Remote sensing of H from Ulysses and Galileo

W. Pryor, I. Stewart, K. Simmons, M. Witte, J. Ajello, K. Toskiba, D. McComas, D. Hall

Research output: Contribution to journalArticle

7 Scopus citations

Abstract

We model interplanetary H Lyman-α (Lα) observations from Galileo UVS (Ultraviolet Spectrometer) and EUVS (Extreme Ultraviolet Spectrometer) (Hord et al., 1992) and the Ulysses interstellar neutral gas (GAS) instrument (Witte et al., 1992). EUVS measurements near solar maximum (max) in 1990-1992 have a peaked brightness maximum upwind due to a rather isotropic solar wind charge-exchange ionization pattern (A=0-0.25). GAS measurements from solar minimum (min) in 1997 have a plateau in the upwind direction that we model using Ulysses SWOOPS (solar wind plasma experiment) solar min data on solar wind density and velocity at different heliographic latitudes. The isotropic ionization pattern deduced from EUVS at solar max may be consistent with recent SWOOPS results (McComas et al., 2000b, c) that high speed solar wind is absent at high latitudes during solar max. Galileo and Ulysses Lα data favor higher H temperatures (15 000-18 000 K) than previous models.

Original languageEnglish (US)
Article number338878
Pages (from-to)393-399
Number of pages7
JournalSpace Science Reviews
Volume97
Issue number1-4
DOIs
StatePublished - Jan 1 2001
Externally publishedYes

All Science Journal Classification (ASJC) codes

  • Astronomy and Astrophysics
  • Space and Planetary Science

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    Pryor, W., Stewart, I., Simmons, K., Witte, M., Ajello, J., Toskiba, K., McComas, D., & Hall, D. (2001). Remote sensing of H from Ulysses and Galileo. Space Science Reviews, 97(1-4), 393-399. [338878]. https://doi.org/10.1023/A:1011870210363