Naturality of the actual mean operators #
Radial endpoints, the normalized density, the compactification cutoff, frequencies, and amplitudes are transported together. The identities below are identities of the defined integral/Fourier/rank operators, not an assumption that separately chosen chart outputs coincide.
The density transforms with the inverse radial length.
Chart linear, given by (l • ContinuousLinearMap.id ℝ ℝ).prodMap C.
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Pull, given by u * f (chartLinear l C z).
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- NavierStokes.MeanChartCompatibility.pull l C u f z = u * f ((NavierStokes.MeanChartCompatibility.chartLinear l C) z)
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Scaling of the actual compact radial integral, with transformed endpoints and the exact transformed transport direction.
The stream potential has one less velocity length factor.
Parameter pull, given by pull l (P.prodMap (ContinuousLinearMap.id ℝ Plane)) u f.
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Cover pull, given by pull l (P.prodMap (TemporalMeanUpdate.coverMap k)) u f.
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Naturality of the actual pressure formula, including its normalized mass correction and compactification, on a common covering.
The physical temporal update is one fixed Fourier operator. The native cover factor and the momentum/velocity unit factors cancel exactly.
The common-index form of the actual temporal update. A common index is independent of the dyadic band; the native recipe is its specialization.
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Physical temporal, given by -TemporalMeanUpdate.temporalInverse (TemporalMeanUpdate.centered f) z.
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All common indices give the same physical temporal operator after the actual velocity and momentum normalizations.
Naturality of the constructed five-row inverse, not just of its rows.
Common ratio, given by ChartScales.Tg ^ ChartScales.nativeIndex h n / ChartScales.Tg ^ i.
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Fast at index, given by (ChartScales.Tg ^ i * ChartScales.Q n ^ (1 + h)) * PressureStream.graphDz ((0 : S), vector .temporal) f z.
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Radial frequency, given by M * ChartScales.Lambda ^ i * ChartScales.Q n ^ (d / 2).
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- NavierStokes.MeanChartCompatibility.radialFrequency _h n i d M = M * NavierStokes.ChartScales.Lambda ^ i * NavierStokes.ChartScales.Q n ^ (d / 2)
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The physical slow variables are (z,τ) with τ=1-t.
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Physical to chart, given by chartLinear (chartScale n) ((slowToChart h n).prodMap (TemporalMeanUpdate.coverMap i)).
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Normalize a chart field of scaling degree a on the actual physical
slow variables and absolute auxiliary lift.
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A chart-specific instance of the existing reconstruction recipe. The physical endpoints and frequency are transported, rather than copied.
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The normalized chart pressure is exactly one physical pressure operator applied to the normalized radial source.
Reconstruct pressure family, given by { u with pressure := fun n => (CorrectionState.reconstructPressure (r n) c u).pressure n }.
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If the normalized sources are one physical source, the recomputed pressures are representations of its single, defined physical pressure. Compatibility of the output is the conclusion, not an input.
The axial alias itself transforms as a velocity. It is retained as the exact compactification term.
The potential uses the explicitly chosen common torus index.
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Common temporal fields, bundling radial, angular, axial.
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Common temporal alias, constructed using PressureStream.divideRadius.
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Common temporal increment, given by commonTemporalFields r h index c.operators.epsilon axial (u.thetaResidual c) (u.axialResidual c).
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Physical auxiliary, given by (slowToChart h n).prodMap (TemporalMeanUpdate.coverMap i).
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Axial unit, given by ((1, 0), (0, 0)).
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One physical vector field, constructed from the two physical sources.
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The three defined chart components are restrictions of one physical vector field. The source identities are the only compatibility premises.
Source moment, given by PressureStream.pressureMass (fun z => z.1 ^ m * f z) s.
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- NavierStokes.MeanChartCompatibility.sourceMoment m f s = NavierStokes.PressureStream.pressureMass (fun (z : NavierStokes.PressureStream.Lift S) => z.1 ^ m * f z) s
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Source debt, given by ![sourceMoment 0 g s, sourceMoment 2 qθ s, sourceMoment 1 qz s - (1 / 2 : ℝ) * sourceMoment 2 g s].
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The radial source carries one additional inverse-length factor. The actual three integrated debts then have the required different length powers.
Naturality with slow-dependent length, velocity, amplitude and debt. Only the primitive input data are transported.
Slow projection, given by (z.1, z.2.1).
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Every function of the true profile coordinates (X,η) is invariant,
including the radial profile weight and its logarithmic edge distance.
The slow similarity length itself scales; it is not a fixed radial endpoint shared by all normalized band charts.