SECT. 3] EASTERN BOUNDARY CURRENTS 279 



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Trop. Tuna Comm., 2 (4), 129-156. 

 Hutchinson, G. E., 1950. Survey of existing knowledge of biogeochemistry. The bio- 

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 Knauss, J., I960. Measurements of the Cromwell Current. Deep-Sea Res., 6, 265-286. 

 Koninklijk Nederlands Meteorologisch Instituut, 1952. Indian Ocean oceanographic and 



meteorological data. K.N.M.I. No. 135, 2nd Ed., 24 charts. 

 Marchand, J. M., 1953. Twenty-third annual report for the year ended December, 1951. 



Un. S. Africa, Dep. Comm. Indus., Div. Fish., 181 pp. 

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and salinity in water under the action of radiation, conduction, evaporation and 



mixing due to the resulting convection. Bull. Scripps. Inst. Oceanog. Univ. Calif., 2, 



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 Meteorological Office, 1956. Monthly Meteorological Charts of the Eastern Pacific Ocean. 



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 Montgomery, R. B., 1938. Circulation in upper layers of southern North Atlantic deduced 



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Woods Hole Oceanog. Inst., 6 (2), 1-55. 

 Munk, W. H., 1950. On the wind-driven ocean circulation. J. Met., 7, 79-93. 

 National Institute of Oceanography, 1957. Station list 1950-1951. Discovery Reps., 28, 



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 Pacific Oceanographic Group, 1957. Physical, chemical and plankton data record, North 



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 Posner, G. S., 1957. The Peru Current. Bull. Bingham Oceanog. Coll., 16 (2), 106-155. 

 Redfield, A. C, 1958. The biological control of chemical factors in the environment. 



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respect to the 1000-decibar surface. Tellus, 13, 489-502. 

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Atlantic and Pacific Oceans in their upper kilometer. Deep-Sea Res., 7, No. 4, 265-275. 

 Reid, J. L., Jr., 1962. Measurements of the California Countercurrent at a depth of 



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 Schott, G., 1933. Auftriebwasser an den australischen Westkiisten ? Ja und Nein! Ann. 



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 xx + 413 pp., 37 plates. 



