. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. (b) 160° 140° 120° 100. Fig. 15. Geostrophic circulation at 200 m (dynamic height anomalies, 200 over 1000 db.) (Prepared by Reid from a variety of Pacific data; Atlantic derived from Defant, 1941.) B. Subpolar Eastern Currents Where the continents extend to sufficiently high latitudes, they form a barrier to the west-wind drift and cause some portion of the waters to turn poleward. These poleward currents form the eastern limbs of the subpolar gyres and are observed in the North and South Pacif
. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. (b) 160° 140° 120° 100. Fig. 15. Geostrophic circulation at 200 m (dynamic height anomalies, 200 over 1000 db.) (Prepared by Reid from a variety of Pacific data; Atlantic derived from Defant, 1941.) B. Subpolar Eastern Currents Where the continents extend to sufficiently high latitudes, they form a barrier to the west-wind drift and cause some portion of the waters to turn poleward. These poleward currents form the eastern limbs of the subpolar gyres and are observed in the North and South Pacific and in the North Atlantic. They are similar to the subtropical eastern currents in that they are broad and. 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 Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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