Exploring spectropolarimetric inversions using neural fields. Solar chromospheric magnetic field under the weak-field approximation

TL;DR

This paper introduces a neural field-based method for spectropolarimetric inversions that leverages spatiotemporal coherence to improve magnetic field reconstruction in the solar chromosphere, especially under the weak-field approximation.

Contribution

It presents a novel neural field approach for spectropolarimetric inversions that regularizes solutions across space and time, enhancing fidelity over traditional pixel-wise methods.

Findings

Improved magnetic field vector reconstruction, especially the transverse component.

Implicit regularization increases effective signal-to-noise ratio.

Potential for depth-stratified inversions with reduced free parameters.

Abstract

Full-Stokes polarimetric datasets, originating from slit-spectrograph or narrow-band filtergrams, are routinely acquired nowadays. The data rate is increasing with the advent of bi-dimensional spectropolarimeters and observing techniques that allow long-time sequences of high-quality observations. There is a clear need to go beyond the traditional pixel-by-pixel strategy in spectropolarimetric inversions by exploiting the spatiotemporal coherence of the inferred physical quantities. We explore the potential of neural networks as a continuous representation of the physical quantities over time and space (also known as neural fields), for spectropolarimetric inversions. We have implemented and tested a neural field to perform the inference of the magnetic field vector (approach also known as physics-informed neural networks) under the weak-field approximation (WFA). By using a neural field to describe the magnetic field vector, we can regularize the solution in the spatial and temporal domain by assuming that the physical quantities are continuous functions of the coordinates. We investigated the results in synthetic and real observations of the Ca II 8542 A line. We also explored the impact of other explicit regularizations, such as using the information of an extrapolated magnetic field, or the orientation of the chromospheric fibrils. Compared to the traditional pixel-by-pixel inversion, the neural field approach improves the fidelity of the reconstruction of the magnetic field vector, especially the transverse component. This implicit regularization is a way of increasing the effective signal-to-noise of the observations. Although it is slower than the pixel-wise WFA estimation, this approach shows a promising potential for depth-stratified inversions, by reducing the number of free parameters and inducing spatio-temporal constraints in the solution.