Calculation of the sound field between noise sources and a closed two-dimensional measurement surface is an inverse propagation problem. A powerful and popular method for the reconstruction of sound fields in this space is based on boundary element methods applied to the Helmholtz integral equation. Unfortunately, due to the numerical nature of these solutions, the physics associated with backtracking (backpropagating) the field from the measurement surface to the source surfaces is hidden. Analytic models are used to view this backpropagation as a deconvolution operation on the measured field. The nature of this deconvolving function (called the inverse propagator) is examined; it is a singular function, it is spatially local, and it unsoothes the measured pressure field. An understanding of the nature of the inverse propagator is critical to successful solution of the inverse problem by BEM methods (especially the regularization process), as well as the sucessful development of three-dimensional sound projection methods for sound synthesis. Furthermore, this understanding leads to new insights into the solution of the inverse problem. [Work supported by ONR and NASA.]
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