Abstract
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The circulation and changing properties of Eighteen Degree Water are studied using hydrographic data from a long time series at the Panulirus station (32°10'N, 64°30'W) and from the Gulf Stream '60 experiment....
Recommended Citation
Talley, L. D., and M. E. Raymer. 1982. "Eighteen Degree Water variability." Journal of Marine Research 40, (S). https://elischolar.library.yale.edu/journal_of_marine_research/1666
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