Obtaining Potential Field Solution with Spherical Harmonics and Finite Differences
Gabor Toth, Bart van der Holst, and Zhenguang Huang

TL;DR
This paper introduces two improved methods for calculating solar magnetic potential fields from magnetogram data, addressing artifacts and inaccuracies in traditional spherical harmonics approaches, especially near the poles.
Contribution
It presents a new finite difference iterative solver (FDIPS) and discusses remeshing strategies to enhance potential field solutions from solar magnetograms.
Findings
Finite difference method reduces artifacts compared to spherical harmonics.
Remeshing magnetograms improves accuracy near polar regions.
FDIPS code is publicly available for broader use.
Abstract
Potential magnetic field solutions can be obtained based on the synoptic magnetograms of the Sun. Traditionally, a spherical harmonics decomposition of the magnetogram is used to construct the current and divergence free magnetic field solution. This method works reasonably well when the order of spherical harmonics is limited to be small relative to the resolution of the magnetogram, although some artifacts, such as ringing, can arise around sharp features. When the number of spherical harmonics is increased, however, using the raw magnetogram data given on a grid that is uniform in the sine of the latitude coordinate can result in inaccurate and unreliable results, especially in the polar regions close to the Sun. We discuss here two approaches that can mitigate or completely avoid these problems: i) Remeshing the magnetogram onto a grid with uniform resolution in latitude, and…
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