Literal physical data for the actual candidate #
The initial fields use the same primary choice and the same initialized
mean state as ActualCandidateConstruction. Their support, smoothness,
and axis germs are derived from those constructors.
The same initialized correction sequence and its physical prefixes #
Every state below comes from the actual initialized primary choice and the fixed actual cycle parameters. The finite labels, phase carriers, base error, and current pressure alias are retained through the literal recurrence.
Point: an abbreviation for CorrectionStep.CyclePoint.
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Parameters, given by ActualCycleParameters.fixedParameters B N0.
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Parameter sequence, defined pointwise by parameters B N0.
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Cycle, given by CycleState.iterate (parameterSequence B N0) (commonContext B) (ActualInitialization.initialCycleState B N0).
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Recomputing the actual constructor at this state selects precisely the fixed parameters used by the recurrence.
Initial temporal alias, constructed using VariableGaugeMean.temporalAliasState.
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Temporal alias, given by CycleStateCoherence.temporalAliasAt (parameterSequence B N0) (commonContext B) (ActualInitialization.initialCycleState B N0) j.
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Every earlier temporal alias and exactly the current pressure alias remain present, with the signs inherited from the actual state updates.
One positive band floor is retained for every physical stage.
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One extra comparison band keeps every native point with q/Q < 2
inside the original raw field's validity domain.
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Physical domain, given by CutStageEstimates.physicalSublevel h (qbig B N0).
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One selected initialization #
Selected budget, given by 0.
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Selected threshold, given by ActualCarrierGeometry.startingThreshold 0.
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Selected cycle, given by cycle selectedBudget selectedThreshold.
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Selected qbig, given by qbig selectedBudget selectedThreshold.
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Exact finite physical prefixes in any valid polar chart #
Graph, given by PhysicalResidualBridge.commonGraph (ChartScales.Q n) h (CorrectionInitialization.CommonWindow.index h n).
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Base pressure, given by ActualBaseResidual.basePressure certificate modulation upper B n.
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Chart velocity, given by CyclePhysicalPrefixes.velocity a i (graph n) n (commonContext B) (cycle B N0 j).state.
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Chart pressure, given by CyclePhysicalPrefixes.pressure a i (graph n) n (basePressure B n) (cycle B N0 j).state.
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Chart velocity stages, constructed using CyclePhysicalPrefixes.velocityStages.
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Chart pressure stages, constructed using CyclePhysicalPrefixes.pressureStages.
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Chart potential parts, constructed using CyclePhysicalPrefixes.potentialParts.
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Chart direct stages, constructed using CyclePhysicalPrefixes.directStages.
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The global physical representatives need only agree with an individual chart on its open validity set. Finite summation and the genuine residual preserve precisely this local agreement.
The actual mean fields, with one common physical representative #
The selector defining this atlas depends on the physical point and the fixed validity strip. It is independent of the scalar being represented. Consequently sums and differences retain the original absolute mean and pressure; no new integration constant or choice enters a later stage.
Mean atlas, given by ActualMeanPhysicalData.initialAtlas (firstBand B N0).
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Mean field, given by (meanAtlas B N0).physical standardRegion.carrier degree f ∘ PhysicalMeanJetBounds.physicalPoint h.
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Mean angular field, defined pointwise by meanField B N0 degree f w • PhysicalMeanJetBounds.angularVector (PhysicalGraphBounds.radialProjection w).
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Angular native stages as an element of ℕ → ActualMeanPhysicalData.Scalar.
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Pressure native stages, defined pointwise by Nat.casesOn k (cycle B N0 0).state.pressure (fun j => (cycle B N0 (j + 1)).state.pressure - (cycle B N0 j).state.pressure).
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Angular mean stages, defined pointwise by meanAngularField B N0 (CoordinateAlgebra.A h) (angularNativeStages B N0 j).
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Pressure mean stages, defined pointwise by meanField B N0 (2 * CoordinateAlgebra.A h) (pressureNativeStages B N0 j).
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Temporal native, constructed using VariableGaugeMean.temporalPotential.
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Rank native, constructed using VariableGaugeMean.rankPotential.
