We have considered a model of the evolution of the pick-up ion distribution including both the pre-shock and the post-shock regions of the heliosphere. The pre-acceleration of the pick-up ions by the turbulence in the pre-shock solar wind was taken into account. The results suggest that the energetic ion spectrum near the termination shock may, for the energies below 50-100 keV, be determined by the shock-modified pre-accelerated pick-up ion spectrum rather than the power-law spectrum expected from the shock acceleration.
The ion flux at the shock obtained in the model is at low energy (up
to 60-70 keV) significantly higher than the extrapolated ACR power law
spectrum. In result, also the ENA flux from the pick-up ions is high and
agrees with the observations by CELIAS/HSTOF (the
alternative interpretation, assuming that the ENA come from the
shock-accelerated ACR particles, may have problems with explaining the
observed ENA flux level: see Czechowski et al. 2001). The directional
dependence of the ENA flux is also in agreement with observations, with
the flux intensity peaks from the (approximately) anti-apex
direction. This may be an indication that the ENA flux comes from
the post-shock region, although there is a possible alternative (Kota
et al. 2001) connected with the CIR accelerated ions interacting by
charge-exchange with the helium atoms in the region where the helium
density is increased due to gravitational focusing (the helium cone).
Although the errors are large, the data suggest the anti-apex to apex
flux ratio lower than calculated. This may imply that the model
of the heliosphere used in the calculations (Fahr et al. 2000; Czechowski et al. 2001) should be
modified. Another
possibility is that a part of the ENA flux comes from another
source, with no peaks from the anti-apex direction.
The results are consistent with the "normal turbulence'' case, with the
amplitude of the magnetic field perturbations evolving adiabatically
(
case). The other version of the model
(persisting source of the perturbations,
)
does
not fit the ENA data, but it is not realistic enough in any case (too
large total energy in the PUI spectrum).
The calculated ENA energy spectrum is steeper than the spectrum deduced from CELIAS/HSTOF data. The experimental spectrum is, however, sensitive to assumptions about the proton energy spectrum and the transmission function. Also, the PUI model disregards the effects of diffusive shock acceleration, which can in fact become important in the considered energy range and make the proton and the ENA spectrum less steep.
The energy range of the CELIAS/HSTOF observations (58-88 keV) coincides with the region where the PUI and PUI ENA spectrum decrease very fast (for the normal turbulence case) and other contributions may appear. The forthcoming data from INCA/Cassini (Krimigis et al. 2000) and HENA/Image (Mitchell et al. 2000; first results: Roelof 2000) which should include also the lower energy region where the model predicts high ENA flux, are therefore of particular interest.
Acknowledgements
A.C. is grateful for financial support within the framework of a Polish-German cooperation (project 436 POL 113/80/0) and acknowledges support from KBN grant 8 T12E 029 20. A.C. also wishes to thank the Max-Planck-Institut für Aeronomie for hospitality.
Copyright ESO 2001