. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. 490 PATTULLO [chap. 22 We cannot, with such a distribution of data, be certain as to the behavior of the central portion of this ocean. Fig. 5a does illustrate, however, that all of these gauges show negative deviations in March, with the extreme value recorded at Cape Schmidt ( — 19 cm) as noted in the discussion of Fig. 1. Fig. 5b (September) contains no negative values within the Arctic proper, and. Please note that these images are extracted from scanned page images that may have been digita
. The Composition of sea-water : comparative and descriptive oceanography. Seawater -- Composition. 490 PATTULLO [chap. 22 We cannot, with such a distribution of data, be certain as to the behavior of the central portion of this ocean. Fig. 5a does illustrate, however, that all of these gauges show negative deviations in March, with the extreme value recorded at Cape Schmidt ( — 19 cm) as noted in the discussion of Fig. 1. Fig. 5b (September) contains no negative values within the Arctic proper, 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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