PrincipalResponseLegsBudgetEllipticity #
Ported from scottnarmstrong/Superdiffusion at 7f20476385d4af418f110303085ad0740c9eba46. Module imports, support namespace and local option directives adapted for Lean Pool.
Provider: sub-step (ii) of the principal response, the ellipticity budget #
Source display, immediately preceding the independence sentence:
avsum_{z in 3^n Zd cap cu_K}
E[ shom_{m-h} |p_z|^2 + shom_{m-h}^{-1} |q_z|^2 ] <= C ,
quoted from e.nablaw.in.L.eight (label). Here (p_z; q_z) = P_z is the
localized load of e.Pz.def (label), carried in this repository by
principalPz with components principalPz_fst and principalPz_snd.
What this module proves #
Because P_z is by definition bfAhom_{m-h}^{-1/2} applied to the raw averaged
slope pair, the two normalizations cancel exactly against the two weights
shom_{m-h} and shom_{m-h}^{-1} of the display. The integrand is therefore an
unnormalized quantity:
ellipticityBudget_eq-- the exact collapse
an unconditional identity, withshom |p_z|^2 + shom^{-1}|q_z|^2 = |e' + (grad w_D)_R|^2 + |e + (grad w_N + shom^{-1} h e')_R|^2 ,Rthe localization cube.
The per-cube Jensen step, the grid average over the triadic subcubes of cu_K
at the localization scale, and the passage to expectations all belong to the
consuming lane. Carried out there, this identity gives the manuscript's
left-hand side bounded by
2(|e|^2 + |e'|^2) + 2 E[ ‖grad w_D‖^2_{L^2(cu_K)} ] + 2 E[ ‖grad w_N + shom^{-1} h e'‖^2_{L^2(cu_K)} ],
which is what e.nablaw.in.L.eight is quoted for.
The grid rendering #
The source averages over the lattice 3^n Zd cap cu_K, i.e. over the cubes `z
- cu_n
tilingcu_K. Those cubes are exactly the triadic descendants ofcu_Kat depthK - n, and the repository'sdescendantsAverageis the corresponding average; this is the standard rendering used throughout`Provider/BadEvents` and elsewhere in this tree.
The collapse of the two normalizations #
The integrand, collapsed. The weights shom_{m-h} and shom_{m-h}^{-1}
cancel the two legs of the normalization bfAhom_{m-h}^{-1/2} in e.Pz.def
exactly, leaving the squared lengths of the raw averaged slope pair.