Direct angular means in the physical diagonal #
The angular velocity is retained as a direct field. It is not replaced by an axial primitive. Axisymmetry proves its divergence equation, and an annular zero germ removes the coordinate singularity on the axis.
Slow: an abbreviation for ℝ × ℝ.
Equations
Instances For
Cyl point: an abbreviation for ℝ × (ℝ × ℝ).
Instances For
Slow point, given by (w.1, w.2 2).
Instances For
Cyl point, given by (w.1, (radius w, w.2 2)).
Equations
Instances For
Slow of cyl, given by (p.1, p.2.2).
Equations
- NavierStokes.DirectAngularDiagonal.slowOfCyl p = (p.1, p.2.2)
Instances For
Physical domain, given by slowPoint ⁻¹' U.
Equations
Instances For
Profile to cyl, given by (p.1, (Real.sqrt (2 * p.2.1), p.2.2)).
Instances For
Rate, given by b (profileToCyl p) / Real.sqrt (2 * p.2.1).
Equations
- NavierStokes.DirectAngularDiagonal.rate b p = b (NavierStokes.DirectAngularDiagonal.profileToCyl p) / √(2 * p.2.1)
Instances For
Literal angular velocity with physical tangential magnitude b.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Rotation field, constructed using AxisymmetricResidual.pack.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The cancellation is computed from actual Cartesian derivatives.
A moving positive inner support radius is a primitive support datum. It may shrink as the physical terminal point is approached.
- scalar : Coefficient
Scalar of
AngularData, of typeCoefficient. - smooth : ContDiffOn ℝ (↑⊤) self.scalar (positiveDomain U)
Inner of
AngularData, of typeSlow → ℝ.- inner_continuous : ContinuousOn self.inner U
Instances For
Multiply, bundling scalar, smooth, inner, inner_continuous and the required
compatibility proofs.
Equations
Instances For
Cut coefficient, defined pointwise by SmoothCutoffs.scaledCutoff a (q p) * b p.
Equations
- NavierStokes.DirectAngularDiagonal.cutCoefficient a q b p = NavierStokes.SmoothCutoffs.scaledCutoff a (q p) * b p
Instances For
Cut, given by D.multiply (fun p => SmoothCutoffs.scaledCutoff a (q p)) ((SmoothCutoffs.scaledCutoff_contDiff a).comp_contDiffOn hq).
Equations
- D.cut a q hq = D.multiply (fun (p : NavierStokes.DirectAngularDiagonal.CylPoint) => NavierStokes.SmoothCutoffs.scaledCutoff a (q p)) ⋯
Instances For
Locally finite direct angular sums #
Angular sum, given by SolenoidalDiagonal.potentialSum a q (fun j => angularField (b j)).
Equations
Instances For
Angular partial, given by SolenoidalDiagonal.partialPotential a q (fun j => angularField (b j)) N.
Equations
- NavierStokes.DirectAngularDiagonal.angularPartial a q b N = NavierStokes.SolenoidalDiagonal.partialPotential a q (fun (j : ℕ) => NavierStokes.DirectAngularDiagonal.angularField (b j)) N
Instances For
Curl potentials plus direct angular velocity #
Mixed velocity, defined pointwise by SolenoidalDiagonal.velocitySum a q A x + angularSum a q b x.
Equations
Instances For
The actual similarity cutoff #
Preterminal slow, given by {s | s.1 < 1}.
Equations
Instances For
Q coefficient, given by SimilarityProfile.q h.
Instances For
The existing Cartesian spatial cutoff is axisymmetric #
Spatial profile, given by SpatialLocalization.cutoffProfile (p.2.1 ^ 2, p.2.2).
Equations
Instances For
Actual full-fiber means restricted to a physical graph #
The time/axial variables in the actual mean-field convention (T,Z).
Equations
- NavierStokes.DirectAngularDiagonal.graphSlow G s = (G.velocityScale * G.radialScale * G.epsilon * (1 - s.1), G.radialScale * G.epsilon * s.2)
Instances For
Graph point as an element of Lift.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The physical velocity normalization is included here.
Equations
Instances For
Smoothness and the positive moving support of the actual mean field produce the angular data. No divergence or physical output is assumed.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Common angular data, given by graphAngularData _ (Real.rpow_pos_of_pos hQ _) hU ha ell hell hpos f hf hs.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The common-graph coefficient carries exactly the manuscript's
Q^(-A) velocity factor, with no independent angular choice.
The direct angular part of the literal temporal update, with its regularity and support inherited from the actual input residual.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The direct angular part of the literal rank update. Its smoothness comes from the actual five-row rank family and current debt.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Agreement with the actual offplane continuation fields #
Native graph data, bundling radialScale, velocityScale, epsilon, exponent and the
required compatibility proofs.
Equations
- One or more equations did not get rendered due to their size.
Instances For
This is the direct continuation field, with no curl applied.
Continuation angular data, constructed using graphAngularData.
Equations
- One or more equations did not get rendered due to their size.
Instances For
Mixed finite prefixes and preservation of every axis jet #
If the actual potentials vanish near the axis, adding the direct angular diagonal preserves the entire axis germ, hence every axis jet.