Physical bounds for locally finite native copies #
Each native copy retains its own center and its own full oscillatory carrier. We sum these waves, not their amplitudes under one unwrapped phase. Closed, locally finite, disjoint native cells give an actual single-copy germ. The physical estimate is then the center-independent single-carrier estimate, followed by the existing bounded overlap estimate for the outer labels.
Pull back the native cells only near the evaluation point. Global continuity of the physical graph at the axis is not needed.
The lattice copy is a separate index. In particular, neither the center nor the phase profiles have to agree between different copies.
- gap : PhysicalWaveSum.BandLabel → ℕ
Gap of
CopyFamily, of typeBandLabel → ℕ. - carrier : K → PhysicalWaveSum.BandLabel → PhysicalWaveSum.CarrierData
Carrier of
CopyFamily, of typeK → BandLabel → CarrierData. - amplitude : K → PhysicalWaveSum.WaveIndex H → PhysicalWaveSum.LiftPoint → ℂ
Amplitude of
CopyFamily, of typeK → WaveIndex H → LiftPoint → ℂ.
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Copy, given by ⟨f.gap, f.carrier k, f.amplitude k⟩.
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Term, given by (f.copy k).term a h r0 I.
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Sum full local carriers, including their individual phases.
Equations
- f.periodized a h r0 I w = ∑' (k : K), f.term a h r0 I k w
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Sum, given by ∑ᶠ I, f.periodized a h r0 I w.
Equations
- f.sum a h r0 w = ∑ᶠ (I : NavierStokes.PhysicalWaveSum.WaveIndex H), f.periodized a h r0 I w
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The old single-copy regularity hypotheses are imposed separately on each actual copy. No support condition is imposed using one center for the whole periodized amplitude.
- copy (k : K) : PhysicalWaveSum.RegularFamily (f.copy k) a b h r0 Z Δ
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Native support cells can depend on the outer label. Their index is independent of both the harmonic and the physical point.
Cells of
SupportCells, of typeBandLabel → PeriodizedWaveBounds.Cells LiftPoint K.- support (I : PhysicalWaveSum.WaveIndex H) (k : K) : Function.support (f.amplitude k I) ⊆ (self.cells I.1).carrier (↑I.1).1 k
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Off the fixed radial annulus, all copies vanish on one common neighborhood. This also handles the axis without a smooth graph there.
On a specified native copy cell, the full sum equals that full copy. The identity keeps the copy's own phase as well as its amplitude.
Actual full derivative tensors agree with the selected local copy.
Closed-cell membership holds at every point where a copy can have a nonzero jet, including the boundary of its amplitude support.
Only native jets on a copy's own closed cell are used. No bounds for uncut data far from that copy are required.
- amplitude (k : K) (I : PhysicalWaveSum.WaveIndex H) (w : ProblemStatement.SpaceTime) : w ∈ PhysicalWaveSum.preterminal → PhysicalWaveSum.physicalParams h w ∈ PhysicalWaveSum.labelRegion (CoordinateAlgebra.D h) ↑I.1 → (PhysicalGraphBounds.scaledRadial (↑I.1).1) w ∈ PhysicalGraphBounds.annulus a b → PhysicalWaveSum.commonLift h (↑I.1).1 (f.gap I.1) w ∈ (hc.cells I.1).carrier (↑I.1).1 k → ∀ i ≤ m, ‖iteratedFDeriv ℝ i (f.amplitude k I) (PhysicalWaveSum.commonLift h (↑I.1).1 (f.gap I.1) w)‖ ≤ A * ChartScales.Q (↑I.1).1 ^ g * ChartScales.S (↑I.1).1 ^ eAmp
