Improving the Alfvén Wave Solar Atmosphere Model Based on Parker Solar Probe Data

• Published in: The Astrophysical journal Vol. 925; no. 2; pp. 146 - 156
• Main Authors: van der Holst, B., Huang, J., Sachdeva, N., Kasper, J. C., Manchester IV, W. B., Borovikov, D., Chandran, B. D. G., Case, A. W., Korreck, K. E., Larson, D., Livi, R., Stevens, M., Whittlesey, P., Bale, S. D., Pulupa, M., Malaspina, D. M., Bonnell, J. W., Harvey, P. R., Goetz, K., MacDowall, R. J.
• Format: Journal Article
• Language: English
• Published: Philadelphia The American Astronomical Society 01.02.2022; IOP Publishing
• Subjects: Alfven waves; Astrophysics; Atmosphere; Atmospheric models; Corona; Coronal heating; Equatorial regions; Heating; Heliosphere; Magnetic fields; Magnetohydrodynamics; Modelling; Perihelions; Photosphere; Polarity; Protons; Solar atmosphere; Solar corona; Solar probes; Solar surface; Solar wind; Turbulence; Wave dissipation
• ISSN: 0004-637X; 1538-4357
• DOI: 10.3847/1538-4357/ac3d34

Abstract In van der Holst et al. (2019), we modeled the solar corona and inner heliosphere of the first encounter of NASA’s Parker Solar Probe (PSP) using the Alfvén Wave Solar atmosphere Model (AWSoM) with Air Force Data Assimilative Photospheric flux Transport–Global Oscillation Network Group magnetograms, and made predictions of the state of the solar wind plasma for the first encounter. AWSoM uses low-frequency Alfvén wave turbulence to address the coronal heating and acceleration. Here, we revise our simulations, by introducing improvements in the energy partitioning of the wave dissipation to the electron and anisotropic proton heating and using a better grid design. We compare the new AWSoM results with the PSP data and find improved agreement with the magnetic field, turbulence level, and parallel proton plasma beta. To deduce the sources of the solar wind observed by PSP, we use the AWSoM model to determine the field line connectivity between PSP locations near the perihelion at 2018 November 6 UT 03:27 and the solar surface. Close to the perihelion, the field lines trace back to a negative-polarity region about the equator.