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The general surface quasi-geostrophic equation is the scalar transport equation defined by \begin{equation*} \frac{\partial \theta}{\partial t}+v^\gamma_1 \frac{\partial \theta}{\partial x_1}+v^\gamma_2 \frac{\partial \theta}{\partial x_2}…

Analysis of PDEs · Mathematics 2025-07-15 Diego Córdoba , José Lucas-Manchón , Luis Martínez-Zoroa

We construct solutions in $\mathbb{R}^2$ with finite energy of the surface quasi-geostrophic equations (SQG) that initially are in $C^k$ ($k\geq 2$) but that are not in $C^{k}$ for $t>0$. We prove a similar result also for $H^{s}$ in the…

Analysis of PDEs · Mathematics 2022-05-03 Diego Córdoba , Luis Martínez-Zoroa

We establish the well/ill-posedness theories for the inviscid $\alpha$-surface quasi-geostrophic ($\alpha$-SQG) equations in H\"older spaces, where $\alpha = 0$ and $\alpha = 1$ correspond to the two-dimensional Euler equation in the…

Analysis of PDEs · Mathematics 2024-05-03 Young-Pil Choi , Jinwook Jung , Junha Kim

In this paper, we are concerned with the Cauchy problem of the generalized surface quasi-geostrophic (SQG) equation in which the velocity field is expressed as $u=K\ast\omega$, where $\omega=\omega(x,t)$ is an unknown function and…

Analysis of PDEs · Mathematics 2018-10-02 Huan Yu , Xiaoxin Zheng , Quansen Jiu

This paper establishes several existence and uniqueness results for two families of active scalar equations with velocity fields determined by the scalars through very singular integrals. The first family is a generalized surface…

Analysis of PDEs · Mathematics 2011-01-19 Dongho Chae , Peter Constantin , Diego Córdoba , Francisco Gancedo , Jiahong Wu

We introduce and analyze a class of Surface Quasi-Geostrophic (SQG) equations in the presence of moving rigid obstacles. The model is motivated both by vortex-wave type asymptotics for singular structures in active scalar equations and by…

Analysis of PDEs · Mathematics 2026-05-25 Ludovic Godard-Cadillac , Arnab Roy

In this article we consider the low regularity well-posedness of the surface quasi-geostrophic (SQG) front equation. Recent work on other quasilinear models, including the gravity water waves system and nonlinear waves, have demonstrated…

Analysis of PDEs · Mathematics 2023-11-09 Albert Ai , Ovidiu-Neculai Avadanei

In this article we consider the following generalized quasi-geostrophic equation \partial_t\theta + u\cdot\nabla \theta + \nu \Lambda^\beta \theta =0, \quad u= \Lambda^\alpha \mathcal{R}^\bot\theta, \quad x\in\mathbb{R}^2, where $\nu>0$,…

Analysis of PDEs · Mathematics 2011-08-24 Changxing Miao , Liutang Xue

We consider the SQG equation without dissipation on the half-plane with Dirichlet boundary condition, and prove local wellposedness in the spaces $W^{3,p}$ and $C^{2,\beta}$ for any $1<p<\infty$ and $0<\beta<1$. We complement this…

Analysis of PDEs · Mathematics 2025-06-10 In-Jee Jeong , Junha Kim , Hideyuki Miura

We use a nonlocal maximum principle to prove the global existence of smooth solutions for a slightly supercritical surface quasi-geostrophic equation. By this we mean that the velocity field $u$ is obtained from the active scalar $\theta$…

Analysis of PDEs · Mathematics 2015-05-28 Michael Dabkowski , Alexander Kiselev , Vlad Vicol

We prove the existence of global $L^2$ weak solutions for a family of generalized inviscid surface-quasi geostrophic (SQG) equations in bounded domains of the plane. In these equations, the active scalar is transported by a velocity field…

Analysis of PDEs · Mathematics 2018-03-16 Huy Quang Nguyen

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…

Analysis of PDEs · Mathematics 2025-12-30 Ken Abe , Javier Gómez-Serrano , In-Jee Jeong

The $\beta$-generalized quasi-geostrophic equation is studied in the range of $\alpha \in (0, 1), \beta \in (1/2, 1), 1/2 < \alpha + \beta < 3/2$. When $\alpha \in (1/2, 1), \beta \in (1/2, 1)$ such that $1 \leq \alpha + \beta < 3/2$, using…

Analysis of PDEs · Mathematics 2011-08-23 Kazuo Yamazaki

In the present study, we find that the surface quasi-geostrophic equation admits exact solutions, which evolve with time in quasi-stationary states. The solutions presented are available for any dissipation effect $\kappa (-\Delta)^\alpha$…

Analysis of PDEs · Mathematics 2021-05-04 Zhi-Min Chen

We address the well-posedness theory for the magento-geostrophic equation, namely an active scalar equation in which the divergence-free drift velocity is one derivative more singular than the active scalar. In the presence of supercritical…

Analysis of PDEs · Mathematics 2015-05-30 Susan Friedlander , Walter Rusin , Vlad Vicol

This paper studies a family of generalized surface quasi-geostrophic (SQG) equations for an active scalar $\theta$ on the whole plane whose velocities have been mildly regularized, for instance, logarithmically. The well-posedness of these…

Analysis of PDEs · Mathematics 2021-09-10 Michael S. Jolly , Anuj Kumar , Vincent R. Martinez

We establish the short-time existence and uniqueness of non-decaying solutions to the generalized Surface Quasi-Geostrophic equations in H\"older-Zygmund spaces $C^r(\mathbb{R}^2)$ for $r>1$ and uniformly local Sobolev spaces…

Analysis of PDEs · Mathematics 2025-07-15 Zachary Radke

In this article, we study the critical dissipative surface quasi-geostrophic equation (SQG) in $ \mathbb{R}^2$. Motivated by the study of the homogeneous statistical solutions of this equation, we show that for any large initial data…

Analysis of PDEs · Mathematics 2015-06-11 Omar Lazar

We consider the inviscid generalized surface quasi-geostrophic equation (gSQG) in a patch setting, where the parameter $\alpha \in (1,2)$. The cases $\alpha = 0$ and $\alpha = 1$ correspond to 2d Euler and SQG respectively, and our choice…

Analysis of PDEs · Mathematics 2017-06-01 Diego Córdoba , Javier Gómez-Serrano , Alexandru D. Ionescu

We consider the Cauchy problem for the logarithmically singular surface quasi-geostrophic (SQG) equation, introduced by Ohkitani, $$\partial_t \theta - \nabla^\perp \log(10+(-\Delta)^{\frac12})\theta \cdot \nabla \theta = 0 ,$$ and…

Analysis of PDEs · Mathematics 2025-02-18 Dongho Chae , In-Jee Jeong , Jungkyoung Na , Sung-Jin Oh
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