Abstract
In standard oceanographic usage the suffix "-cline" denotes a layer in which there is a relatively large vertical gradient of the given property. However, oceanographers have no term available to denote the contrasting feature: a layer of water in which there is a relative minimum of the absolute value of the vertical gradient....
Recommended Citation
Seitz, R. C.. 1967. "Thermostad, the antonym of thermocline." Journal of Marine Research 25, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1099
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