As a model problem for the barotropic mode of the primitive equations of the oceans and atmosphere, we consider the Euler system on a bounded convex planar domain Ω, endowed with non-penetrating boundary conditions. For 43≤p≤2, and initial and forcing data with Lp(Ω) vorticity we show the existence of a weak solution, enriching and extending the results of Taylor (2000) [32].In the physical case of a rectangular domain Ω=[0, L1]×[0, L2], a similar result holds for all 2<∞ as well. Moreover, by means of a new BMO-type regularity estimate for the Dirichlet problem on a planar domain with corners, we prove uniqueness of solutions with bounded initial vorticity. © 2013 Elsevier Ltd.
The Euler equations in planar nonsmooth convex domains / Bardos, C.; Di Plinio, F.; Temam, R.. - In: JOURNAL OF MATHEMATICAL ANALYSIS AND APPLICATIONS. - ISSN 0022-247X. - 407:1(2013), pp. 69-89. [10.1016/j.jmaa.2013.05.005]
The Euler equations in planar nonsmooth convex domains
Di Plinio F.;
2013
Abstract
As a model problem for the barotropic mode of the primitive equations of the oceans and atmosphere, we consider the Euler system on a bounded convex planar domain Ω, endowed with non-penetrating boundary conditions. For 43≤p≤2, and initial and forcing data with Lp(Ω) vorticity we show the existence of a weak solution, enriching and extending the results of Taylor (2000) [32].In the physical case of a rectangular domain Ω=[0, L1]×[0, L2], a similar result holds for all 2<∞ as well. Moreover, by means of a new BMO-type regularity estimate for the Dirichlet problem on a planar domain with corners, we prove uniqueness of solutions with bounded initial vorticity. © 2013 Elsevier Ltd.File | Dimensione | Formato | |
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