The actual similarity-dependent mean gauge #
The endpoints are multiplied by the actual sqrt(q). The cutoff and
normalized density are defined explicitly, and the primitive is the existing
integral operator evaluated with those endpoints on each slow fiber.
The estimates use the moving profile R / sqrt(q) and the full ordinary
Fréchet derivatives. Their constants are uniform in the source family and
the radial transport frequency. The exact cutoff alias is retained.
The final State theorems derive pressure, pressure-change and temporal increment classes from the actual input fields on the valid slow domain. The common torus index and its bounded gap from the native index remain explicit. This module does not assert arbitrary-power alias decay.
Radial ratio, given by z.1 / ell z.2.1.
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- NavierStokes.VariableGaugeMean.radialRatio ell z = z.1 / ell z.2.1
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Cutoff, given by RadialPullback.physicalCutoff d a b (radialRatio ell z).
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Density, given by (ell z.2.1)⁻¹ * PressureStream.rho a b hab (radialRatio ell z).
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- NavierStokes.VariableGaugeMean.density a b hab ell z = (ell z.2.1)⁻¹ * NavierStokes.PressureStream.rho a b hab (NavierStokes.VariableGaugeMean.radialRatio ell z)
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Supported gauge, given by ∀ z, z.2.1 ∈ U → f z ≠ 0 → z.1 ∈ Icc (ell z.2.1 * a) (ell z.2.1 * b).
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- NavierStokes.VariableGaugeMean.SupportedGauge a b ell U f = ∀ (z : NavierStokes.PressureStream.Lift S), z.2.1 ∈ U → f z ≠ 0 → z.1 ∈ Set.Icc (ell z.2.1 * a) (ell z.2.1 * b)
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Genuine integral with the actual endpoints on this slow fiber.
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- NavierStokes.VariableGaugeMean.compactPrimitive d a b M ell v f z = NavierStokes.RadialPullback.physicalCompact d (ell z.2.1 * a) (ell z.2.1 * b) M (0, v) f z
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Pressure source, given by f z - density a b hab ell z * PressureStream.pressureMass f z.2.1.
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- NavierStokes.VariableGaugeMean.pressureSource a b hab ell f z = f z - NavierStokes.VariableGaugeMean.density a b hab ell z * NavierStokes.PressureStream.pressureMass f z.2.1
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Mean pressure, given by compactPrimitive d a b M ell v (pressureSource a b hab ell f).
Equations
- NavierStokes.VariableGaugeMean.meanPressure d a b M hab ell v f = NavierStokes.VariableGaugeMean.compactPrimitive d a b M ell v (NavierStokes.VariableGaugeMean.pressureSource a b hab ell f)
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Stream potential, given by PressureStream.divideRadius (compactPrimitive d a b M ell v (PressureStream.weightedSource f)).
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Compact alias, given by RadialPullback.physicalAlias d (ell z.2.1 * a) (ell z.2.1 * b) M ((0 : S), v) f z.
Equations
- NavierStokes.VariableGaugeMean.compactAlias d a b M ell v f z = NavierStokes.RadialPullback.physicalAlias d (ell z.2.1 * a) (ell z.2.1 * b) M (0, v) f z
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Slow variables in this module follow the rank/domain convention (T,Z).
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Cutoff model, given by RadialPullback.physicalCutoff d a b (y.2.1 / Real.sqrt y.1).
Equations
- NavierStokes.VariableGaugeMean.cutoffModel d a b y = NavierStokes.RadialPullback.physicalCutoff d a b (y.2.1 / √y.1)
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Density model, given by (Real.sqrt y.1)⁻¹ * PressureStream.rho a b hab (y.2.1 / Real.sqrt y.1).
Equations
- NavierStokes.VariableGaugeMean.densityModel a b hab y = (√y.1)⁻¹ * NavierStokes.PressureStream.rho a b hab (y.2.1 / √y.1)
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All joint cutoff jets, including actual derivatives of q, are derived
from the inverse-coordinate jet theorem on its compact model box.
Physical past, constructed using TransportPrimitive.pastIntegral.
