. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. 268 WOOSTER AND REID [CHAP. 11 minimal values of the index (at 30°-35°N and 20°-25°S respectively) appear to separate two seasonally different upwelling regimes. 4. In the Canary, Benguela and California Currents the latitude of the index maximum migrates seasonally, being farther south in spring than in summer. Unfortunately no direct measurements of vertical velocity are available, but indirect manifestations of the upwelling process can be used to investigate the validity of the index as an i
. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. 268 WOOSTER AND REID [CHAP. 11 minimal values of the index (at 30°-35°N and 20°-25°S respectively) appear to separate two seasonally different upwelling regimes. 4. In the Canary, Benguela and California Currents the latitude of the index maximum migrates seasonally, being farther south in spring than in summer. Unfortunately no direct measurements of vertical velocity are available, but indirect manifestations of the upwelling process can be used to investigate the validity of the index as an indicator of 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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