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A&A 439, 1-22 (2005)
DOI: 10.1051/0004-6361:20052874
On the "injection problem" at the solar wind termination shock
R. Kallenbach1, M. Hilchenbach2, S. V. Chalov3, J. A. le Roux4 and K. Bamert51 International Space Science Institute, Hallerstrasse 6, 3012 Bern, Switzerland
e-mail: kallenbach@soho.unibe.ch
2 Max Planck Institute for Solar System Research, Postfach 20, 37191 Katlenburg-Lindau, Germany
e-mail: hilchenbach@mpae.mpg.de
3 Institute for Problems in Mechanics of the Russian Academy of Sciences, Prospect Vernadskogo 101-1, 117526 Moscow, Russia
e-mail: chalov@ipmnet.ru
4 Institute of Geophysics and Planetary Physics, University of California, Riverside, CA 92521, USA
e-mail: Jakobus@citrus.ucr.edu
5 Institut für Experimentelle und Angewandte Physik, University of Kiel, Leibnizstrasse 19, Kiel 24098, Germany
e-mail: bamert@physik.uni-kiel.de
(Received 14 February 2005 / Accepted 6 April 2005)
Abstract
This article presents an integrated analytical model on
the injection efficiencies of the different ion species of the
Anomalous component of the Cosmic Rays (ACRs) at the solar wind
termination shock. We find that the injection into diffusive
(first-order Fermi) acceleration is dominated by parallel ion
diffusion and not by perpendicular diffusion unless the angle
between the shock normal and the heliospheric magnetic field is almost exactly 90° (
). In steady state the threshold speed for injection into
first-order Fermi acceleration at a not exactly perpendicular
solar wind termination shock - with the Parker shock angle
- adjusts itself self-consistently. Increased
anisotropic ACR flux amplifies Alfvénic turbulence which in turn
suppresses parallel diffusion. It therefore increases the
injection threshold and decreases the ACR flux until equilibrium
is reached. For this equilibrium situation, we estimate the
injection efficiencies of different species of suprathermal ions
at the termination shock. We consider the following
pre-acceleration processes: 1) momentum diffusion in compressional
(ion-acoustic and magnetosonic) turbulence in the upstream
supersonic solar wind and adiabatic cooling during convection to
the termination shock; 2) reflection, transmission, and
acceleration in the electric potential of the termination shock;
and 3) momentum diffusion (stochastic or second-order Fermi
acceleration) in the subsonic solar wind downstream of the
termination shock in the inner heliosheath region. Our model
results are compared to data from instruments on board the SOHO,
ACE, Ulysses, and Voyager spacecraft.
Key words: solar wind -- plasmas -- acceleration of particles -- turbulence -- shock waves -- solar system: general
© ESO 2005
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