FINITE-TIME SINGULARITY REACHED
Gradient blowup: ||∇u||_L∞ → ∞. Smoothness breaks down at x* = (0, 0, 0).
Controls viscous dissipation rate (-νΔu). Set to 0 for Euler flow.
Spatial wavepacket frequency scale for initial perturbation.
Self-similar vortex stretching exponent: ||ω||_∞ ~ (T* - t)⁻⁷.
Initial Parameters Extracted from Proof
The problem: Existence and smoothness of the Navier-Strokes equation
Solution parameters derived from the Lean 4 formalized proof repository (openai/NavierStokesAndEuler) based on the
Córdoba–Martínez-Zoroa & Alpöge–Buckmaster multiscale wavepacket induction scheme.
Odd-symmetric initial profile with zero spatial mean
Viscous dissipation term νΔu
Geometric sequence of high-frequency modes
Rapidly decaying envelope ensuring C^∞ regularity
Bounded high-frequency background force counteracting viscous dissipation during scale transitions
A smooth solution u(x,t) breaks down at time T* if and only if the time integral of peak vorticity ||ω(t)||_L∞ diverges to infinity. As t → T*, the vorticity concentrates near the origin x* = 0 according to:
Peak Vorticity ||ω||_∞ & Enstrophy Divergence
Fourier Energy Cascade Spectrum E(k)
Energy transferring from low wavenumbers (k₀) to fine scales (k_N) as singularity approaches.