Long‐Time Decay to the Global Solution of the 2D Dissipative Quasigeostrophic Equation
Jamel Benameur and
Mongi Blel
Abstract and Applied Analysis, 2012, vol. 2012, issue 1
Abstract:
We study the behavior at infinity in time of any global solution θ∈𝒞(ℝ+,H.22-α(ℝ2)) of the surface quasigeostrophic equation with subcritical exponent 2/3 ≤ α ≤ 1. We prove that lim t→∞∥θ(t)∥H.22-α=0. Moreover, we prove also the nonhomogeneous version of the previous result, and we prove that if θ∈𝒞(ℝ+,H.22-α(ℝ2)) is a global solution, then lim t→∞∥θ(t)∥H22-α=0.
Date: 2012
References: Add references at CitEc
Citations:
Downloads: (external link)
https://doi.org/10.1155/2012/627813
Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.
Export reference: BibTeX
RIS (EndNote, ProCite, RefMan)
HTML/Text
Persistent link: https://EconPapers.repec.org/RePEc:wly:jnlaaa:v:2012:y:2012:i:1:n:627813
Access Statistics for this article
More articles in Abstract and Applied Analysis from John Wiley & Sons
Bibliographic data for series maintained by Wiley Content Delivery ().