The receding-axis contradiction #
eq:aniso:zoom:receding:quotient: the final contradiction of the receding-axis case.
In the recentred variables eq:aniso:zoom:receding:variables the selected point is the
origin of ℝ × ℝ and the axis sits at R = -A_n, so the meridional fields live on the
whole plane. The limiting divergence identity of eq:aniso:zoom:receding:div is
∂_R V + ∂_Z W = 0 with no radial quotient, the term V_n / (A_n + R) vanishing
uniformly on compact sets because A_n → ∞ while V_n stays bounded. Endpoint vanishing
is therefore CIV.endpoint_vanishing_rec, which holds at every point of the plane and
needs no continuity statement at a boundary; and the radial quotient at the selected point
is bounded by M / A_n. All three summands of eq:aniso:zoom:selected thus tend to 0.
Uniform convergence on a set to a constant implies pointwise convergence to that constant at every point of the set.
eq:aniso:zoom:receding:endpoint in pointwise form: a divergence-free meridional pair
(V, W) on ℝ × ℝ with ∂_R W = 0 and V bounded has ∂_R V and ∂_Z W vanishing at
every point, in particular at the origin, which is the selected point in the variables
eq:aniso:zoom:receding:variables. The divergence hypothesis is the quotient-free identity
of eq:aniso:zoom:receding:div.
The final contradiction of the receding-axis zoom. On a set S containing the selected
point — the origin of the variables eq:aniso:zoom:receding:variables — the recentred
derivatives converge uniformly to the endpoint derivatives, which vanish identically by
eq:aniso:zoom:receding:endpoint; the radial quotient at the selected point is at most
M / A_n with A_n → ∞, which is eq:aniso:zoom:receding:quotient. The three summands of
eq:aniso:zoom:selected therefore tend to 0, and ge_of_tendsto' forces c₀ ≤ 0,
contradicting hc₀.