Thermohaline Convection with Two Stable Regimes of Flow

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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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Henry Stommel (Sun,) studied this question.

synapsesocial.com/papers/69d7543baa68b335b4f30f8d https://doi.org/https://doi.org/10.3402/tellusa.v13i2.9491

Discussion

Journals

Tellus A Dynamic Meteorology and Oceanography

Institutions

Harvard University

Los Angeles Pierce College

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