Approximate Stein Classes for Truncated Density Estimation
Daniel J. Williams, Song Liu
TL;DR
This work tackles truncated density estimation where the normalising constant is intractable and the boundary is unknown. It introduces approximate Stein classes and the truncated kernelised Stein discrepancy (TKSD), which can be evaluated from boundary samples without a fixed boundary weighting function. By formulating TKSD via a Lagrangian dual and minimising it, the authors estimate unnormalised truncated densities and prove consistency under mild conditions. Theoretical analysis is complemented by experiments showing TKSD competitive with existing methods while requiring fewer boundary details, and practical demonstrations on complex boundaries such as the United States border. Overall, the approach provides a data-driven, boundary-agnostic framework for truncated density estimation with solid theoretical guarantees and practical effectiveness.
Abstract
Estimating truncated density models is difficult, as these models have intractable normalising constants and hard to satisfy boundary conditions. Score matching can be adapted to solve the truncated density estimation problem, but requires a continuous weighting function which takes zero at the boundary and is positive elsewhere. Evaluation of such a weighting function (and its gradient) often requires a closed-form expression of the truncation boundary and finding a solution to a complicated optimisation problem. In this paper, we propose approximate Stein classes, which in turn leads to a relaxed Stein identity for truncated density estimation. We develop a novel discrepancy measure, truncated kernelised Stein discrepancy (TKSD), which does not require fixing a weighting function in advance, and can be evaluated using only samples on the boundary. We estimate a truncated density model by minimising the Lagrangian dual of TKSD. Finally, experiments show the accuracy of our method to be an improvement over previous works even without the explicit functional form of the boundary.
