. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. 33-8% Fig. 49.— Salinity profile from the trough between Jeffrey's Ledge and the mainland (Station 10104) to the centre of the Gulf of Maine (Station 10090). than further east, especially at the bottom, while the very sudden dip of the curve of suggests that vertical circulation was active in the Bay. And this may well have been the case, as the tidal currents are of some strength in the neighborhood of Station 10106. The eastern end of the profile shows a sudden spreading of the curves over the coast
. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. 33-8% Fig. 49.— Salinity profile from the trough between Jeffrey's Ledge and the mainland (Station 10104) to the centre of the Gulf of Maine (Station 10090). than further east, especially at the bottom, while the very sudden dip of the curve of suggests that vertical circulation was active in the Bay. And this may well have been the case, as the tidal currents are of some strength in the neighborhood of Station 10106. The eastern end of the profile shows a sudden spreading of the curves over the coast bank, such as we found in 1912 (1914a), the range of salinity for the entire column of water on German Bank being only from The only exception to the rule that salinity in- creased from west to east is afforded by Station 10093, where the. 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 Harvard University. Museum of Comparative Zoology. Cambridge, Mass. : The Museum
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