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Changing the auxiliary regularization radius leaves the actual primitive unchanged; only the compactification cutoff remains.
The integration and physical radial pullback cost is uniform in the transport frequency. Every input and output derivative is an actual joint jet.
The actual similarity gauge in every normalized chart.
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Reconstruct state as an element of CorrectionState.State (PressureStream.Lift S).
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Pressure alias state as an element of CorrectionState.Oscillation (PressureStream.Lift S).
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Temporal potential, constructed using streamPotential.
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Temporal increment state, bundling radial, angular, axial.
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Temporal axial difference, constructed using MeanChartCompatibility.temporalAtIndex.
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Temporal alias state, defined pointwise by ![0, 0, -c.operators.fastTime (temporalAxialDifference g h index c u) n p.1].
Equations
- NavierStokes.VariableGaugeMean.temporalAliasState g h index c u n p = ![0, 0, -c.operators.fastTime (NavierStokes.VariableGaugeMean.temporalAxialDifference g h index c u) n p.1]
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Temporal stage state, given by reconstructState g c (u.addIncrement (temporalIncrementState g h index axial c u) 0 0 0 ⟨0, 0, temporalAliasState g h index c u⟩).
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Rank potential, constructed using streamPotential.
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Rank increment state, bundling radial, angular, axial.
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Rank stage state, given by reconstructState g c (u.addIncrement (rankIncrementState g r axial c u) 0 0 0 CorrectionState.ExcludedErrors.zero).
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Naturality on a single genuine slow fiber. The source is only required to be smooth and periodic on its open physical slow domain.
Full Leibniz control with an explicit cutoff-jet bound. The integration constant is chosen before the domain, scale function, frequency and source.
The same physical change, in the rank/domain order (T,Z).
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Swap slow as an element of PressureStream.Lift Plane →L[ℝ] PressureStream.Lift Plane.
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Physical to chart TZ, given by chartLinear (chartScale n) ((slowToChartTZ h n).prodMap (TemporalMeanUpdate.coverMap i)).
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Field on physical TZ, given by coverPull (chartScale n) (slowToChartTZ h n) i (ChartScales.Q n ^ (-a)) f.
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The actual variable-gauge chart pressures are the same physical operator, with the exact pressure and momentum units.
The fixed normalization map has uniform weighted jet bounds when the weight is read on any admissible dilated radial fiber.
Normalized cutoff, given by TransportPrimitive.interiorCutoff a b (radialRatio ell z).
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Transport gauge, constructed using TransportPrimitive.pastIntegral.
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No derivative is taken after the scalar change of integration variable. The estimate uses the original full joint derivatives under the fixed-u integral.
A fixed containing shell is used only to normalize the integral. The weight and the actual cutoff continue to use the moving profile endpoints.
Normalized cutoff model, given by TransportPrimitive.interiorCutoff (a ^ d) (b ^ d) (y.2.1 / (Real.sqrt y.1) ^ d).
Equations
- NavierStokes.VariableGaugeMean.normalizedCutoffModel d a b y = NavierStokes.TransportPrimitive.interiorCutoff (a ^ d) (b ^ d) (y.2.1 / √y.1 ^ d)
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Uniform finite seminorm inequality for the actual q-gauge primitive. The constant precedes all frequencies, sources, amplitudes and evaluation points.
Cutoff radial derivative, given by (ell z.2.1)⁻¹ * deriv (physicalCutoff d a b) (radialRatio ell z).
Equations
- NavierStokes.VariableGaugeMean.cutoffRadialDerivative d a b ell z = (ell z.2.1)⁻¹ * deriv (NavierStokes.RadialPullback.physicalCutoff d a b) (NavierStokes.VariableGaugeMean.radialRatio ell z)
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Cutoff radial derivative model, given by (Real.sqrt y.1)⁻¹ * deriv (physicalCutoff d a b) (y.2.1 / Real.sqrt y.1).
Equations
- NavierStokes.VariableGaugeMean.cutoffRadialDerivativeModel d a b y = (√y.1)⁻¹ * deriv (NavierStokes.RadialPullback.physicalCutoff d a b) (y.2.1 / √y.1)