  In this paper, we consider the following anisotropic quasi-geostrophic
equations \begin{equation}\tag*{$(AQG)_{\alpha,\beta}$} \partial_t\theta+
u_\theta.\nabla\theta +\mu|\partial_1|^{2\alpha}\theta+\nu
|\partial_2|^{2\beta}\theta=0,\quad u_\theta=\mathcal{R}^{\perp}\theta,
\end{equation} where $\min\{\alpha,\beta\}=\frac{1}{2}$ et
$\max\{\alpha,\beta\}\in \left(\frac{1}{2},1\right)$. This equation is a
particular case of the equation introduced by Ye (2019) in \cite{YZ}. In this
paper, we prove that for any initial data $\theta^0$ in the Sobolev space
$H^{s}(\mathbb{R}^2)$, $s >1$, the equation $(AQG)_{\alpha,\beta}$ has a global
solution $\theta$ in $C_b(\mathbb{R}^+,H^s(\mathbb{R}^2)).$
