Physical jets of coherent mean fields #
The graph below is the actual common-cover cylindrical graph, with slow order
(T,Z). It is identified with VariableGaugeMean.physicalToChartTZ, and its
derivative estimates are derived from the actual physical graph and radius map.
The final restriction is a single coherent physical field, not a sum over bands.
Point: an abbreviation for PressureStream.Lift PhysicalGraphBounds.Plane.
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The unscaled physical cylindrical point with the actual auxiliary graph.
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A bounded-gap common-cover graph, in the mean-field coordinate order.
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Exact identification with the variable-gauge mean chart. The cover index is the native index minus the actual common-cover gap.
Selection of a comparable dyadic band #
Every sufficiently small positive physical scale has a comparable band above any prescribed cutoff. No summation over bands is introduced.
The local, nonoscillatory graph estimate #
Band field, defined pointwise by (ChartScales.Q n ^ (-degree)) • f (graph h n d w).
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- NavierStokes.PhysicalMeanJetBounds.bandField h n d degree f w = NavierStokes.ChartScales.Q n ^ (-degree) • f (NavierStokes.PhysicalMeanJetBounds.graph h n d w)
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Loss, given by PhysicalGraphBounds.graphLoss m + 1 + degree.
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- NavierStokes.PhysicalMeanJetBounds.loss degree m = NavierStokes.PhysicalGraphBounds.graphLoss m + 1 + degree
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Actual cylindrical mean-field restriction. Both graph stages are differentiated using their proved jet bounds. Raw input smoothness is local.
The actual normalized slow coordinate #
One physical field represented in all valid bands #
Exact chart coherence for the same physical lifted field. The data do not define a sum of band fields and contain no physical derivative estimate.
Native of
CoherentFamily, of typeℕ → Point → E.- physical : Point → E
Physical of
CoherentFamily, of typePoint → E. Gap of
CoherentFamily, of typeℕ → ℕ.- gap_native (n : ℕ) : n ≥ N → self.gap n ≤ ChartScales.nativeIndex h n
- coherent (n : ℕ) : n ≥ N → ∀ (z : Point), 0 < z.2.1.1 → ((VariableGaugeMean.physicalToChartTZ h n (ChartScales.nativeIndex h n - self.gap n)) z).2.1 ∈ U → self.physical z = ChartScales.Q n ^ (-degree) • self.native n ((VariableGaugeMean.physicalToChartTZ h n (ChartScales.nativeIndex h n - self.gap n)) z)
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Field, given by D.physical ∘ physicalPoint h.
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Supported native coefficients, stated for an arbitrary normed target.
For real-valued coefficients this is the actual SupportedGauge condition.
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Native moving-annulus support gives a fixed Cartesian chart annulus at every supported physical point with a comparable band.
Band-independent native jets after absorbing the actual flat weight.
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A uniform estimate for the same coherent physical field. A comparable band is selected at each point and used through an exact field germ.
The local mean-class consumer #
Incoming local band jets of any real class exponent give physical Cartesian jets of that same coherent field.
The open physical region on which the local native hypotheses imply smoothness, including the zero neighborhood at the spatial axis.
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The actual Cartesian angular frame #
The Cartesian unit angular direction, with the usual totalized value at the axis. Axis regularity below comes from the supported coefficient.
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A local Leibniz estimate for scalar multiplication, including order zero. It uses actual Fréchet tensors on the supplied open set.
The angular frame has uniform jets on the fixed padded annulus. No slow or auxiliary coordinate enters these constants.
This is the direct angular vector when degree = A h, and the
azimuthal stream potential when degree = A h - 1/2.
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The actual angular direction is incorporated before estimating the physical graph. Thus it incurs no additional power loss.
The actual Cartesian vector associated with the coherent scalar field. The formula applies both to angular velocity and stream potential.
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The actual spatial curl of the azimuthal stream potential. Its fixed physical loss uses one more derivative; no derivative is postulated.
Genuine moving-weight mean classes #
The existing moving two-edge mean class supplies the native input jets. The only extra regularity is the genuine supported extension across the edges, on the valid slow region.
Coherence of the actual reconstructed pressure and stream #
Reconstruct the physical pressure from the coherent momentum source. The output coherence is proved from the actual integral operator; it is not an additional premise.
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Reconstruct the azimuthal stream potential from a coherent axial
source. Its physical degree is exactly A h - 1/2.
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