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Stream native stages as an element of ℕ → ActualMeanPhysicalData.Scalar.
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Stream mean stages, defined pointwise by meanAngularField B N0 (CoordinateAlgebra.A h - 1 / 2) (streamNativeStages B N0 j).
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Chart mean pressure parts, constructed using CyclePhysicalPrefixes.polarPressureMap.
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Chart stream parts as an element of ℕ → VelocityField.
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Chart base velocity, constructed using CyclePhysicalPrefixes.polarVelocityMap.
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Chart base pressure, given by CyclePhysicalPrefixes.polarPressureMap a i (CyclePhysicalPrefixes.pressureMap (graph n) (basePressure B n)).
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Chart wave parts as an element of ℕ → VelocityField.
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Chart wave pressure parts as an element of ℕ → PressureField.
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The fixed physical base in the same chart #
Both normalizations below are computed from the actual graph map. In particular the pressure factor is the square of the velocity factor.
Constructed direct angular and mean-stream stage data #
Direct data as an element of ℕ → DirectAngularDiagonal.AngularData (LocalAngularDiagonal.localSlowDomain h (qbig B N0)).
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Stream data as an element of ℕ → DirectAngularDiagonal.AngularData (LocalAngularDiagonal.localSlowDomain h (qbig B N0)).
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Mean stream support, given by MixedAxisPreservation.AngularSupport.ofAngularData (streamData H j) (fun _ hw => hw).
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The stage constructors retain the actual copy data. The wave producers supply these records; the mean field is fixed by the same cycle above.
Initial potential stage, bundling waveCount, waves, streamCount, streams.
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Positive potential stage, bundling waveCount, waves, streamCount, streams.
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Endpoint inputs for the actual raw candidate stages #
Positive stages use their already proved raw estimates. Stage zero uses the actual initial mean families and the existing extensions of the same base potential and pressure. No output extension is an input below.
The three off-plane endpoint obligations of candidate_of_finite_stages.
This is an output package; the construction below does not assume its fields.
- potential (x : ProblemStatement.Space) : x.ofLp 2 ≠ 0 → EndpointCoordinates.endpointRoot (2 * h) (x.ofLp 2) < qbig → ∀ (j : ℕ), Nonempty (JointResidualLimits.OneSidedExtension (A j) x)
- direct (x : ProblemStatement.Space) : x.ofLp 2 ≠ 0 → EndpointCoordinates.endpointRoot (2 * h) (x.ofLp 2) < qbig → ∀ (j : ℕ), Nonempty (JointResidualLimits.OneSidedExtension (V j) x)
- pressure (x : ProblemStatement.Space) : x.ofLp 2 ≠ 0 → EndpointCoordinates.endpointRoot (2 * h) (x.ofLp 2) < qbig → ∀ (j : ℕ), Nonempty (JointResidualLimits.OneSidedExtension (P j) x)
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The exact base and bounded finite initial potential correction.
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Initial direct model, given by (ActualMeanPhysicalData.initialAngularFamily B N0 N).angularField.
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The pressure of the same summed base and the actual finite initial wave and mean-pressure correction.
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The physical bounds and exact initial representations supply all three endpoint inputs, including index zero. No extension or endpoint limit is assumed for any raw stage.
Application to the literal raw families expected by
MixedCandidateAssembly.candidate_of_finite_stages. The remaining
equalities identify the produced physical fields, not their endpoint jets.
The chosen direct angular constructor supplies its stage-zero representation by its proved global field identity.
Direct application to the fixed actual run. Native wave and mean data
and their exact physical representations already imply the endpoint
inputs; no finite-residual estimate or completed StageEstimates record
is required for this conclusion.
Endpoint inputs for physical fields assembled by germs #
The potential increments may be literal glued physical fields. Only their interior smoothness and actual derivative estimates enter the extension argument; a representation by a fixed-reference copy family is unnecessary. The zeroth potential and pressure retain the separately extended slow base.
Interior data for one actual physical field. The exponent and logarithmic loss may depend on the derivative order and on the field. In particular this record neither assumes an endpoint limit nor compares different stages.
