[IPOL announce] new article: Thin-plate Splines on the Sphere for Interpolation, Computing Spherical Averages, and Solving Inverse Problems
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Sat Feb 14 00:34:56 CET 2026
A new article is available in IPOL: https://www.ipol.im/pub/art/2026/451/
Max Dunitz,
Thin-plate Splines on the Sphere for Interpolation, Computing Spherical
Averages, and Solving Inverse Problems,
Image Processing On Line, 16 (2026), pp. 1–112.
https://doi.org/10.5201/ipol.2026.451
Abstract
In many applications, planar spline interpolations of scattered data on
the sphere are unsatisfactory; spherical splines are desired. Wahba
(1981) defined the thin-plate splines on the sphere by analogy with the
polynomial splines on the circle and the thin-plate splines in Rd. The
thin-plate spline fit to a scattered data set on the sphere is the
solution to an empirical risk minimization problem that penalizes the
infidelity of the fit to the data as well as its 'wiggliness'. This
latter term is the square of a seminorm penalty based on the
Laplace-Beltrami operator. The minimization problem is posed in a
reproducing kernel Hilbert space (RKHS) of functions of finite
wiggliness, whose reproducing kernel is isotropic and, due to a result
by Schoenberg (1942), given by a Legendre series. A closed-form
expression (in terms of the polylogarithm) for the kernel was found by
Wendelberger (1982) and re-discovered by Beatson and zu Castell (2018).
These closed-form expressions make not just spline interpolation but
also downstream signal-processing tasks, such as cubature or resolution
of inverse problems, more tractable in fields where scattered data and
spherical models are common, such as remote sensing, geostatistics,
motion planning, graphics, and medical imaging. In this paper, we
present a tutorial on spline methods in RKHSs and show how they can be
used to interpolate, smooth, and numerically integrate scattered data on
the sphere and solve related inverse problems. The accompanying demo
compares thin-plate spline interpolation over the sphere with thin-plate
splines on an equirectangular projection and natural cubic splines on a
one-dimensional latitudinal projection used in greenhouse gas
monitoring. Global mean values of the interpolation surfaces are
presented as well, to illustrate how this isotropic spherical kernel -
which penalizes interpolant wiggliness without concern for
application-specific factors like atmospheric winds - affects the
computation of global averages.
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