Global attractor of the three dimensional primitive equations of large-scale ocean and atmosphere dynamics in an unbounded domain
Bo You, Fang Li

TL;DR
This paper investigates the long-term behavior of solutions to the 3D primitive equations modeling large-scale ocean and atmosphere dynamics in an unbounded domain, establishing the existence of a global attractor despite compactness challenges.
Contribution
It proves the existence of a global attractor for the primitive equations in an unbounded domain by overcoming the lack of Sobolev compactness using tail-estimates and energy methods.
Findings
Existence of a global attractor for the primitive equations.
Overcoming Sobolev embedding limitations in unbounded domains.
Establishment of asymptotic compactness in a weak phase space.
Abstract
This paper is concerned with the long-time behavior of solutions for the three dimensional primitive equations of large-scale ocean and atmosphere dynamics in an unbounded domain. Since the Sobolev embedding is no longer compact in an unbounded domain, we cannot obtain the asymptotical compactness of the semigroup generated by problem (2.4)-(2.6) by the Sobolev compactness embedding theorem even if we obtain the existence of an absorbing set in more regular phase space. To overcome this difficulty, we first prove the asymptotical compactness in a weak phase space of the semigroup generated by problem (2.4)-(2.6) by combining the tail-estimates and the energy methods. Thanks to the existence of an absorbing set in more regular phase space, we establish the existence of a global attractor of problem (2.4)-(2.6) by virtue of Sobolev interpolation inequality.
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsStability and Controllability of Differential Equations · Advanced Mathematical Physics Problems · Arctic and Antarctic ice dynamics