- smooth : ContDiffOn ℝ (↑⊤) f (CutStageEstimates.physicalSublevel h qbig)
- bound (m : ℕ) : ∃ (C : ℝ) (p : ℝ) (e : ℝ), ∀ w ∈ CutStageEstimates.physicalSublevel h qbig, |w.1| ≤ 1 → PhysicalWaveSum.physicalQ h w ≤ 1 → ‖iteratedFDeriv ℝ m f w‖ ≤ C * (1 + |Real.log (PhysicalWaveSum.physicalQ h w)|) ^ p * PhysicalWaveSum.physicalQ h w ^ e
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Adapter for the power bounds of the current-band physical construction. The time restriction is kept, as in the physical wave estimate.
The positive-index restriction in RawStageBounds is preserved.
A smaller scale cap preserves the same constants.
Physical identities on the open validity region identify every actual ordinary jet. Values at a chart face or beyond the region are irrelevant.
Finite sums retain derivative bounds without identifying a summand with any copy-family construction.
This is an application of the existing local bounded-jet extension theorem. No new boundary regularity hypothesis is introduced.
The actual mean-pressure native bounds supply the single-field input.
This applies to both actual mean-stream potentials and the direct angular increments, with their own physical degree and their original first band.
Existing initial or signed wave data can be used for those summands. No such data are requested for the glued particular summand.
The finite potential correction at index zero uses the actual initial wave, temporal mean, and rank mean. The slow-base gauge is excluded here.
The finite initial pressure correction retains the actual initial wave pressure and the pressure mean.
A finite physical sum can be extended directly from estimates of its actual summands. Equality is required only on the physical validity region.
Bounds for literal raw fields imply all three candidate endpoint inputs. The base gauge is never subjected to a growth assumption, and the positive stage estimate is never applied to index zero.
Literal fields accepted by GermCandidateAssembly. In particular
stages j may be a glued current-particular field plus signed and mean
corrections; there is no copy-family or potential-stage argument.
Once the finite-stage estimates have been derived, only the bounded finite initial pieces remain to be supplied. This wrapper does not inspect or impose a representation of any positive physical stage.
The chosen initial potential supplies its own native wave data. The consumer does not have to provide or postulate such a witness.
The same-choice mixed raw sequence has all endpoint inputs. Positive fields are arbitrary physical fields, including the genuine glued particular fields. Only their derived interior jet estimates are used. Initialization is bound to the actual initial wave and actual mean families by local field identities, with no supplied wave-data or endpoint-extension witness.
A derived StageEstimates record is an alternative source of the
positive-stage estimates. No quantitative conclusion or representation of
the glued particular field is added as a hypothesis here.
The Cartesian curl of the actual finite particular-wave sum #
The potential and pressure are the literal current-band sums constructed in
ActualCurrentParticularPhysical. Their modes are identified with the same
canonical solver used by the correction cycle. On a valid current polar chart,
the curl is therefore the actual particular velocity increment, with its physical
scale and moving frame. No output representation is an input to these identities.
The literal finite potential has exactly the physical curl required by the particular stage of the correction cycle, throughout each valid current chart.
The pressure uses the same finite harmonic and label sums and the square of the physical velocity scale.
Exact exterior vanishing of the actual mean fields #
The native moving support is the nominal profile interval itself. Squaring the exact normalized-radius identity places the physical support in the closed nominal active annulus, without enlarging either edge. This applies to the literal initialized fields and to every mean stage of the same coherent cycle.
The actual moving radial support gives the closed nominal active annulus at every physical support point with a comparable band.
Scalar coefficients and their Cartesian angular realization vanish as germs on the exterior of the closed nominal active annulus.
The direct angular-field constructor used for both angular velocity and stream potentials retains the same exact exterior zero.
The same initialized fields #
The full initialized stream is the literal temporal-plus-rank stream.
Every stage of the same coherent cycle #
Exterior germs for physical stages #
One certificate supplies support and axis-germ bounds. The existing exterior lemmas on closed sublevels remain available; they imply this local certificate.
The exterior of the active annulus is open within the preterminal region: the profile radius is continuous there and the annulus is its preimage of a closed interval.
