A Wave Scattering Theory of Solar Seismic Power Haloes
Shravan M. Hanasoge

TL;DR
This paper introduces a wave scattering theory explaining solar seismic power haloes as a result of magnetic-field-induced mode mixing, supported by simulations and observational data showing increased scattering at higher frequencies and wavenumbers.
Contribution
It presents a novel wave scattering model for solar power haloes, linking magnetic fields to mode mixing and providing simulation and observational evidence.
Findings
High to low modal order scattering channels are favored.
Halo enhancements increase with frequency and wavenumber.
Simulation results align with observed halo magnitudes.
Abstract
Spatial maps of the high-pass frequency filtered time-averaged root-mean-squared (RMS) Doppler velocities tend to show substantial decrements within regions of strong field and curiously, randomly distributed patches of enhancement in the vicinity. We propose that these haloes or enhancements are a consequence of magnetic-field-induced mode mixing (scattering), resulting in the preferential powering of waves that possess strong surface velocity signatures (i.e. scattering from low to high wavenumbers). Evidently, this process can occur in the reverse, and therefore in order to determine if the haloes are indeed caused by mode mixing, we must answer the question: {\it how are acoustic waves scattered by magnetic fields?} Through simulations of the interactions between waves and sunspots and models of plage, we demonstrate that the high to low modal order scattering channels are favoured.…
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