Abstract. Current controversy exists in the interpretation and modeling of helioseismic signals in and around magnetic regions like sunspots. Unresolved issues include the dependence of the sign of both the inferred flows and wave speed on the type of filtering used, and the discrepancy between the relatively deep two-layer wave-speed models derived from standard time-distance methods and shallow, positive wave-speed models derived using forward models which include effects of mode conversion To make full use of the year-round, almost limb-tolimb, coverage provided by the Solar Dynamics Observatory, an efficient and reliable inversion method incorporating possible magnetic effects and the currently unexplained sensitivity to methodology is critical. . This behavior has also been qualitatively (and in some cases remarkably quantitatively) reproduced with artificial data -derived from hydrostatic models [7], magnetostatic models [8], and MHD models [9] -in which no slower layer is present. In contrast to measurements made using phase-speed filters, travel-time perturbations derived using ridge filters are exclusively negative (implying faster wave speeds) in sunspots [4]. A number of forward models, including some with magnetic fields, provide evidence for shallow, positive wave speed perturbations below sunspots [10]. Thus, considerable uncertainty remains in the inference of the wave-speed structure below sunspots. However, an efficient, robust inverse method which includes the effects of magnetic fields has not yet been developed.
Introduction