English

Global solutions to the dissipative quasi-geostrophic equation with dispersive forcing

Analysis of PDEs 2019-11-07 v2

Abstract

We consider the initial value problem for the 2D quasi-geostrophic equation with weak dissipation term κ(Δ)α/2θ (0<α1)\kappa(-\Delta)^{\alpha/2}\theta\ (0<\alpha\leqslant 1) and dispersive forcing term Au2Au_2. We establish a unique global solution for a given initial data θ0\theta_0 which belongs to the scaling subcritical Sobolev space Hs(R2) (s>2α)H^s(\mathbb{R}^2)\ (s>2-\alpha) if the size of dispersion parameter is sufficiently large. This phenomenon is so-called the global regularity. We also obtain the relationship between the initial data and the dispersion parameter, which ensures the existence of the global solution. Moreover, we show the global regularity in the scaling critical Sobolev space H2α(R2)H^{2-\alpha}(\mathbb{R}^2) and find that the size of dispersion parameter to ensure the global existence is determined by each subset KH2α(R2)K\subset H^{2-\alpha}(\mathbb{R}^2), which is precompact in some homogeneous Sobolev spaces.

Keywords

Cite

@article{arxiv.1908.11524,
  title  = {Global solutions to the dissipative quasi-geostrophic equation with dispersive forcing},
  author = {Mikihiro Fujii},
  journal= {arXiv preprint arXiv:1908.11524},
  year   = {2019}
}

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28pages