Residual estimates from the actual correction-cycle invariant #
The primary family, common chart, weighted strip and carrier sets below are
the actual selected objects. Finite harmonic bounds are read from sourceBand.
Joint flatness of the actual excluded slow-base error #
One fixed schedule controls its entire compact similarity box. Beyond that box the actual residual and virtual stress force both vanish, so the error vanishes in every jet. The resulting estimates impose no upper bound on the similarity radius of the approach to the origin.
The field estimated here is FinalSlowBase.error, which is the actual
Navier--Stokes residual minus its virtual stress force.
The actual implicit scale tends to zero on a joint approach, without
any bound on X = radialEnergy / q.
The original schedule box contains both the supplied upper radius and the end of the active stress annulus.
The exterior equalities hold on an open neighborhood, so they control all actual derivatives of the error, not only its value.
An arbitrary physical approach with compact carrier and q → 0 is
allowed. Its similarity radius need not be bounded. The scale sequence in
FinalSlowBase.error H v upper B is unchanged between the two regions.
The joint past filter at the physical origin #
Origin past, given by 𝓝[SpacetimeEndpoint.openPast 1] ((1 : ℝ), (0 : Space)).
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Full joint vanishing of all actual error jets at (1,0) from the past,
with no bounded-similarity-radius premise.
One actual profile and one fixed enlarged schedule #
The enlargement depends only on the originally selected profile and
the supplied constant, never on the physical point, derivative order, or q.
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Actual error, given by FinalSlowBase.error FinalSlowBase.actualProfile.certificate FinalSlowBase.actualProfile.modulation (actualUpper upper) B.
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Label carrier, given by ActualInitialExcluded.labelCarrier (l.2, l.1) n.
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Invariant type used in actual cycle residual bounds.
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Source, constructed using HarmonicResidual.residualBlock.
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The current pressure alias has every power, by the actual compact primitive and gauge estimates, independently of the accumulated alias.
The missing radial component is derived from the measured pressure debt, the literal reconstructed pressure and the current compact alias.
The independent accumulated axisymmetric alias is retained in the grouping and cancels only through the proved angular mean equation.
The fixed base error uses its actual all-power physical estimate. No flat edge weight is incorrectly assigned to this term.
Smoothness of the actual full graph operator follows from its primitive coefficients and their actual directional derivatives.
The local primitive realization also supplies smoothness of the full native residual across the radial edges. It is not an output-jet premise.
The fixed exterior base and the full physical endpoint #
Actual carriers, phases, and bounded label sums #
Gaussian modes, bundling velocity, pressure, frequency, phase and the required
compatibility proofs.
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Removing each zero Fourier mode preserves the total Gaussian field: the sum of those modes is its actual angular mean, which is zero.
Every term of the literal state residual has the required native gain. The phase loss is fixed once, independently of the cycle index.
The four operations retain the same fixed base error at every stage.
Restriction through the selected dyadic band, including radial edges #
These are geometric statements about the single band actually selected by the dyadic argument. The upper comparison is strict.
- annulus (n : ℕ) : N ≤ n → ∀ w ∈ PhysicalWaveSum.preterminal, PhysicalWaveSum.physicalQ h w ≤ ChartScales.Q n → ChartScales.Q n < 2 * PhysicalWaveSum.physicalQ h w → w ∈ S → (PhysicalGraphBounds.scaledRadial n) w ∈ PhysicalGraphBounds.annulus a b
- in_domain (n : ℕ) : N ≤ n → ∀ w ∈ PhysicalWaveSum.preterminal, PhysicalWaveSum.physicalQ h w ≤ ChartScales.Q n → ChartScales.Q n < 2 * PhysicalWaveSum.physicalQ h w → w ∈ S → ∀ (j : PolarCharts.Index), (PhysicalGraphBounds.scaledRadial n) w ∈ PolarCharts.chartDomain a j → PhysicalResidualJetBounds.polarGraph a h j n (gap n) w ∈ U
- in_closure (n : ℕ) : N ≤ n → ∀ w ∈ PhysicalWaveSum.preterminal, PhysicalWaveSum.physicalQ h w ≤ ChartScales.Q n → ChartScales.Q n < 2 * PhysicalWaveSum.physicalQ h w → w ∈ S → ∀ (j : PolarCharts.Index), (PhysicalGraphBounds.scaledRadial n) w ∈ PolarCharts.chartDomain a j → PhysicalResidualJetBounds.polarGraph a h j n (gap n) w ∈ closure V
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Actual gap, given by ChartScales.nativeIndex ActualPrimary.h n - CommonWindow.index ActualPrimary.h n.
