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Closed-form finite-time blow-up and stability for a $(1+2)$D system (E1) derived from the 2D inviscid Boussinesq equations

Yaoming Shi

Abstract

In polar variables $(x,θ)$ on a planar sector, we study a $(1+2)$D system (E1) derived from the two-dimensional inviscid Boussinesq equations. Under a parity/symmetry ansatz on the whole plane (odd/even reflection across the axes), we show that the velocity-pressure form of the 2D inviscid Boussinesq system admits an exact reformulation in terms of Hou--Li type new variables $(u,v,g)$. In the reformulated system (E1), the vortex stretching terms are greatly simplified $(uv,v^2-u^2,-g^2)$. This prompts us to treat $(u,v,g)$ as the \textbf{vorticity building blocks}. Our first main result is the discovery of explicit \emph{smooth} solutions that blow up in finite time $0<T<\infty$ while a natural weighted energy remains \emph{uniformly bounded} for all $t\in[0,T]$. The construction proceeds in three steps. (1) We identify special \emph{ridge rays} $θ_0=\pmπ/4$ such that, under the divergence-free constraint, system (E1) reduces on each ridge to a $(1+1)$D Constantin--Lax--Majda type \emph{convection-free} reaction system in $(t,x)$; (2) We then embed these $(1+1)$D closed-form ridge solutions into the full sector $x\in[0,\infty)$, $θ\in[-π/4,π/4]$ by introducing carefully tuned $θ$-dependent seed data, producing an explicit background profile that blows up only at $(x,θ)=(0,\pmπ/4)$. (3) Finally, we derive the perturbation equations around this background and prove \emph{linear and nonlinear stability} in high-regularity weighted Sobolev norms. Consequently, the constructed background profiles are \emph{stable finite-time blow-up solutions} of (E1).

Closed-form finite-time blow-up and stability for a $(1+2)$D system (E1) derived from the 2D inviscid Boussinesq equations

Abstract

In polar variables on a planar sector, we study a D system (E1) derived from the two-dimensional inviscid Boussinesq equations. Under a parity/symmetry ansatz on the whole plane (odd/even reflection across the axes), we show that the velocity-pressure form of the 2D inviscid Boussinesq system admits an exact reformulation in terms of Hou--Li type new variables . In the reformulated system (E1), the vortex stretching terms are greatly simplified . This prompts us to treat as the \textbf{vorticity building blocks}. Our first main result is the discovery of explicit \emph{smooth} solutions that blow up in finite time while a natural weighted energy remains \emph{uniformly bounded} for all . The construction proceeds in three steps. (1) We identify special \emph{ridge rays} such that, under the divergence-free constraint, system (E1) reduces on each ridge to a D Constantin--Lax--Majda type \emph{convection-free} reaction system in ; (2) We then embed these D closed-form ridge solutions into the full sector , by introducing carefully tuned -dependent seed data, producing an explicit background profile that blows up only at . (3) Finally, we derive the perturbation equations around this background and prove \emph{linear and nonlinear stability} in high-regularity weighted Sobolev norms. Consequently, the constructed background profiles are \emph{stable finite-time blow-up solutions} of (E1).

Paper Structure

This paper contains 24 sections, 6 theorems, 90 equations.

Key Result

Theorem 2.5

System E1(including the divergence-free condition E1(4)) restricted to the rays determined by $\xi^2=\xi_0^2=1$ Assuming Ansatz (I) and Ansatz (II), then we have: (A): Divergence constraint and ridge flatness fixes the ridge rays. Under eq:ray-ansatz and eq:flat, the divergence identity EE10m-4 im Equivalently, In the $(r,z)$--plane this corresponds to the two straight lines through the origin

Theorems & Definitions (19)

  • Remark 2.1
  • Remark 2.2
  • Remark 2.3: $t$-scaling factor ${\color{blue}{\lambda}}$ and $z$-scaling factor ${\mu}$
  • Remark 2.4
  • Theorem 2.5
  • proof : Proof of \ref{['thm:ridge-ray-ridge-functions']}
  • Theorem 2.6: Explicit ridge background and localized finite-time blow-up
  • proof
  • Theorem 2.7: Compatibility condition for preserving ridge flatness
  • proof
  • ...and 9 more