Geodesic
Solution of the inverse problem describing slow thermal convection in a rotating layer
The Bulletin of Irkutsk State University. Series Mathematics, Tome 44 (2023), pp. 3-18 Cet article a éte moissonné depuis la source Math-Net.Ru

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The linear inverse initial-boundary value problem arising when modeling the rotational motion of a viscous heat-conducting liquid in a flat layer is solved. It is shown that the problem has two different integral identities. Based on these identities, a priori estimates of the solution in a uniform metric are obtained and its uniqueness is proved. The conditions for the input data are also determined, under which this solution goes to the stationary mode with increasing time according to the exponential law. In the final part, the existence of a unique classical solution of the inverse problem is proved. To do this, differentiating the problem by a spatial variable, we come to a direct non-classical problem with two integral conditions instead of the usual boundary conditions. The new problem is solved by the method of separation of variables, which makes it possible to find a solution in the form of rapidly converging series on a special basis.
Keywords: thermal convection, inverse problem, stationary solution.
Mots-clés : liquid motion 
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Viktor K. Andreev; Liliya I. Latonova. Solution of the inverse problem describing slow thermal convection in a rotating layer. The Bulletin of Irkutsk State University. Series Mathematics, Tome 44 (2023), pp. 3-18. http://geodesic.mathdoc.fr/item/IIGUM_2023_44_a0/

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