Abstract
In the absence of horizontal flow, the surface salinity of any part of the ocean is mainly determined by three processes: Decrease of salinity by precipitation P, increase of salinity by evaporation E, and change of salinity by vertical mixing
Recommended Citation
Jacobs, Woodrow C.. 1948. "Some empirical relations between seasonal values of (E–P) and surface salinities over the North Atlantic." Journal of Marine Research 7, (3). https://elischolar.library.yale.edu/journal_of_marine_research/672
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