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Thermohaline Convection with Two Stable Regimes of Flow

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Stommel, Henry·1961·Tellus A: Dynamic Meteorology and Oceanography

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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Metadata

Authors
Stommel, H.
Venue
Tellus A: Dynamic Meteorology and Oceanography
Published
1961-01-01
Volume
13
Issue
2
Pages
224-230
ISSN
  • 0280-6495 (ISSN-L)
  • 1600-0870
OpenAlex
W2024330627
Cited by
1,289
References
0
FWCI
0.00
Type
journal article
Language
en
Open access
hybrid

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CoChat. (2026). Citation check: Thermohaline Convection with Two Stable Regimes of Flow. https://app.cochat.ai/papers/10.3402/tellusa.v13i2.9491
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Stommel, H. (1961). Thermohaline Convection with Two Stable Regimes of Flow. Tellus A: Dynamic Meteorology and Oceanography. https://doi.org/10.3402/tellusa.v13i2.9491

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.