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Actual band graph, given by PhysicalResidualBridge.commonGraph (ChartScales.Q n) ActualPrimary.h (CommonWindow.index ActualPrimary.h n).
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Actual base pressure, given by ActualBaseResidual.basePressure ActualPrimary.certificate ActualPrimary.modulation ActualPrimary.upper B n.
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Only the actual physical realization remains external. Native regularity, the fixed base equation, and all size estimates are derived in this module.
- velocity_smooth (n : ℕ) : N ≤ n → ∀ z ∈ PhysicalWaveSum.preterminal, z ∈ PhysicalResidualTZ.graphSourceTZ (actualBandGraph n) U → ContDiffAt ℝ 2 u (z.1, CylindricalResidual.chart z.2)
- pressure_differentiable (n : ℕ) : N ≤ n → ∀ z ∈ PhysicalWaveSum.preterminal, z ∈ PhysicalResidualTZ.graphSourceTZ (actualBandGraph n) U → DifferentiableAt ℝ P (z.1, CylindricalResidual.chart z.2)
- velocity_germ (n : ℕ) : N ≤ n → ∀ z ∈ PhysicalWaveSum.preterminal, z ∈ PhysicalResidualTZ.graphSourceTZ (actualBandGraph n) U → (fun (y : ProblemStatement.SpaceTime) => u (y.1, CylindricalResidual.chart y.2)) =ᶠ[nhds z] fun (y : ProblemStatement.SpaceTime) => (CylindricalResidual.frame (y.2.ofLp 1)) (PhysicalResidualTZ.velocityTZ (actualBandGraph n) (fun (v : PhysicalResidualTZ.Cylinder) (i : Fin 3) => PhysicalResidualBridge.baseComponents (CorrectionInitialization.ActualPrimary.commonContext B) n v i + PhysicalResidualBridge.incrementComponents s n v i) y)
- pressure_germ (n : ℕ) : N ≤ n → ∀ z ∈ PhysicalWaveSum.preterminal, z ∈ PhysicalResidualTZ.graphSourceTZ (actualBandGraph n) U → CylindricalResidual.pressurePullback P =ᶠ[nhds z] PhysicalResidualTZ.pressureTZ (actualBandGraph n) fun (v : PhysicalResidualTZ.Cylinder) => actualBasePressure B n v + s.totalPressureIncrement n v
- exterior (w : ProblemStatement.SpaceTime) : w ∈ PhysicalWaveSum.preterminal → PhysicalWaveSum.physicalQ CorrectionInitialization.ActualPrimary.h w < ChartScales.Q N → w ∉ active → u w = FinalSlowBase.velocity CorrectionInitialization.ActualPrimary.certificate CorrectionInitialization.ActualPrimary.modulation CorrectionInitialization.ActualPrimary.upper B w ∧ P w = FinalSlowBase.pressure CorrectionInitialization.ActualPrimary.certificate CorrectionInitialization.ActualPrimary.modulation CorrectionInitialization.ActualPrimary.upper B w
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Local exterior equality gives actual field germs inside the valid past sublevel; no global topological-support condition is used.
The native operator and base-pressure obligations of the physical bridge are consequences of the actual selected base and the invariant.
Actual physical stage and iteration consumers #
Physical data: an abbreviation for PhysicalFields B N ActualPolarCoverage.nativeDomain s u P.
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Fixed loss, given by physicalLoss ActualPrimary.h (2 * ActualPrimary.h) m.
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The complete physical residual rate follows from the actual invariant.
The local physical fields are only identified, never bounded, by d.
The finite-residual input of the mixed diagonal assembly. J is the
number of completed correction cycles, including the actual initialized
state at zero. The derivative loss is fixed before J is chosen.