Abstract
The relation of the hydrodynamic helicity and alpha-effect predicted by the mean-field dynamo theory is considered using the three-dimensional dynamo model in the rapidly rotating flat layer heated from below. Despite the theoretical limitations associated with the requirement of uniformity and isotropism of random fields, the alpha-effect is actually proportional to helicity in the geostrophic flows under consideration. Interpretation of this nice agreement is proposed.
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Original Russian Text © M.Yu. Reshetnyak, 2012, published in Doklady Akademii Nauk, 2012, Vol. 444, No. 5, pp. 496–500.
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Reshetnyak, M.Y. The alpha-effect in the presence of rapid rotation. Dokl. Phys. 57, 224–228 (2012). https://doi.org/10.1134/S1028335812060067
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DOI: https://doi.org/10.1134/S1028335812060067