WawHelioGlow: A Model of the Heliospheric Backscatter Glow. II. The Helioglow Buildup and the Potential Significance of the Anisotropy in the Solar EUV Output

• Published in: The Astrophysical journal. Supplement series Vol. 254; no. 1; pp. 17 - 36
• Main Authors: Kubiak, M. A., Bzowski, M., Kowalska-Leszczynska, I., Strumik, M.
• Format: Journal Article
• Language: English
• Published: Saskatoon The American Astronomical Society 01.05.2021; IOP Publishing
• Subjects: Anisotropy; Astrosphere interstellar medium interactions; Backscatter; Backscattering; Distribution functions; Fluorescence; Gas density; Heliosphere; Interplanetary gas; Interplanetary scintillation; Interstellar atomic gas; Interstellar gas; Interstellar medium; Neutral gases; Phases; Solar cycle; Solar EUV; Solar extreme ultraviolet emission; Solar system; Solar wind
• ISSN: 0067-0049; 1538-4365
• DOI: 10.3847/1538-4365/abeb78

Abstract The helioglow is the fluorescence of interstellar atoms inside the heliosphere, where they are excited by the solar EUV. Because the mean free path between collisions for interstellar gas is comparable to the size of the heliosphere, the distribution function of this gas inside the heliosphere strongly varies in space and with time and is non-Maxwellian. Coupling between realistically modeled solar factors and the distribution function of interstellar neutral gas is accounted for in a helioglow model that we have developed. WawHelioGlow is presented in the accompanying Paper I. Here, we present the evolution of the gas density, solar illumination, helioglow source function, and other relevant parameters building up the helioglow signal for selected lines of sight observed at 1 au. We compare these elements for various phases of the solar cycle, and we present the sensitivity of the results to the heliolatitudinal anisotropy of the solar EUV output. We assume a realistic latitudinal anisotropy of the solar wind flux using results from the analysis of interplanetary scintillations. We compare the simulated helioglow with selected maps observed by the SOHO/SWAN instrument. We demonstrate that WawHelioGlow is able to reproduce fundamental features of the sky distribution of the helioglow. For some phases of the solar cycle, the model with solar EUV output anisotropy better reproduces the observations, while for other phases, no EUV anisotropy is needed. In all simulated cases, the solar wind anisotropy following insight from interplanetary scintillation measurements is present.