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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 105, NO. A3,
PAGES 5189–5200,
2000
Heliopause imaging in EUV: Oxygen O+ ion 83.4-nm resonance line emission
Mike Gruntman
Department of Aerospace Engineering, University of Southern California, Los Angeles
Hans J. Fahr
Institut für Astrophysik und Extraterrestrische Forschung, Universität Bonn, Bonn, Germany
Abstract
We explore the possibility of remote, from 1 AU, study of the heliopause by an observer outside the geocorona. We argue that
the heliopause, a boundary that separates the solar wind and the galactic plasma of the local interstellar medium (LISM),
can be imaged by detecting solar extreme ultraviolet (EUV) radiation reflected by interstellar ions. Such EUV imaging would
map the heliopause and provide important insight into its three-dimensional structure and the LISM parameters as well. We
consider heliopause mapping in the oxygen O+ ion resonance line (83.4 nm); imaging in the helium He+ ion line (30.4 nm) will be considered in a future article. We show
that the expected heliopause brightness map at 83.4 nm is essentially different from that of the foreground glow of the solar
wind O+ pickup ions. The interstellar plasma glow is brighter in the upwind (with respect to the interstellar wind) direction,
while the pickup ion glow dominates in the downwind direction. The spectral characteristics of the radiation scattered by
the LISM plasma and by the pickup ions are significantly different. The all-sky images at 83.4 nm are highly sensitive to
the ionization state of the LISM and would allow one to probe the asymmetry of the interstellar magnetic field. We briefly
discuss the experimental requirements to heliopause EUV mapping, which would require 3 orders of magnitude improvement in
instrumentation sensitivity. This is a challenging but not impossible task.
Received 20
September
1999;
accepted 17
November
1999.
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Citation: Gruntman, M., and H. J. Fahr
(2000),
Heliopause imaging in EUV: Oxygen O+ ion 83.4-nm resonance line emission,
J. Geophys. Res.,
105(A3),
5189–5200.
Copyright 2000 by the American Geophysical Union.
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