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Solar wind ionization state as a coronal temperature diagnostic

Journal Article · · Astrophys. J.; (United States)
DOI:https://doi.org/10.1086/161538· OSTI ID:5016652
The solar wind ionization state is ''frozen'' within a few solar radii of the photosphere, and measurements of the ions at 1 AU can therefore potentially yield information about conditions (e.g., electron temperature) at the base of the coronal expansion. We examine the nature of this freezing-in process, first employing a straightforward interpretation of the interplanetary ionization state to estimate the electron temperature of the coronal freezing-in region by making traditional simplifying assumptions about the coronal expansion, namely, that the electron temperature decreases monotonically with height, that the bulk flow speeds of all charge stages of a given ion species are equal (at a given location) to the proton speed, and that the ion outflow is spherically symmetric. We then investigate the consequences of relaxing these simplifying assumptions and find: (1) The traditional, straightforward interpretation of the interplanetary ionization state tends to underestimate the magnitude of a temperature maximum occurring near the freezing-in radius. (2) The tradional interpretation tends to overestimate (understimate) the actual coronal electron temperature if ion flow speeds in the coronal freezing-in region increase (decrease) with ionization stage. (3) Because it is associated with high-speed, low-density flow, an areal divergence that is faster than that in spherical outflow lowers the ionization state freezing-in level relative to that typical in spherically symmetric expansion, but the ionization states of all species should still freeze above the coronal base.
Research Organization:
Harvard-Smithsonian Center for Astrophysics
OSTI ID:
5016652
Journal Information:
Astrophys. J.; (United States), Journal Name: Astrophys. J.; (United States) Vol. 275:1; ISSN ASJOA
Country of Publication:
United States
Language:
English