Exact linear harmonic residual #
Every differential operator uses an actual Fréchet derivative. The coefficient field supplied to the linearization is arbitrary, so the formula also applies to a curl-corrected coefficient without replacing it by its tangent principal part. The angular direction is unscaled.
Time direction, given by Vf x - ε • Vs x.
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- NavierStokes.LinearWaveResidual.timeDirection ε Vf Vs x = Vf x - ε • Vs x
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Complex base, defined pointwise by (base R b F G x i : ℂ).
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- NavierStokes.LinearWaveResidual.complexBase R b F G x i = ↑(NavierStokes.LinearWaveResidual.base R b F G x i)
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Cylindrical bilinear advection, including the derivative of the frame.
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Gradient, given by ![along Vr p x, (R x)⁻¹ • along Vθ p x, along Vz p x].
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The genuine differential linearization with viscosity ε.
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Matrix K from (27), with its radial coefficients actually differentiated.
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The base derivative and radial-flow connection terms outside K.
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Material phase defect, given by along Vt Φ x + b x * along Vr Φ x + F x * along Vθ Φ x + G x * along Vz Φ x.
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Slow transport, defined pointwise by -(ε : ℂ) * along Vs (fun y => a y i) x + (b x : ℂ) * along Vr (fun y => a y i) x + (G x : ℂ) * along Vz (fun y => a y i) x.
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Stripped pressure gradient, given by ![along Vr p x, 0, along Vz p x].
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The complete viscous braces in (31), after removal of phase-square damping.
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Principal as an element of ComplexVector.
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Remainder as an element of ComplexVector.
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The two linear advection terms produce K and exactly the displayed
base-derivative and radial-flow connection terms.
The scalar and frame Laplacian identities assembled into the viscous braces of (31), with the phase-square term separated.
Full identity (31) for the actual amplitude supplied to the linear operator. The principal and remainder are both explicitly defined above.
Actual slot phase and projected pressure #
Scaling a prescribed fast direction produces exactly the manuscript's
prefactor, for example c = Q^(1+h) multiplying Nabs.
The material defect used in the residual is the actual backward-time
material derivative already computed in PhaseCalculus.
Explicit formula for the phase material defect, including the sign of the slow-time term. No estimate for this term is assumed.
A base coefficient depending only on slow coordinates has precisely the slow differential along a slot direction.
Numerator in the pressure from the projected equation. The derivative
of n is the actual derivative in the fast direction.
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Projected pressure, given by (Complex.I / (κ : ℂ)) * projectionNumerator Vf n a Ka f x / Complex.ofReal (‖n x‖ ^ 2).
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- NavierStokes.LinearWaveResidual.projectedPressure κ Vf n a Ka f x = Complex.I / ↑κ * NavierStokes.LinearWaveResidual.projectionNumerator Vf n a Ka f x / ↑(‖n x‖ ^ 2)
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Substituting the projected pressure into the principal part is an exact identity for arbitrary amplitudes; no tangent ODE is imposed on the actual coefficient supplied to the residual.
Real-linear transfer of the complex calculation #
Real lift, defined pointwise by (a x i : ℂ).
Equations
- NavierStokes.LinearWaveResidual.realLift a x i = ↑(a x i)
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Real transport as an element of Fin 3 → ℝ.
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Real frame laplacian as an element of Fin 3 → ℝ.
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Real component form of the same differential linearization.
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The complex linearization transfers through any real continuous linear functional, in particular real and imaginary parts, because its base is real.
The actual Cartesian and cylindrical linearizations #
Bilinear advection, constructed using u.
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Cylindrical linear residual, constructed using temporalDerivative.
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Linearization in the original Cartesian derivative definitions.
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The real differential linearization is exactly conjugated by the cylindrical frame. Both cross-advections are derived from the actual Cartesian derivative, rather than from a postulated residual identity.
Space direction, given by (0, coordinateVector i).
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Physical time direction, given by (1, 0).
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Coordinate radius, given by x.2 0.
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The generic real component operator used for the harmonic calculation is the actual cylindrical linearization when its directions are the physical spacetime coordinate directions.