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Flexibility for the SQG Equation with an L4/3+L^{4/3+} Active Scalar

Published 17 Aug 2026 in math.AP | (2608.16641v1)

Abstract: We develop a new convex-integration scheme, inspired by \cite{BCK26}, for the inviscid surface quasi-geostrophic equation on the two-dimensional torus. For the explicit, nonoptimized exponent pˉ=43+10<sup>5,\bar p=\frac{4}{3}+10<sup>{-5}, we prove a flexibility theorem for weak solutions in the standard momentum formulation with active scalar [ θ\in C([0,1];L{\bar p}(\mathbb T2)). ] More precisely, any two prescribed mean-zero states in L<sup><ˉ/sup>p(T<sup>2)L<sup>{\bar</sup> p}(\mathbb T<sup>2) can be approximated at the initial and final times by such a solution. The perturbations are constructed from localized, concentrated traveling SQG profiles whose centers move along rational directions and whose radii depend on the Reynolds stress. Time averages of auxiliary sources along these trajectories reconstruct the preceding-stage stress, while a two-dimensional bilinear null-form estimate compensates for the derivative loss caused by the nonlocal constitutive law. Exploiting the time-locality of the iteration, we also obtain a dense subset of the mean-zero space L<sup><ˉ/sup>p(T<sup>2)L<sup>{\bar</sup> p}(\mathbb T<sup>2) such that every initial datum in this subset admits at least two distinct momentum weak solutions. Thus, the construction establishes both flexibility and nonuniqueness beyond the concentration-critical exponent p=4/3p=4/3.

Authors (3)

Summary

  • The paper develops a convex-integration scheme proving flexibility for inviscid SQG in C([0,1];L^{4/3+10^{-5}}), allowing arbitrary mean-zero endpoint states to be approximated by weak solutions.
  • The construction combines traveling counter-rotating dipoles, time-averaged Reynolds-stress reconstruction, variable-radius profiles, and a bilinear null-form estimate that offsets the derivative loss from the nonlocal velocity law.
  • The results yield dense nonuniqueness and weak solutions that fail to conserve the SQG Hamiltonian, while leaving the broader range 4/3 ≤ p < 3 and the endpoint p = 4/3 open.

This paper by Brué, Jin, and Nguyen (2608.16641) develops a convex-integration scheme for the inviscid surface quasi-geostrophic (SQG) equation on the two-dimensional torus and proves two theorems concerning weak solutions whose active scalar has integrability just above the critical threshold p=4/3p=4/3. The work extends the moving-dipole construction of Brué, Colombo, and Kumar for two-dimensional Euler to the SQG momentum formulation, where the transport velocity is one derivative more singular than the potential velocity.

Main results

The paper works with the SQG equation tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=0, u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta, on T2\mathbb T^2, interpreted through the momentum formulation for the potential velocity v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta:

tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.

Weak solutions are defined via the commutator form of the nonlinearity, which remains meaningful for vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2}). The Sobolev embedding W1,pH1/2W^{1,p}\hookrightarrow H^{1/2} holds precisely when p4/3p\ge 4/3, which identifies L4/3L^{4/3} as the natural Lebesgue threshold for this solution class; this is the endpoint treated by De Rosa, Latocca, and Park via vanishing-viscosity limits.

For the explicit, non-optimized exponent tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=00, the first main theorem establishes flexibility: any two prescribed mean-zero states in tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=01 can be approximated in tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=02 at times tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=03 and tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=04 by a weak solution tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=05. The second theorem uses the time-locality of the iteration to produce a dense subset tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=06 of the mean-zero subspace of tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=07 such that every datum in tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=08 admits at least two distinct momentum weak solutions. The authors state this is the first nonuniqueness result for SQG in tθ+uθ=0\partial_t\theta+u\cdot\nabla\theta=09 with u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta0 above the critical threshold.

An immediate consequence of the flexibility theorem concerns the Hamiltonian u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta1. Choosing endpoint states with different Hamiltonians yields a weak solution that does not conserve u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta2, since u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta3 is continuous in the u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta4 topology. This is a strong claim: it is the first failure of Hamiltonian conservation at any u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta5, and the resulting solutions cannot arise as vanishing-viscosity limits of the type constructed by De Rosa, Latocca, and Park, whose procedures produce Hamiltonian-conserving solutions. On the rigidity side, u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta6 guarantees conservation, so the gap between u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta7 and u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta8 remains.

Traveling SQG building blocks

The seed profile is the compactly supported Lipschitz traveling counter-rotating circular pair of Cao, Qin, Zhan, and Zou, satisfying u=Λ1θu=\nabla^\perp\Lambda^{-1}\theta9 with T2\mathbb T^20 and zero total mass. After rotation and rescaling at scale T2\mathbb T^21, the potential velocity scales as T2\mathbb T^22 while the scalar scales as T2\mathbb T^23, so that T2\mathbb T^24 and T2\mathbb T^25 are invariant. The nonzero first moment T2\mathbb T^26 of the profile produces the key identity

T2\mathbb T^27

which forces the exponent T2\mathbb T^28 in the radius-amplitude relation used in the iteration.

