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Thermohaline Convection with Two Stable Regimes of Flow

Henry Stommel
- 01 May 1961 - 
- Vol. 13, Iss: 2, pp 224-230
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TLDR
Free convection between two interconnected reservoirs, due to density differences maintained by heat and salt transfer to the reservoirs, is shown to occur sometimes in two different stable regimes, and may possibly be analogous to certain features of the oseanic circulation as discussed by the authors.
Abstract
Free convection between two interconnected reservoirs, due to density differences maintained by heat and salt transfer to the reservoirs, is shown to occur sometimes in two different stable regimes, and may possibly be analogous to certain features of the oseanic circulation.

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Vertical mixing, energy, and the general circulation of the oceans

TL;DR: In particular, small-scale mixing processes are necessary to resupply the potential energy removed in the interior by the overturning and eddy-generating process as discussed by the authors, and it is shown that over most of the ocean significant vertical mixing is confined to topographically complex boundary areas implies a potentially radically different interior circulation than is possible with uniform mixing.
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