1846 — The Polar Double-Morse Coefficient Is a Legendre Variation
Frozen branch data
Entry 1845 gives the ordered branch points
Use the uniquely normalized Möbius coordinate
which sends to . The fourth branch point is
Thus the polar double-Morse coefficient is the pullback of the universal Legendre Gauss--Manin variation by this Hessian-weighted normal modulus, up to the Kummer factor already typed by the physical current in Entry 1843.
Labelled cusps
The three nodal degenerations are
The first two are the existing labelled wall normals. The third is Entry 1845's internal coefficient collision. Standard Legendre nearby cycles at all three cusps are Tate/Kummer; no additional carrier incidence is needed.
Exchanging the two labelled walls gives
so occurrence covariance is retained rather than erased by an unlabelled cross-ratio.
Narrow result
The five-site polar sector repeats, at a new local geometry, the architecture previously found in the homogeneous three-site loop:
This supports H2: the carrier supplies the labelled walls and their incidence, while the elliptic period system is a sector-specific coefficient object.
Scope
This is a local coefficient theorem near the polar double-Morse point. It does not construct the global physical relative-chain pairing, and it does not prove that the complete five-site observable is exhausted by this block.
Next falsifier
Compute the coarse modular parameter near each labelled cusp. Test whether each linear resolved normal is a square-root coordinate over the coarse modular degeneration, as at the three-site total-energy boundary.
Evidence
research/benincasa/checkers/five_site_region_pair_polar_legendre_modulus.pyresearch/benincasa/results/five-site-region-pair-polar-legendre-modulus.json- Entries 1843--1845
- allocator claim:
seqclaim-0aca92678db7f957d2438692