Abstract
Since the ocean is hydrostatic to a very good approximation, it is well known that dynamic topography at the surface (for example, across the Gulf Stream) is inverted and magnified at the thermocline by a factor proportional to the average density difference of the regions above and below the thermocline....
Recommended Citation
Baker, D. J.. 1968. "A demonstration of magnification of dynamic topography at the thermocline." Journal of Marine Research 26, (3). https://elischolar.library.yale.edu/journal_of_marine_research/1134
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