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.
DOI: https://doi.org/10.3402/tellusa.v13i2.9491 | Journal eISSN: 3035-9554
Language: English
Page range: 224 - 230
Published on: Jan 1, 1961
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1961 Henry Stommel, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.