A stage field of the actual candidate: zero near every point of the physical domain outside the active annulus.
- exterior (w : ProblemStatement.SpaceTime) : w ∈ ActualCandidateConstruction.physicalDomain B N0 → w ∉ ActualPolarCoverage.active → f =ᶠ[nhds w] fun (x : ProblemStatement.SpaceTime) => 0
The field vanishes in a neighborhood of each exterior point.
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A pointwise exterior identity suffices, since the exterior is open in the domain.
The zero field is a physical stage.
Shrinking support: a support point lies in the active annulus, whose outer edge is below the outer constant.
The axis of the local domain lies outside the active annulus, so the hub's axis zero germ is a projection.
Exterior zero germs are preserved by addition.
The finite initialization, without the base fields #
Initial potential, given by InitialPhysicalData.potential B N0 + ActualCandidateConstruction.streamMeanStages B N0 0.
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Initial pressure, given by InitialPhysicalData.pressure B N0 + ActualCandidateConstruction.pressureMeanStages B N0 0.
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Initial direct, given by ActualCandidateConstruction.angularMeanStages B N0 0.
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Initial direct data, constructed using ActualMeanStageData.initialAngularData.
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Exact exterior coordinates #
The initial potential has an exterior zero germ on its physical domain.
The initial pressure has an exterior zero germ on its physical domain.
The initial direct field has an exterior zero germ on its physical domain.
The literal zeroth potential and pressure retain the base #
Zeroth potential, given by `TailGaugePotential.finalPotential certificate modulation upper B
- initialPotential B N0`.
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Zeroth pressure, given by FinalSlowBase.pressure certificate modulation upper B + initialPressure B N0.
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The particular fields come from the same current state #
The valid-band representative uses the common physical floor. Its local
formulas are the actual current solves, with the initializer's label order
converted by ActualCycleParameters.particularState inside the producer.
Particular potential, given by ActualValidBandWaves.potential (ActualCandidateConstruction.cycle B N0 j) (ActualCandidateConstruction.firstBand B N0).
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Particular pressure, constructed using ActualValidBandWaves.pressure.
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Mean fields on the exact residual-comparison charts #
The actual native run supplies every mean and signed request #
Run data, bundling invariant, step, particular.
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- NavierStokes.ActualCandidateAssembly.runData B N0 hN = { invariant := ⋯, step := NavierStokes.ActualCyclePreservation.stateStepData B N0 hN, particular := ⋯ }
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Signed potential, constructed using ActualSignedExterior.cyclePotential.
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Signed pressure, constructed using ActualSignedExterior.cyclePressure.
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Positive potential, given by particularPotential B N0 j + signedPotential B N0 hN j + ActualCandidateConstruction.streamMeanStages B N0 (j + 1).
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Positive pressure, given by particularPressure B N0 j + signedPressure B N0 hN j + ActualCandidateConstruction.pressureMeanStages B N0 (j + 1).
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Direct data, given by ActualCandidateConstruction.directData (meanCycleInput B N0 hN).
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Potential stages, given by GermCandidateAssembly.potentialStages certificate modulation upper B (initialPotential B N0) (positivePotential B N0 hN).
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Direct stages, given by LocalAngularDiagonal.rawSeries (directData B N0 hN).
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Pressure stages, given by MixedCandidateAssembly.pressureStages certificate modulation upper B (initialPressure B N0) (positivePressure B N0 hN).
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Geometric inputs are consequences of the same constructed fields #
The stream correction inherits its zero germs from its exterior identity.
The mean pressure inherits its zero germs from its exterior identity.
The positive stages are sums of three physical stages.
The quantitative component record uses these exact sequences #
Estimates, constructed using GluedStageEstimates.actualStageEstimates.
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The common schedule and its actual fields #
The output retains the actual three sums, the smooth force, and the strong consequences for this same velocity and pressure.
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One closed choice fixes all three raw sequences together.
Selected potential stages, constructed using potentialStages.
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Selected direct stages, constructed using directStages.
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Selected pressure stages, constructed using pressureStages.
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