Abstract
We consider a family of singular surface quasi-geostrophic equations
on \([0,\infty )\times {\mathbb {T}}^{2}\), where \(\nu \geqslant 0\), \(\gamma \in [0,3/2)\), \(\alpha \in [0,1/4)\) and \(\xi \) is a space-time white noise. For the first time, we establish the existence of infinitely many non-Gaussian
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probabilistically strong solutions for every initial condition in \(C^{\eta }\), \(\eta >1/2\);
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ergodic stationary solutions.
The result presents a single approach applicable in the subcritical, critical as well as supercritical regime in the sense of Hairer (Invent Math 198(2):269–504, 2014). It also applies in the particular setting \(\alpha =\gamma /2\) which formally possesses a Gaussian invariant measure. In our proof, we first introduce a modified Da Prato–Debussche trick which, on the one hand, permits to convert irregularity in time into irregularity in space and, on the other hand, increases the regularity of the linear solution. Second, we develop a convex integration iteration for the corresponding nonlinear equation which yields non-unique non-Gaussian solutions satisfying powerful global-in-time estimates and generating stationary as well as ergodic stationary solutions.
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R.Z. and X.Z. are grateful for the financial supports by National Key R &D Program of China (No. 2022YFA1006300). R.Z. gratefully acknowledges financial support from the NSFC (No. 11922103, 12271030). X.Z. is grateful for the financial supports in part by National Key R &D Program of China (No. 2020YFA0712700) and the NSFC (Nos. 12090014, 12288201) and the support by key Lab of Random Complex Structures and Data Science, Youth Innovation Promotion Association (2020003), Chinese Academy of Science. The research of M.H. was funded by the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (Grant Agreement No. 949981). The research of M.H., R.Z. and X.Z. was funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)—SFB 1283/2 2021—317210226.
Appendix A. Some auxiliary results
Appendix A. Some auxiliary results
In this part, we recall some auxiliary lemmas from [12]. The first result is rather classical and permits to rewrite the nonlinearity and formulate the notion of weak solution as in Definition 1.1.
Proposition A.1
[12, Proposition 5.1] Let \({\mathcal {R}}={\mathcal {R}}_{j}\), \(j=1,2\). Assume that \(\phi \in H^{3}\) and \(\theta \in {\dot{H}}^{-1/2}\). Then we have
The second result is a kind of Leibniz rule useful in the estimate of the new stress in Sect. 6.5.
Lemma A.2
[12, Lemma 2.1] Let \(|l|=1,\lambda l\in {\mathbb {Z}}^2\), and \(g(x)=a(x)\cos (\lambda l\cdot x).\) Then
where
Finally, in order to control the operators in Lemma A.2, we rely on the following.
Lemma A.3
[12, Lemma 3.3] Assume \(b_0:{{\mathbb {T}}}^2\rightarrow {{\mathbb {R}}}\) with \({{\,\textrm{supp}\,}}({\hat{b}}_0)\subset \sup \{|k|\leqslant \mu \}\) and \(10\leqslant \mu \leqslant \frac{1}{2}\lambda \). Then
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Hofmanová, M., Luo, X., Zhu, R. et al. Surface quasi-geostrophic equation perturbed by derivatives of space-time white noise. Math. Ann. (2024). https://doi.org/10.1007/s00208-024-02881-1
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DOI: https://doi.org/10.1007/s00208-024-02881-1