- base_F (k : K) (I : PhysicalWaveSum.WaveIndex H) (w : ProblemStatement.SpaceTime) : w ∈ PhysicalWaveSum.preterminal → PhysicalWaveSum.physicalParams h w ∈ PhysicalWaveSum.labelRegion (CoordinateAlgebra.D h) ↑I.1 → (PhysicalGraphBounds.scaledRadial (↑I.1).1) w ∈ PhysicalGraphBounds.annulus a b → PhysicalWaveSum.commonLift h (↑I.1).1 (f.gap I.1) w ∈ (hc.cells I.1).carrier (↑I.1).1 k → ∀ (chart : PolarCharts.Index), (PhysicalGraphBounds.scaledRadial (↑I.1).1) w ∈ PolarCharts.chartDomain a chart → ∀ i ≤ m, ‖iteratedFDeriv ℝ i (f.carrier k I.1).F (PhysicalGraphBounds.slotMap (PolarCharts.chart a chart) (ChartScales.timeCoefficient h (↑I.1).1) (f.carrier k I.1).center r0 (PhysicalGraphBounds.physicalLift h (↑I.1).1 w)).1‖ ≤ B * ChartScales.S (↑I.1).1 ^ eBase
- base_G (k : K) (I : PhysicalWaveSum.WaveIndex H) (w : ProblemStatement.SpaceTime) : w ∈ PhysicalWaveSum.preterminal → PhysicalWaveSum.physicalParams h w ∈ PhysicalWaveSum.labelRegion (CoordinateAlgebra.D h) ↑I.1 → (PhysicalGraphBounds.scaledRadial (↑I.1).1) w ∈ PhysicalGraphBounds.annulus a b → PhysicalWaveSum.commonLift h (↑I.1).1 (f.gap I.1) w ∈ (hc.cells I.1).carrier (↑I.1).1 k → ∀ (chart : PolarCharts.Index), (PhysicalGraphBounds.scaledRadial (↑I.1).1) w ∈ PolarCharts.chartDomain a chart → ∀ i ≤ m, ‖iteratedFDeriv ℝ i (f.carrier k I.1).G (PhysicalGraphBounds.slotMap (PolarCharts.chart a chart) (ChartScales.timeCoefficient h (↑I.1).1) (f.carrier k I.1).center r0 (PhysicalGraphBounds.physicalLift h (↑I.1).1 w)).1‖ ≤ B * ChartScales.S (↑I.1).1 ^ eBase
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The number of native copies does not enter the constant or the power loss. At a physical point the actual wave has just one copy germ.
Actual cutoff amplitudes, pulled from their weighted native coefficient through the common-coordinate map. Only the map's positive jets are bounded; its values and the copy centers may be unbounded.
- sourceIndex : K → PhysicalWaveSum.WaveIndex H → ι
Source index of
CommonChart, of typeK → WaveIndex H → ι. - map : K → PhysicalWaveSum.WaveIndex H → PhysicalWaveSum.LiftPoint → D
Map of
CommonChart, of typeK → WaveIndex H → LiftPoint → D. - domain : K → PhysicalWaveSum.WaveIndex H → Set PhysicalWaveSum.LiftPoint
Domain of
CommonChart, of typeK → WaveIndex H → Set LiftPoint. - smooth (k : K) (I : PhysicalWaveSum.WaveIndex H) : ContDiffOn ℝ (↑⊤) (self.map k I) (self.domain k I)
- amplitude_eq (k : K) (I : PhysicalWaveSum.WaveIndex H) : f.amplitude k I = fun (x : PhysicalWaveSum.LiftPoint) => ChartScales.Q (↑I.1).1 ^ σ • source (self.sourceIndex k I) (↑I.1).1 (self.map k I x)
- contains (k : K) (I : PhysicalWaveSum.WaveIndex H) (z : ProblemStatement.SpaceTime) : z ∈ PhysicalWaveSum.preterminal → PhysicalWaveSum.physicalParams h z ∈ PhysicalWaveSum.labelRegion (CoordinateAlgebra.D h) ↑I.1 → (PhysicalGraphBounds.scaledRadial (↑I.1).1) z ∈ PhysicalGraphBounds.annulus a b → PhysicalWaveSum.commonLift h (↑I.1).1 (f.gap I.1) z ∈ (hc.cells I.1).carrier (↑I.1).1 k → PhysicalWaveSum.commonLift h (↑I.1).1 (f.gap I.1) z ∈ self.domain k I
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The native weighted bound is converted using the genuine higher chain rule. The same constants work for every label and every native copy.
