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Homogeneous steady states for the generalized surface quasi-geostrophic equations

Ken Abe, Javier Gómez-Serrano, In-Jee Jeong

TL;DR

This work classifies homogeneous stationary self-similar solutions of the generalized surface quasi-geostrophic equations across the full parameter range 0< s <1. It builds a linear-nonlinear framework on high-frequency angular spaces, delivering a sharp polar-mode formula for the fractional Laplacian and introducing the non-local 2s-th order operator $\mathcal{L}(s,β)$. Through rigorous L^p and Hölder estimates and a PS-based variational scheme, the authors prove existence of odd-symmetric solutions for β in $(-m_0-2s, -2s)$ and $(0, m_0+2)$ and nonexistence for $-2s\le β\le 0$, while identifying five distinct regimes relating to scale-invariance and local well-posedness. Numerical experiments corroborate the analytical results and illustrate how the angular profiles encode high-frequency content as β varies, including the approach to Bahouri–Chemin-type patches. The results illuminate the landscape of self-similar structures in gSQG and provide a robust methodology for analyzing nonlocal, scale-invariant PDEs in fluid dynamics.

Abstract

We consider homogeneous (stationary self-similar) solutions to the generalized surface quasi-geostrophic (gSQG) equations parametrized by the constant $0<s<1$, representing the 2D Euler equations ($s=1$), the SQG equations $(s=1/2)$, and stationary equations ($s=0$); namely, solutions whose stream function $ψ$ and advected scalar $ω$ are of the form \begin{align*} ψ=\frac{w(θ)}{r^β},\quad ω=\frac{g(θ)}{r^{β+2s}}, \end{align*} in polar coordinates $(r,θ)$ with parameter $β\in \mathbb{R}$. We classify homogeneous steady states across the full parameter space, and we identify the limiting singular regimes assuming an odd symmetric profile $(w,g)$ with Fourier modes larger than $m_0\geq 1$. Specifically, we show existence of such solutions for $-m_0-2s<β<-2s$ and $0<β<m_0+2$ ($1/2-s<β< m_0+2$ for $0<s<1/2$) and non-existence of such solutions for $-2s\leq β\leq 0$. The main result provides examples of self-similar solutions which belong to critical and supercritical regimes for the local well-posedness of the gSQG equations for $0<s<1$ and the first examples of self-similar solutions for the SQG equations and the more singular equations $0<s\leq 1/2$ in the stationary setting. We also complement our findings with a numerical illustration of the solutions.

Homogeneous steady states for the generalized surface quasi-geostrophic equations

TL;DR

This work classifies homogeneous stationary self-similar solutions of the generalized surface quasi-geostrophic equations across the full parameter range 0< s <1. It builds a linear-nonlinear framework on high-frequency angular spaces, delivering a sharp polar-mode formula for the fractional Laplacian and introducing the non-local 2s-th order operator . Through rigorous L^p and Hölder estimates and a PS-based variational scheme, the authors prove existence of odd-symmetric solutions for β in and and nonexistence for , while identifying five distinct regimes relating to scale-invariance and local well-posedness. Numerical experiments corroborate the analytical results and illustrate how the angular profiles encode high-frequency content as β varies, including the approach to Bahouri–Chemin-type patches. The results illuminate the landscape of self-similar structures in gSQG and provide a robust methodology for analyzing nonlocal, scale-invariant PDEs in fluid dynamics.

Abstract

We consider homogeneous (stationary self-similar) solutions to the generalized surface quasi-geostrophic (gSQG) equations parametrized by the constant , representing the 2D Euler equations (), the SQG equations , and stationary equations (); namely, solutions whose stream function and advected scalar are of the form \begin{align*} ψ=\frac{w(θ)}{r^β},\quad ω=\frac{g(θ)}{r^{β+2s}}, \end{align*} in polar coordinates with parameter . We classify homogeneous steady states across the full parameter space, and we identify the limiting singular regimes assuming an odd symmetric profile with Fourier modes larger than . Specifically, we show existence of such solutions for and ( for ) and non-existence of such solutions for . The main result provides examples of self-similar solutions which belong to critical and supercritical regimes for the local well-posedness of the gSQG equations for and the first examples of self-similar solutions for the SQG equations and the more singular equations in the stationary setting. We also complement our findings with a numerical illustration of the solutions.

Paper Structure

This paper contains 43 sections, 42 theorems, 208 equations, 19 figures.

Key Result

Theorem 1.2

Let $0< s< 1$, $m_0\in \mathbb{N}$, and $-m_0-2s<\beta< m_0+2$. The following holds for odd symmetric homogeneous solutions eq:HS and eq:Sineseri for the stationary gSQG equations eq:SgSQG with profiles $(w,g)$.

Figures (19)

  • Figure 1: $1/2< s< 1$ (Case $s=3/4$)
  • Figure 2: $s=1/2$
  • Figure 3: $0<s< 1/2$ (Case $s=1/4$)
  • Figure 6: Five self-similar regimes (i)-(v) in critical and supercritical regimes $\beta\geq -2$ for local well-posedness of gSQG (Case $s=3/4$ and $m_0=2$)
  • Figure 7: The ranges of $\beta$ and variational principles. Case $s=1/4$ and $m_0=2$
  • ...and 14 more figures

Theorems & Definitions (82)

  • Theorem 1.2
  • Lemma 2.1
  • Proposition 2.3: Poles and zeros for $|m|$
  • proof
  • Proposition 2.4: Monotonicity
  • proof
  • Proposition 2.5: Asymptotics
  • proof
  • Proposition 2.6: Poles and zeros for $\beta$
  • proof
  • ...and 72 more