Uniform weighted coefficients and physical wave sums #
The constants below are selected before the label and the band. The first
step absorbs the actual two flat edges, including every inverse-edge power.
Global smoothness and support then extend the estimate across the boundary.
The final passage uses genuine common-coordinate compositions and the
physical carrier estimates of PhysicalWaveSum.
Explicit fixed flat-edge geometry, pulled back through any radial coordinate. This is an equality of the weights, not a bound on them.
- delta_eq (x : D) : x ∈ s.domain → s.delta x = WeightedRadialPrimitive.delta L (ρ x)
- zeta_eq (x : D) : x ∈ s.domain → s.zeta x = WeightedRadialPrimitive.zeta cL cR L (ρ x)
Instances For
Remove the edge growth from an actual uniform coefficient class. The input envelope may depend on the label and band; its domination is uniform.
The support boundary is included by continuity of the actual jets. Outside it all jets vanish, because there is an actual zero neighborhood.
Conversion to physical band powers is exact; no exponent is lost when the two flat edges are removed.
Primitive input for the physical bridge. In particular, uniform
places its constants before the label, and support concerns the actual
coefficient, not a prescribed bound for its derivatives.
- uniform : LabelSumBounds.UniformClass s w α f
- flat_geometry : ∃ (cL : ℝ) (cR : ℝ) (L : ℝ) (ρ : D → ℝ), FlatGeometry s cL cR L ρ
Instances For
A local form of the genuine higher chain-rule estimate. Only positive derivatives of the coordinate map are needed; the map's values may be unbounded.
The common-chart identity for actual amplitudes. This records only the source formula and the coordinate map's jets, before any physical graph or carrier has been differentiated.
- sourceIndex : PhysicalWaveSum.WaveIndex H → ι
Source index of
CommonChart, of typePhysicalWaveSum.WaveIndex H → ι. - map : PhysicalWaveSum.WaveIndex H → PhysicalWaveSum.LiftPoint → D
Map from a lifted point in each wave chart to the common physical domain.
- domain : PhysicalWaveSum.WaveIndex H → Set PhysicalWaveSum.LiftPoint
Domain of
CommonChart, of typePhysicalWaveSum.WaveIndex H → Set PhysicalWaveSum.LiftPoint. - open_domain (I : PhysicalWaveSum.WaveIndex H) : IsOpen (self.domain I)
- smooth (I : PhysicalWaveSum.WaveIndex H) : ContDiffOn ℝ (↑⊤) (self.map I) (self.domain I)
- amplitude_eq (I : PhysicalWaveSum.WaveIndex H) : F.amplitude I = fun (x : PhysicalWaveSum.LiftPoint) => ChartScales.Q (↑I.1).1 ^ σ • f (self.sourceIndex I) (↑I.1).1 (self.map I x)
- contains (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 ∈ self.domain I
Instances For
Actual composition and the explicit band prefactor produce the
stripped amplitude estimate. Its exponent is h*α+σ, and its constants
are independent of the label.
The natural slow scale for a band label is at least one because the physical sum starts at band four.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Polynomial jets of the actual two base profiles entering the phase, on open slow-coordinate regions containing every relevant chart point.
- region : PhysicalWaveSum.BandLabel → Set PhysicalGraphBounds.Slow
Region of
CarrierBounds, of typePhysicalWaveSum.BandLabel → Set PhysicalGraphBounds.Slow. - open_region (L : PhysicalWaveSum.BandLabel) : IsOpen (self.region L)
- jets : PhaseJetBounds.PolynomialJets (bandDomain self.region ⋯) fun (L : PhysicalWaveSum.BandLabel) (x : PhysicalGraphBounds.Slow) => ((F.carrier L).F x, (F.carrier L).G x)
- contains (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 → ∀ (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 I.1).center r0 (PhysicalGraphBounds.physicalLift h (↑I.1).1 z)).1 ∈ self.region I.1
Instances For
The full StrippedClass is derived from the uniform weighted source,
the primitive common-chart identity, and the actual base-profile jets.
The derivative loss includes the displayed physical field rescaling. It depends on the derivative order and fixed scaling parameters only.
Equations
Instances For
Full physical jets of the actual locally finite wave sum. The derivative-loss function does not depend on the harmonic cutoff, cover gap, label, slow polynomial degrees, or correction stage.
Taking the real part, as for the physical pressure, loses no constant.
Inclusion of a spatial direction into a joint spacetime direction.
Equations
Instances For
A fixed continuous linear map takes the spatial curl from a joint Jacobian. Its norm is independent of every band and correction stage.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Taking the actual spatial curl costs exactly one joint derivative and a fixed linear-operator norm.
The actual Cartesian-to-cylindrical coefficient map #
Cylindrical point: an abbreviation for ℝ × ((ℝ × ℝ) × PhysicalGraphBounds.Plane).
Equations
Instances For
Cartesian radius, given by Real.sqrt (y.1 ^ 2 + y.2 ^ 2).
Instances For
Slow order (T,Z) and the actual common auxiliary coordinate.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Cylindrical map, given by (cartesianRadius (PhysicalGraphBounds.liftXY x), slowFast x).
Equations
Instances For
Cylindrical domain, given by (fun x => ‖PhysicalGraphBounds.liftXY x‖) ⁻¹' Ioo (a / 2) (b + 1).
Equations
- NavierStokes.PhysicalClassBounds.cylindricalDomain a b = (fun (x : NavierStokes.PhysicalWaveSum.LiftPoint) => ‖NavierStokes.PhysicalGraphBounds.liftXY x‖) ⁻¹' Set.Ioo (a / 2) (b + 1)
Instances For
All positive jets of the actual radius map are uniformly bounded on a fixed padded annulus, regardless of slow or auxiliary coordinates.
The actual common graph has the expected cylindrical radius, scaled slow variables, and inverse-covered auxiliary coordinate.
Direct adapter for a genuine cylindrical coefficient. No coordinate derivative estimate is assumed: the preceding theorems prove it.
Equations
- One or more equations did not get rendered due to their size.