ObservableScaleAntitone #
Ported from scottnarmstrong/Superdiffusion at 7f20476385d4af418f110303085ad0740c9eba46. Module imports, support namespace and local option directives adapted for Lean Pool.
Provider: antitonicity of the Section 3 error observable in the scale #
ABK26's display e.mathcalE.monotone.ordered asserts, among other things, that
for t < s
๐_{s,p,q}(โก_m; a, aโ) โค ๐_{t,p,q}(โก_m; a, aโ) ,
i.e. the multiscale homogenization error is antitone in the smoothness
exponent. At p = โ this is already proved on CoarseGraining's carrier by
ErrorComparison.homogenizationErrorOnCube_infinity_finite_le_of_lt
(ErrorComparison.Monotonicity); the mechanism is that the p = โ scale
response is monotone in the depth (scaleResponse_depth_monotone), so that
CoarseGraining's Homogenization.tsum_geometricWeight_le_of_monotone applies
and the geometric reweighting costs nothing.
This file transports that inequality, at q = 2, from CoarseGraining's carrier
onto the Section 3 observable Observable.cutoffHomogenizationError, and
composes it with CoarseGraining's a.e. weak-Orlicz monotonicity so that a tail
estimate proved at one scale is available verbatim at every larger scale.
It is Algsuperdiff.Section3.baseLoss, not the error observable, that is
restricted to the open interval.
No new constant, and no summability side condition: both are already
discharged inside the Monotonicity lemma, whose tsum bookkeeping uses the
root cube's uniform deterministic response bound.
Main results #
cutoffHomogenizationError_ae_antitone: a.e. antitonicity of the observable in the smoothness exponent.isBigOWith_cutoffHomogenizationError_of_lt: a weak-Orlicz upper-tail estimate for the observable at a scaletholds verbatim at every larger scales.
References #
- ABK26,
e.mathcalE.monotone.ordered;d.mathcal.E(2.28).
e.mathcalE.monotone.ordered on the Section 3 observable, at q = 2.
For 0 < t < s, almost surely under the cutoff-sample law,
๐_{s,โ,2}(โก_m; a_m, ฯ_m) โค ๐_{t,โ,2}(โก_m; a_m, ฯ_m) .
Taking s = 1 gives the endpoint instance of any estimate proved on the open
interval 0 < t < 1.
Endpoint transport of a weak-Orlicz upper-tail estimate along the scale.
If the Section 3 error observable at a scale t satisfies ๐_t โค O_ฮจ(A), then
so does the observable at every larger scale s, with the same ฮจ and the
same amplitude A.
This is the composition of cutoffHomogenizationError_ae_antitone with
CoarseGraining's Homogenization.Book.Ch04.isBigOWith_of_ae_le; neither piece
alone delivers the endpoint instance the Section 3.2 base case needs.