A boundary integral method for wave scattering in a heterogeneous medium with a moving obstacle

arXiv:2605.095007.6
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This work extends boundary integral methods to heterogeneous and moving-boundary settings, addressing a known bottleneck in computational wave scattering for applications like acoustics and electromagnetics.

The paper proposes a time-domain boundary integral method for wave scattering in heterogeneous media with moving obstacles, avoiding volumetric discretization. Numerical experiments demonstrate stable performance up to Mach 0.9 and accurate capture of refractive and Doppler effects.

We propose a time-domain boundary integral method to model linear wave propagation with refractive, focusing, and Doppler effects arising from medium heterogeneities and moving obstacles. In contrast to existing techniques, our method avoids volumetric discretization and yields a formulation posed only on the boundary of the obstacle. We combine two classical ingredients: a geometric--optics parametrix to capture leading-order behavior at propagating wavefronts, and a ray-based characterization of the distorted causal geometry. The former provides a framework for defining layer potentials and deriving the associated boundary integral equations, while the latter enables a pure boundary-only formulation. Taken together, these ingredients extend existing numerical techniques for the homogeneous, fixed-boundary case to the heterogeneous, moving-boundary setting, with appropriate modifications to capture the discrete causal structure arising from the intersection of distorted light cones with the worldsheet of the moving boundary. Numerical experiments demonstrate the ability of the method to resolve Doppler effects from moving obstacles, including a rotating turbine configuration, with stable performance up to Mach 0.9. In heterogeneous media, the method captures strong refractive effects from spherical inclusions: wave propagation wrapping around a gas bubble in water, and defocusing from a hot fireball rising through a stratified atmosphere.

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