Abstract
The existence of modes of cellular convection driven by thermal instability which are oscillatory in type, rather than steady, has been predicted theoretically for systems that are rotating as a whole. Such modes are of a type called "overstable" by Eddington in a different connection. The result of an initial successful experiment with mercury is given.
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Publication Info
- Year
- 1954
- Type
- article
- Volume
- 94
- Issue
- 6
- Pages
- 1471-1472
- Citations
- 34
- Access
- Closed
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Identifiers
- DOI
- 10.1103/physrev.94.1471