) 20 40 60 Figure Atlantic meridional heat transport for experiment 1 (positive values northward negative values southward). 84. 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
