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Horospherical Convexity (h-convexity) in Hyperbolic Spaces

Updated 11 July 2026
  • Horospherical convexity is a hyperbolic convexity concept where supporting horoballs replace half-spaces and smooth boundaries satisfy curvature conditions (κ_i ≥ 1 or κ_i > 1 for strict cases).
  • The horospherical support function and Gauss map enable reparametrization of h-convex hypersurfaces over the sphere, facilitating analysis through fully nonlinear PDEs.
  • Variants such as weak and horocyclic convexity extend the concept to immersed hypersurfaces and Hadamard-manifold optimization, linking geometric support with asymptotic structures.

Horospherical convexity, usually abbreviated h-convexity, is a hyperbolic analogue of Euclidean convexity in which affine half-spaces are replaced by horoballs, horospheres, or Busemann-function sublevel sets. In hyperbolic space, a bounded domain KHn+1K\subset \mathbb H^{n+1} is h-convex if every boundary point admits a supporting horoball; for smooth boundaries this is equivalent to the principal-curvature condition κi1\kappa_i\ge 1, while strict or uniform h-convexity requires κi>1\kappa_i>1 (Luo et al., 2024). Closely related variants appear for immersed hypersurfaces, planar horocyclically convex domains, and Hadamard-manifold optimization, all built from the same principle: the supporting objects are adapted to the asymptotic geometry of nonpositively curved spaces rather than to linear structure (Bonini et al., 2016, Arango et al., 2024, Criscitiello et al., 22 May 2025).

1. Supporting horoballs and curvature thresholds

The basic geometric definition in Hn+1\mathbb H^{n+1} is a support condition. A bounded domain KHn+1K\subset \mathbb H^{n+1} is h-convex if every boundary point of K\partial K admits a supporting horoball, that is, a horoball BB with KBK\subset B and the boundary point lying on B\partial B. Geometrically, this means that the domain is an intersection of horoballs, just as a Euclidean convex body is an intersection of half-spaces. In the hyperboloid model, horospheres are the hypersurfaces whose principal curvatures are all equal to $1$, so for a smooth boundary the support condition is equivalent to

κi1\kappa_i\ge 10

and strict h-convexity to

κi1\kappa_i\ge 11

This curvature threshold is the hyperbolic shift that distinguishes horospherical convexity from ordinary geodesic convexity (Luo et al., 2024, Andrews et al., 2017).

A weaker immersion-theoretic version is weak horospherical convexity. For an oriented immersed hypersurface κi1\kappa_i\ge 12, one considers the tangent horosphere κi1\kappa_i\ge 13 at κi1\kappa_i\ge 14 whose outward unit normal agrees with the chosen normal field. The hypersurface is weakly horospherically convex at κi1\kappa_i\ge 15 if a neighborhood of κi1\kappa_i\ge 16 stays on one side of κi1\kappa_i\ge 17, equivalently if all principal curvatures satisfy either

κi1\kappa_i\ge 18

The corresponding uniform version requires a constant κi1\kappa_i\ge 19 with κi>1\kappa_i>10 everywhere, and this is the class used in the global correspondence and embeddedness theory (Bonini et al., 2016).

This support viewpoint also has lower-dimensional analogues. In the unit disk κi>1\kappa_i>11, a proper subdomain κi>1\kappa_i>12 is horocyclically convex if every interior boundary point admits a supporting horodisk. The paper on horocyclically convex domains emphasizes the analogy

κi>1\kappa_i>13

and states that every κi>1\kappa_i>14-convex domain is horo-convex (Arango et al., 2024).

2. Support functions, Gauss maps, and conformal correspondences

For smooth uniformly h-convex hypersurfaces, horospherical convexity is encoded by a support function on the sphere. If κi>1\kappa_i>15 is the position vector of κi>1\kappa_i>16 and κi>1\kappa_i>17 is the outward unit normal, then

κi>1\kappa_i>18

for some κi>1\kappa_i>19 and Hn+1\mathbb H^{n+1}0. The function

Hn+1\mathbb H^{n+1}1

is the horospherical support function, and the associated horospherical Gauss map Hn+1\mathbb H^{n+1}2 sends each boundary point to the direction Hn+1\mathbb H^{n+1}3. For uniformly h-convex domains this Gauss map is a diffeomorphism, so the hypersurface can be reparametrized over Hn+1\mathbb H^{n+1}4. In this parametrization the decisive tensor is

Hn+1\mathbb H^{n+1}5

and uniform h-convexity is equivalent to

Hn+1\mathbb H^{n+1}6

Moreover,

Hn+1\mathbb H^{n+1}7

so the eigenvalues of Hn+1\mathbb H^{n+1}8 are the hyperbolic curvature radii

Hn+1\mathbb H^{n+1}9

The horospherical surface area measure is then

KHn+1K\subset \mathbb H^{n+1}0

and the KHn+1K\subset \mathbb H^{n+1}1-th horospherical KHn+1K\subset \mathbb H^{n+1}2-surface area measure is

KHn+1K\subset \mathbb H^{n+1}3

These formulas make h-convexity directly usable in fully nonlinear PDE (Luo et al., 2024).

A parallel formulation exists for weakly horospherically convex hypersurfaces via the light-cone map. For an oriented immersion KHn+1K\subset \mathbb H^{n+1}4 with unit normal KHn+1K\subset \mathbb H^{n+1}5, the light-cone map is

KHn+1K\subset \mathbb H^{n+1}6

If KHn+1K\subset \mathbb H^{n+1}7 is the hyperbolic Gauss map, then

KHn+1K\subset \mathbb H^{n+1}8

where KHn+1K\subset \mathbb H^{n+1}9 is the horospherical support function, and the induced horospherical metric is

K\partial K0

When K\partial K1 is injective, this becomes a conformal metric K\partial K2 on a domain K\partial K3. The local correspondence is governed by the tensor

K\partial K4

whose eigenvalues \

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