Abstract
A thermodynamic model of sea snow-ice cover growth under the influence of heat flows on its upper and lower surfaces is presented. The growing is described with an extended region of phase transition (a two-phase region) with a linear temperature distribution. The temperature of the upper surface is calculated with the use of a heat-balance equation on the basis of determinable meteorological observation data. The comparison of the model results with freezing experimental data is performed.
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Original Russian Text © P.V. Bogorodskii, A.P. Makshtas, A.V. Pnyshkov, 2009, published in Okeanologiya, 2009, Vol. 49, No. 3, pp. 359–367.
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Bogorodskii, P.V., Makshtas, A.P. & Pnyshkov, A.V. Sea ice growth at nonstationary ocean-atmosphere heat exchange. Oceanology 49, 330–337 (2009). https://doi.org/10.1134/S0001437009030059
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DOI: https://doi.org/10.1134/S0001437009030059