R2-R: the residual of the rescaled receding vorticity-quotient equation tends to zero #
The receding-branch analogue of CIV.tendsto_finResidual (CIV/Zoom/FiniteResidual.lean) at
(m, d) = (2, 1): against a test function φ on Vec 2 × (-∞, -1), the pairing of the
rescaled azimuthal vorticity Θ_n with the adjoint operator of eq:aniso:zoom:receding:limit
tends to zero along the receding zoom sequence.
The weak form comes from CIV.zoomTheta_pde (CIV/Zoom/RecedingEquation.lean), rearranged so
that the drift-divergence pairing CIV.integral_recedingResidual_eq (a receding-axis,
axis-singularity-free analogue of CIV.integral_liftedResidual_eq) applies directly: every
term of eq:aniso:zoom:receding:equation outside the limit operator is collected into the
swirl flux S_n²/(A_n+R) (whose ∂_Z reproduces the swirl-source term) and a source G_n
bundling the ∂_R Θ_n/(A_n+R) term, the two curvature terms, and the force term. Each of the
three pieces of the weak-form remainder — δ_n² ∫ Θ_n ∂_ZZ ψ, -∫ (S_n²/(A_n+R)) ∂_Z ψ, and
∫ G_n ψ — is bounded by a constant times a factor tending to 0 uniformly on tsupport ψ as
n → ∞, since A_n = r_n/λ_n → ∞ and δ_n = λ_n^{2h} → 0.
The weak form of a drift-diffusion equation on Vec 2 × ℝ off a closed set #
The integration by parts of the receding branch of the passage to the limit: if q, the
drift B, the flux Fz and the source G satisfy
∂_τ q + B · ∇q = ∂_RR q + κ ∂_ZZ q + ∂_Z Fz + G pointwise on an open set S, with divB the
divergence of B there, then against every test function supported in a compact subset of S
the residual of eq:aniso:zoom:receding:limit is κ ∫ q ∂_ZZ ψ - ∫ Fz ∂_Z ψ + ∫ G ψ.
The joint-derivative bridge for dr, dz, dtPast on the plane #
A plane function differentiable on an open set D has a differentiable dr on any set
where a further C² bound is known.
A plane function differentiable on an open set D has a differentiable dz on any set
where a further C² bound is known.
The plane-and-time coordinate identification, as a continuous linear map.
Equations
Instances For
The Vec 2 × ℝ double derivative of a plane function composed with planeLiftPoint, in the
direction basisVec 0 twice, in terms of the plane function's own dr ∘ dr.
The Vec 2 × ℝ double derivative of a plane function composed with planeLiftPoint, in the
direction basisVec 1 twice, in terms of the plane function's own dz ∘ dz.
The swirl flux and the receding source term #
The receding-axis swirl flux S_n² / (A_n + R) of eq:aniso:zoom:receding:equation.
Equations
- CIV.swirlFluxPlane lam h rc zc u p = CIV.zoomSRec lam h rc zc u p ^ 2 / (rc / lam + p.1.1)
Instances For
The receding-axis source `(1/(A_n+R))∂_RΘ_n − Θ_n/(A_n+R)² + λ_n⁴δ_n H_n
- (V_n/(A_n+R))Θ_n
ofeq:aniso:zoom:receding:equation: the four terms that vanish together with the∂_Z-part of the swirl flux and theδ_n²∂_ZZterm asn → ∞`.
Equations
- One or more equations did not get rendered due to their size.
Instances For
The ∂_Z-derivative of the swirl flux is (1/(A_n+R)) times the ∂_Z-derivative of
S_n², since the denominator A_n + R does not depend on Z.
The rescaled azimuthal vorticity equation of eq:aniso:zoom:receding:equation, rewritten
with the transport in advective form and the divergence-free correction, swirl source and force
gathered into the swirl flux swirlFluxPlane and the source recedingSourcePlane, ready for
integral_recedingResidual_eq.
dr of a plane function ContDiffOn order ≥ 2 on an open set is continuous there.
Domain membership and bounds along the moving centre #
R2-R: the residual tends to zero #
R2-R: the residual of the rescaled receding vorticity-quotient equation tends to zero.