. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. SECT. 3] EASTERN BOUNDARY CURRENTS 269 most intense up welling, surface temperatures will be lower than normal for that latitude. At the same time the annual variation of net incoming solar energy increases from the equator toward higher latitudes (Haurwitz and Austin, 1944). Thus, at mid-latitudes a summer maximum of upwelling will 160° 140° 120. 160° 140° 120° 100' Fig. 13. Average yearly variations of surface temperature (°C). (Pacific adapted from Schott, 1935, and Meteorological Office, 195
. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. SECT. 3] EASTERN BOUNDARY CURRENTS 269 most intense up welling, surface temperatures will be lower than normal for that latitude. At the same time the annual variation of net incoming solar energy increases from the equator toward higher latitudes (Haurwitz and Austin, 1944). Thus, at mid-latitudes a summer maximum of upwelling will 160° 140° 120. 160° 140° 120° 100' Fig. 13. Average yearly variations of surface temperature (°C). (Pacific adapted from Schott, 1935, and Meteorological Office, 1956; Atlantic adapted from Bohnecke, 1936.). 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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