Two structural obstacles are handled at this stage. First, the whole-space potential velocity has a noncompact far field; subtracting the exterior harmonic gradient and periodizing, then restoring incompressibility with a periodic gradient corrector, yields a localized divergence-free block T2\mathbb T^29 with v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta0. Second, the block must satisfy two exact identities — the constant-speed momentum equation with a small symmetric error v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta1, and the v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta2-derivative identity v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta3 — which allow the center, amplitude, and radius of the block to vary in time. A fixed-scale spatial mollification (independent of v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta4, so that v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta5 commutes with convolution) makes the profile family smooth jointly in v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta6 while preserving the identities and estimates. The gradient corrector acts as a pressure gauge: since it is a gradient, its contribution to the second slot of the momentum nonlinearity v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta7 vanishes identically.

The convex-integration iteration

At stage v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta8, the mollified Reynolds stress is decomposed into four positive rank-one components v=(Δ)1θv=\nabla^\perp(-\Delta)^{-1}\theta9 along rational directions with long periods tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.0. The principal perturbation consists of a single traveling block at any given time: the coarse time interval of length tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.1 is partitioned into four disjoint active subintervals, so distinct principal blocks never interact. The spatially varying radius is chosen by tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.2, where tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.3 is the intervalwise time average of tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.4, and the center moves along the rational direction tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.5 at speed inversely proportional to tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.6. Consequently, the block completes at least tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.7 closed periods per active subinterval, and the time spent in a region is weighted by tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.8.

The stress is reconstructed through temporal averaging rather than low-frequency wave interactions: the time average of an auxiliary vector source along the trajectories reproduces tv+uv(v)Tu+p=0,divv=0,u=Λv.\partial_t v+u\cdot\nabla v-(\nabla v)^Tu+\nabla p=0,\qquad \operatorname{div}v=0,\qquad u=\Lambda v.9 up to an error of size vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})0. An auxiliary fixed-width profile with an explicitly uniform orbit average replaces the variable-radius source, and a Leray-projected time corrector absorbs the zero-mean temporal oscillation, vanishing at the endpoints of each coarse interval. The new Reynolds stress comprises six components — linear interaction, corrector interaction, time-freezing, auxiliary-average, building-block, and source-replacement errors — each bounded by vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})1 under the parameter hierarchy.

The null form and why the gain is small

The central new difficulty relative to the Euler construction of [BCK26] is the nonlocal relation vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})2: the linear interaction with the background contains one derivative of the concentrated profile, and a direct estimate incurs a negative power of the concentration radius. The paper circumvents this with the two-dimensional identity vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})3 and a bilinear null-form estimate

vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})4

proved in the appendix via the multilinear Christ–Journé commutator estimates of Seeger, Smart, and Street. The null form replaces the unfavorable derivative norm of the concentrated perturbation by a norm of its potential velocity, and is essential for closing the linear error.

The null form, however, does not by itself explain the smallness of vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})5. For vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})6 the concentration exponent vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})7 is positive, and the differentiated block satisfies vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})8. Fitting the vLloc2(I;H1/2)v\in L^2_{\mathrm{loc}}(I;H^{1/2})9 bookkeeping requires W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}0, which for the admissible parameters (W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}1, W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}2, W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}3, W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}4, W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}5, W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}6) forces W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}7, i.e., W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}8. Thus the tiny gain above the endpoint is dictated by the amount of profile concentration the remaining parameter hierarchy can absorb, and the exponent is explicitly non-optimized.

Limitations and open problems

The paper is explicit about the boundaries of the construction. The exponent W1,pH1/2W^{1,p}\hookrightarrow H^{1/2}9 is far from the rigidity threshold p4/3p\ge 4/30, and extending flexibility to the full range p4/3p\ge 4/31 — in particular constructing Hamiltonian-nonconserving solutions with integrability arbitrarily close to p4/3p\ge 4/32 — is left open. For the generalized SQG family p4/3p\ge 4/33, the moment scaling, critical exponent, and derivative loss all depend on p4/3p\ge 4/34, and it is unknown whether the temporal stress reconstruction and a fractional analogue of the null form survive the modified scaling; even a fixed small dissipation produces a high-frequency error not absorbed by the present iteration, with a frequency-dependent vanishing-dissipation regime suggested as a more accessible first problem. Finally, the whole-space problem is obstructed by the averaging mechanism itself: the construction relies on closed rational trajectories that repeatedly sample the coefficient being reconstructed, whereas on p4/3p\ge 4/35 a block escapes, so an extension would require finite sweeping trajectories or a large-box limit with uniform control of moments and nonlocal tails.

Conclusion

The paper establishes flexibility between arbitrary prescribed endpoint states, failure of Hamiltonian conservation, and dense nonuniqueness for inviscid SQG weak solutions with active scalar in p4/3p\ge 4/36 for p4/3p\ge 4/37, crossing the concentration-critical Lebesgue exponent in the standard momentum formulation. The construction combines traveling SQG profiles with time-dependent radius and position, orbit-averaged temporal reconstruction of the Reynolds stress, and a bilinear null-form estimate that compensates for the derivative loss inherent in the nonlocal constitutive law p4/3p\ge 4/38. The quantitative gap between the achieved exponent and both the endpoint p4/3p\ge 4/39 and the rigidity threshold L4/3L^{4/3}0 delineates the current reach of the method.

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