A physical signed request on its moving radial shell #
The profile coordinate is R / sqrt(q). Its pullback retains the same flat
edge weight as the primary field. All slow hypotheses are local; in
particular no positive or bounded extension of q to the entire plane is
assumed.
Mean reconstruction on an open slow domain #
Radial transport and torus integration preserve the slow parameter. The
operators in this file are the actual operators from PressureStream and
TemporalMeanUpdate, restricted to an open slow domain. Cutoffs are used only
to prove local smoothness and equality of germs; none of their derivatives
enters the uniform estimates.
All radii and torus variables, with only the slow parameter restricted.
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Strip domain, given by {p | p.1 ∈ Ioo a b ∧ p.2.1 ∈ U}.
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Restriction changes only the domain, leaving all weights and band scales.
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Radial support is required only at slow parameters where the source is used.
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- NavierStokes.PhysicalMeanDomain.SupportedOn a b U f = ∀ (p : NavierStokes.PressureStream.Lift S), p.2.1 ∈ U → f p ≠ 0 → p.1 ∈ Set.Icc a b
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Periodic on, given by ∀ r s, s ∈ U → FourierAlias.TorusPeriodic (fun Y => f (r, (s, Y))).
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- NavierStokes.PhysicalMeanDomain.PeriodicOn U f = ∀ (r : ℝ), ∀ s ∈ U, NavierStokes.FourierAlias.TorusPeriodic fun (Y : NavierStokes.TorusInverse.Plane) => f (r, s, Y)
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The germ of a source on one entire slow fiber, including a slow neighborhood.
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An auxiliary localization, used only for germs.
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- NavierStokes.PhysicalMeanDomain.localize c f p = c p.2.1 • f p
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Freezing the slow parameter never changes a radial transport integral on that fiber. It does not freeze any jet appearing in the integrand.
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Weighted estimates on one slow fiber #
The complete physical inverse preserves the original exponential weight and the same finite inverse-edge degree. All constants precede the arbitrary transport shift, source, amplitude, and evaluation point.
The actual operators preserve slow fibers and their germs #
Fiber local, given by ∀ (f g : PressureStream.Lift S → V) (s : S), (∀ r Y, f (r, (s, Y)) = g (r, (s, Y))) → ∀ r Y, T f (r, (s, Y)) = T g (r, (s, Y)).
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A proved fiber-local operator transfers its global smoothness theorem to local input data. No global extension is an input to this theorem.
Compact integration needs local domination only, not a bound on all parameters. This identity differentiates the literal affine average.
Uniform band jets on the valid slow domain, including all radial edges.
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Local slow strip data as an element of StripData S.
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The local pressure is the same linear integral operator used globally.
Exact identification of the positive-time normalized rank domain #
Normalized slow domain, given by {s | 0 < s.1 ∧ SimilarityCoordinates.coordinateQ coord (s.1, s.2) ∈ Ioo qlo qhi}.
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A bounded source gives a bounded actual cutoff alias, with a constant independent of the transport shift and the slow fiber.
The actual divided alias preserves the local mean class. No mean-zero condition or nonzero transport coefficient is needed for this basic bound.
The exact pullback of the weights, with a local domain for the map.
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Positive jets, rather than the value of an unbounded auxiliary coordinate, are what the composition estimate uses.
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A genuine open positive-time region with bounds on the actual normalized similarity coordinate. Its endpoints and constants are independent of bands.
Carrier of
SlowRegion, of typeSet Plane.- qlo : ℝ
Qlo of
SlowRegion, of typeℝ. - qhi : ℝ
Qhi of
SlowRegion, of typeℝ.
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Profile map, given by (x.1 / Real.sqrt (MeanRankUpdate.chartQ coord x), x.2).
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- NavierStokes.LocalSignedRequest.profileMap coord x = (x.1 / √(NavierStokes.MeanRankUpdate.chartQ coord x), x.2)
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Inverse profile map, given by (Real.sqrt (MeanRankUpdate.chartQ coord x) * x.1, x.2).
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- NavierStokes.LocalSignedRequest.inverseProfileMap coord x = (√(NavierStokes.MeanRankUpdate.chartQ coord x) * x.1, x.2)
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Moving strip data, constructed using localPullbackStrip.
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The actual compact transport primitive preserves the radial flat weight on an arbitrary open slow domain. The cutoff is the supplied fixed cutoff.
The physical signed primitive, in the actual moving weight, costs no power of epsilon. The only constants come from the fixed profile and the bounded normalized slow region.
Both components are computed from the same actual state.
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Normalized request, defined pointwise by (s.epsilon n)⁻¹ • requestedStress P coord c u n x.
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- NavierStokes.LocalSignedRequest.normalizedRequest s P coord c u n x = (s.epsilon n)⁻¹ • NavierStokes.LocalSignedRequest.requestedStress P coord c u n x
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Genuine pullback to the full coefficient domain, including the angle.
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- NavierStokes.LocalSignedRequest.fullRequest s P coord c u n x = NavierStokes.LocalSignedRequest.normalizedRequest s P coord c u n x.1
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Physical radial scaling changes a primitive by exactly one length factor.
One physical request has all chart views. Only the target slow fiber needs regularity and periodicity.
This field has no band index: every normalized request below represents this same physical signed stress.
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Exact Q-normalization of one physical primitive. The hypotheses refer to the actual represented source, not to the desired stress or its bounds.
A measured moment equal to epsilon times a slow derivative yields the extra epsilon in the actual removed physical bump, in the same moving weight.