Copy band domain, bundling scale, carrier, isOpen, one_le_scale.
Equations
- One or more equations did not get rendered due to their size.
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The carrier profiles are estimated on their actual local slow regions. The regions need contain a point only when that point belongs to this copy.
- region : K → PhysicalWaveSum.BandLabel → Set PhysicalGraphBounds.Slow
Region of
CarrierBounds, of typeK → BandLabel → Set PhysicalGraphBounds.Slow. - jets : PhaseJetBounds.PolynomialJets (copyBandDomain self.region ⋯) fun (i : K × PhysicalWaveSum.BandLabel) (x : PhysicalGraphBounds.Slow) => ((f.carrier i.1 i.2).F x, (f.carrier i.1 i.2).G x)
- contains (k : K) (I : PhysicalWaveSum.WaveIndex H) (z : ProblemStatement.SpaceTime) : z ∈ PhysicalWaveSum.preterminal → PhysicalWaveSum.physicalParams h z ∈ PhysicalWaveSum.labelRegion (CoordinateAlgebra.D h) ↑I.1 → (PhysicalGraphBounds.scaledRadial (↑I.1).1) z ∈ PhysicalGraphBounds.annulus a b → PhysicalWaveSum.commonLift h (↑I.1).1 (f.gap I.1) z ∈ (hc.cells I.1).carrier (↑I.1).1 k → ∀ (chart : PolarCharts.Index), (PhysicalGraphBounds.scaledRadial (↑I.1).1) z ∈ PolarCharts.chartDomain a chart → (PhysicalGraphBounds.slotMap (PolarCharts.chart a chart) (ChartScales.timeCoefficient h (↑I.1).1) (f.carrier k I.1).center r0 (PhysicalGraphBounds.physicalLift h (↑I.1).1 z)).1 ∈ self.region k I.1
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Lower weighted coefficient classes and actual phase jets supply all inputs of the physical theorem; no physical derivative estimate is assumed.
All actual physical jets of the full copy and label sum, from the lower weighted class. Slow polynomial degrees and copy count do not enter the derivative-loss function.
Literal native cells and their lattice centers #
Native center, given by g.center + TorusAverages.latticePoint k.
Equations
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The center used by a copy is its own lattice translate.
The physical slot-width bound follows from the native cell width and the exact cover map, rather than being assumed for a periodized field.
Build the abstract support cells from the actual native affine lattice
charts. Compactness gives local finiteness; quotient injectivity gives
disjointness, both through PeriodizedWaveBounds.nativeCells.
Equations
- One or more equations did not get rendered due to their size.
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For the actual localized coefficients, the support premise is itself derived from the literal cutoff factor.
Equations
- NavierStokes.PhysicalCopyBounds.nativeCutoffSupportCells g U hU hinj κ hκ v he = NavierStokes.PhysicalCopyBounds.nativeSupportCells g U hU hinj ⋯
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A native cell description proves all copy-width support conditions in the regularity record. The radial annulus, slow mask, and smooth coefficient inputs are separate, as in the original construction.
Exact support and vector-valued consequences #
A nonzero full sum has a genuine supported copy witness. This is the primitive support statement needed for the shrinking physical annulus.
Vector sum, given by ∑ i : Fin 3, realCoordinate i ((f i).sum a h r0 w).
Equations
- NavierStokes.PhysicalCopyBounds.vectorSum f a h r0 w = ∑ i : Fin 3, (NavierStokes.PhysicalWaveSum.realCoordinate i) ((f i).sum a h r0 w)
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Uniform scalar input bounds give the actual real three-component physical estimate with the same loss exponent.