Sections of convex functions #
A section of a real function u on Ω, centered at x with slope ℓ and height h, is
the set of y ∈ Ω with u y < u x + ℓ (y - x) + h. In an inner product space, taking
ℓ y = ⟪p, y⟫ gives the usual section with subgradient p; at a differentiability point
one takes ℓ = fderiv ℝ u x. Keeping the slope as a linear functional allows changes of
coordinates without choosing an inner product.
These sets are the domains on which local Monge–Ampère estimates are normalized. We prove convexity, openness, height nesting, contraction about the center, and invariance under adding affine functions. A continuous potential takes the boundary value of the section on its frontier, and a chord leaving a point of a section through a second point gives an inclusion into a section at that second point, which is the step behind the engulfing property of sections. Positive rescaling and linear coordinate changes give the exact unit-height normalization identity. A supporting slope is required for the nonpositive-height emptiness statement, but not for convexity or the normalization identities.
The function is real-valued on its specified domain; no extension outside the domain is used. For an extended-real convex potential one can take its real representative on the interior of its effective domain.
References #
- C. E. Gutiérrez, The Monge–Ampère Equation, 2nd ed., Birkhäuser, 2016, §1.8.
- A. Figalli, The Monge–Ampère Equation and Its Applications, EMS, 2017, Chapter 3.
A section is contained in its domain.
Increasing the height enlarges a section.
On a section of a convex function, adding a linear function and a constant to the potential
keeps it convex. With L = -ℓ this subtracts the plane of the section from the potential.
If u y lies above the plane through (x, u x) with slope ℓ (the supporting plane at x),
then a section convexSection Ω u x ℓ h containing y has positive height h.
Contracting a section by a positive factor at most one about its center contracts its height by the same factor. This uses convexity and does not require a supporting slope.
Engulfing along a chord. Let m be a supporting slope at y, and let y lie above the
plane through x with slope ℓ. If z ∈ S(x, h) and the chord from z through y, extended
beyond y by t > 0 times its length, ends in S(x, k), then z lies in the section at y
with slope m and height h + k / t. No convexity is needed: the supporting plane at y lies
below the potential at the end of the chord.
Pulling back the domain, potential and slope by a linear map pulls back the section. The map need not be injective or surjective.
Translating coordinates translates the center and the domain of a section.
Subtracting the supporting plane, dividing by the positive height, and using coordinates
y = x + A z turns a section into a section centered at zero, with zero slope and height one.
For a linear equivalence this is the section normalization used in local estimates.
Sections of a continuous potential on an open domain are open when the slope is continuous. Convexity is not needed for this assertion.
Within the domain, the closure of a section lies in every section of strictly larger height. Continuity is needed only on the domain, which need not be closed.
If the closure of a section lies in the domain of a continuous potential, then adding a continuous linear function and a constant to the potential keeps it continuous on that closure.
If the closure of a section lies in the open domain of a continuous potential, then on the
frontier of the section the potential equals the plane through (x, u x) with slope ℓ, raised
by the height.
A section of height at most H lies in the section of height H, so it inherits its
boundedness and the inclusion of its closure in the domain.