Abstract
This paper examines the relative importance, in the equation of motion, of the convective acceleration terms and of the extra pressure gradient due to a longitudinal gradient of salinity up an estuary. For estuaries in which the latter is the most important, a criterion is given for the direction of mean water velocity just above the bed.
Recommended Citation
Abbott, M. R.. 1960. "Salinity effects in estuauies." Journal of Marine Research 18, (2). https://elischolar.library.yale.edu/journal_of_marine_research/949
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