. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. 274 WOOSTER AND RE1D [CHAP. 1 1 shore to be further evidence of sub-surface flow from the north. Similarly, evidence of sub-surface poleward flow off" the Canary coast was inferred by Montgomery (1938) from the distribution of properties and can be traced as far as 20°N on the 200-db chart (Fig. 15). The relation between coastal upwelling and counterflow at depth has been discussed by Yoshida and collaborators (Yoshida, 1955; Yoshida and Mao, 1957; Yoshida and Tsuchiya, 1957; Yoshida, 1958)

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. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. 274 WOOSTER AND RE1D [CHAP. 1 1 shore to be further evidence of sub-surface flow from the north. Similarly, evidence of sub-surface poleward flow off" the Canary coast was inferred by Montgomery (1938) from the distribution of properties and can be traced as far as 20°N on the 200-db chart (Fig. 15). The relation between coastal upwelling and counterflow at depth has been discussed by Yoshida and collaborators (Yoshida, 1955; Yoshida and Mao, 1957; Yoshida and Tsuchiya, 1957; Yoshida, 1958), but the exact nature of the boundary processes is not yet well understood. (a) 160' 140° 120 100° 80°. (b) 160° 140° 120° 100. 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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