A numerical model of the deep circulation using weighted-mean differences in three dimensions has been developed and applied to the distribution of tracers in the Deep Pacific Ocean. It is found that the Stommel-Arons model of the thermohaline circulation applied to the threedimensional distribution of salinity and oxygen explains reasonably well the general features of these distributions with the following parameters...
Fiadeiro, Manuel E., and Harmon Craig. 1978. "Three-dimensional modeling of tracers in the deep Pacific Ocean: I. Salinity and oxygen." Journal of Marine Research 36, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1433