The actual angular mean equation along the correction cycle #
The analytic input is on the primitive harmonic coefficients and the actual stream reconstructions. Incompressibility and the angular mean identity are conclusions for the literal stored states.
Local regularity of the actual finite harmonic coefficients.
- phase (n : ℕ) : ContDiffOn ℝ (↑⊤) (b.phase n) V
- pressure (n : ℕ) : HarmonicResidual.SmoothCoefficients V (b.pressure n)
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The real and complex cylindrical divergence operators agree on the actual real-valued components, including their Fréchet derivatives.
A zero velocity harmonic also removes its derivative contribution.
Per-mode solenoidality implies divergence zero for the actual finite harmonic field. The zero harmonic is controlled explicitly.
Point: an abbreviation for CyclePoint.
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Inputs on the existing state, the two actual waves, and the primitive stream construction. No outgoing divergence or mean equation is a field.
- domain : p.strip.domain ⊆ LocalRankDefect.positiveDomain U.carrier
- particular_covariance (i j : Fin 3) : GaugeMomentBalances.MovingField U p.gauge.radial.inner p.gauge.radial.outer (SignedMeanGain.covarianceIncrement u.oscillation (p.particularVelocity v c u) i j)
- signed_covariance (i j : Fin 3) : GaugeMomentBalances.MovingField U p.gauge.radial.inner p.gauge.radial.outer (SignedMeanGain.covarianceIncrement (p.afterParticular v c u).oscillation (p.signedVelocity v c u) i j)
- rank : LocalRankDefect.RankGeometry p.gauge p.rank U.carrier c u
- particular_regular (l : ι) : BlockData p.strip.domain (p.particularBlock v c u l)
- signed_regular (l : ι) : BlockData p.strip.domain (p.signedBlock v c u l)
- particular_solenoidal (l : ι) : HarmonicWaveInteraction.ModeSolenoidal p.strip c (p.particularBlock v c u l)
- signed_solenoidal (l : ι) : HarmonicWaveInteraction.ModeSolenoidal p.strip c (p.signedBlock v c u l)
- signed_carrier (l : ι) : CorrectionStep.SameCarrier (v.blocks l) (p.signedBlock v c u l)
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Each wave contributes zero actual divergence; both subsequent mean increments are the genuine divergence-free stream reconstructions.
The complete primitive mean-PDE hypotheses are preserved by the actual four updates, including pressure reconstruction and error refresh.
A fixed local domain is used throughout the actual stored iteration. The step inputs are on its constructed waves and streams, not mean identities.
Specialization to the literal initializer: its mean-PDE hypotheses come from the proved initialization theorem, not an additional premise.