. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. 228 bulletin: museum of compailvtive zoology. Eastern Basin, where the increase, at 200 meters, was about .6%o in this period ( to ). We have no records of seasonal changes in the eastern half of the Gulf after September; for our western stations, this has been discussed (p. 206). Finally, I should point out that the water close to land, off Shel- burne (Station 10313) was even fresher on the surface in September Meter 0. Fig. 74.— Salinity profile across the continental shelf off Shelbume, Nova
. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. 228 bulletin: museum of compailvtive zoology. Eastern Basin, where the increase, at 200 meters, was about .6%o in this period ( to ). We have no records of seasonal changes in the eastern half of the Gulf after September; for our western stations, this has been discussed (p. 206). Finally, I should point out that the water close to land, off Shel- burne (Station 10313) was even fresher on the surface in September Meter 0. Fig. 74.— Salinity profile across the continental shelf off Shelbume, Nova Scotia, June 23. 1915 (Stations 10291-10295). than in June; but it was considerably Salter on the bottom; while a few miles further offshore (Station 10314), salinity as a whole rose considerably during the summer (Fig. 75, 76). The most important seasonal change in density in the Gulf is the fact that the great vertical stability which characterizes the water in summer, practically disappears, as the upper layers cool, in winter,. 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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