. Carnegie Institution of Washington publication. On Changes in the Sea and Their Relation to Organisms. 217 ing of top and bottom water several times a day; the mixing was not rapid enough, however, to equalize the temperature to the depth of 50 meters on a calm sunny day. Palitzsch (1912 6) found the average. FIG. 2.—Currents of the Atlantic Ocean. The arrows show direction. The heavy lines are the courses of two derelicts, drifted by currents and winds. O2 in surface water of the North Atlantic to be per liter during the day and at Please note that these images are ext
. Carnegie Institution of Washington publication. On Changes in the Sea and Their Relation to Organisms. 217 ing of top and bottom water several times a day; the mixing was not rapid enough, however, to equalize the temperature to the depth of 50 meters on a calm sunny day. Palitzsch (1912 6) found the average. FIG. 2.—Currents of the Atlantic Ocean. The arrows show direction. The heavy lines are the courses of two derelicts, drifted by currents and winds. O2 in surface water of the North Atlantic to be per liter during the day and at 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 Carnegie Institution of Washington. Washington, Carnegie Institution of Washington
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