Issue |
A&A
Volume 521, October 2010
|
|
---|---|---|
Article Number | A1 | |
Number of page(s) | 8 | |
Section | The Sun | |
DOI | https://doi.org/10.1051/0004-6361/200913638 | |
Published online | 01 October 2010 |
Comparison of different analytic heliospheric magnetic field configurations and their significance for the particle injection at the termination shock
K. Scherer1 - H. Fichtner1 - F. Effenberger1 - R. A. Burger2 - T. Wiengarten1
1 - Institut für Theoretische Physik IV, Ruhr Universität Bochum, 44780 Bochum, Germany
2 -
Unit for Space Physics, North-West University, 2520 Potchefstroom, South Africa
Received 11 November 2009 / Accepted 19 May 2010
Abstract
Context. Heliospheric magnetic field configurations are
relevant on a large scale for the transport of cosmic rays, especially
for injecting possibly pre-accelerated particles into the Fermi-I
acceleration process of cosmic rays.
Aims. We compare four analytically described fields by
calculating the scalar product between their vectors and the
corresponding vectors of the Parker spiral field. Because the injection
efficiency at the termination shock is highly sensitive to the local
inclination of the upstream magnetic fields with respect to the shock
normal, we discuss the probability that pick-up ions are injected into
the Fermi-I process.
Methods. We extend the previous work comparing different
analytically described heliospheric magnetic fields: the Parker and
hybrid Fisk field and modifications of both. Because the Fisk-like
configurations are only present during periods of low to moderate solar
activity, we restrict ourselves to this case by including high-speed
streams over the ecliptic and low-speed flow in the latter.
In addition, we extend the analysis from an analytic approximation
to a numerically computed termination shock surface.
Results. We find that no strong differences in the injection
efficiency can be expected for the four field configurations despite
significant structural differences inside the termination.
Conclusions. Consequently, the injection efficiency is largely insensitive to the large-scale heliospheric magnetic field configuration.
Key words: magnetic fields - solar wind - acceleration of particles
1 Introduction
The heliospheric magnetic field (HMF) is important for the transport of cosmic rays and especially for the injection of pickup ions (PUIs) into the Fermi-I acceleration process at the termination shock to become anomalous cosmic rays. There are several approaches to describing this field analytically, starting with Parker (1958), who assumed a freezing-in of the magnetic field into the solar wind, which leads to an Archimedian spiral, except at the poles where the field is purely radial. To avoid such a radial field line over the poles, Jokipii & Kota (1989) added a small correction term to the latitudinal component. Similarly, Smith & Bieber (1991) added an additional azimuthal contribution (see also Burger 2005) to describe the under- and over-winding of the HMF close to the ecliptic. Later, Fisk (1996) modeled the HMF and included the footpoint motion of field lines on the Sun's differentially rotating surface. The assumption of a constant solar wind speed in this field, was abandoned by Schwadron (2002), see also Schwadron et al. (2008). For a deeper discussion of these HMFs, see Burger & Hitge (2004), Burger (2005), and Burger et al. (2008).
The existing observational data (see e.g. Mordvinov 2008; Mursula 2007; Ebert et al. 2009; Roberts et al. 2007; Murphy et al. 2002; Burlaga et al. 2002) and corresponding modeling (e.g. Burger & Hitge 2004; Burger 2005; Giacalone & Jokipii 2004; Burger et al. 2008; Schwadron & McComas 2005; Ferreira et al. 2007; Giacalone et al. 2006) that can be used to analyze the asymmetry of the HMF have not yet convincingly settled the debate over which of the fields is closest to reality. For a more detailed discussion of the difficulties to distinguish between different fields on the basis of in situ measurements of magnetic fields, see the recent paper by Hitge & Burger (2010).
A direct and meaningful comparison of three-dimensional vector fields
is not a straightforward task. We discuss the angle between the Parker
field and the above-mentioned fields with respect to heliocentric
distance r, latitude ,
and longitude
.
Furthermore, we use the analytic representation of the different magnetic tilt angles against
,
and
.
We compare the global structure of the four analytic HMF models
mentioned above, especially at the termination shock, and discuss the
consequences for particle injection. Because this injection of PUIs at
the termination shock into the Fermi-I acceleration process strongly
depends on the magnetic tilt angle between the magnetic field and the
shock surface normal, we analyze the tilt angle for the magnetic field
configurations. This is first done in the same way as in Fahr et al. (2008) and Scherer & Fahr (2009), by describing the 3D-shape of the termination
shock by the surface of a triaxial ellipsoid fitted to a shock, which was numerically computed by Borrmann & Fichtner (2005). Second, we extend this analysis by using the actual shock surface
rather than its analytical approximation.
In Sect. 2 we summarize the analytic descriptions of the different HMFs, and in Sect. 3 we discuss the differences of their direction angles with respect to the Parker field. In Sect. 4 we briefly introduce a triaxial ellipsoid as an analytic approximation of the termination shock (Scherer & Fahr 2009) and a numerical representation of it. Finally in Sect. 5 we briefly discuss consequences for particle injection and propagation, as well as for the fluxes of energetic neutral atoms (ENAs) produced by PUIs (see Scherer & Fahr 2003; Heerikhuisen et al. 2008; Sternal et al. 2008a).
2 The different heliospheric magnetic fields
Modeling the time-dependent heliosphere in three dimensions requires
adequate modeling of solar-cycle related high-speed streams in the
heliosphere. This modeling includes the interaction of interstellar
protons and neutral gas with the supersonic solar wind protons (e.g. Borrmann & Fichtner 2005) and involved magnetic fields (Ratkiewicz 2006; Pogorelov et al. 2009; Opher et al. 2006), and also includes both cosmic rays (Fahr et al. 2000; Ferreira et al. 2007) and time-dependent dynamical effects of the solar activity cycle (Izmodenov et al. 2008; Scherer & Ferreira 2005). Here we do not follow up on these topics, but refer the reader to Müller et al. (2008),
where some of these models are compared. We just note that, during
solar maximum conditions the entire volume of the heliosphere is filled
with low-speed solar wind, while during solar minimum conditions, a
high-speed solar wind evolves over the poles,
i.e. above/below
the ecliptic, and persists over a period of about three years as observed by the Ulysses spacecraft (see McComas et al. 2003).
Generally, the HMF, ,
in spherical polar coordinates, can be described by its radial
-, longitudinal
-, and latitudinal
-components:
with the spherical polar coordinate unit vectors, and


2.1 Analytic HMF representations
The most commonly assumed HMF, the so-called Parker field
(Parker 1958), is a modified dipole field of the Sun, with a radial component decreasing like r-2, and a latitude-dependent azimuthal component decreasing with r-1 vanishing with
over the heliospheric poles (e.g. Parker 1958), see also for observational data Forsyth et al. (2002). To avoid the r-2 behavior at the heliospheric poles, Smith & Bieber (1991) added a small term decreasing with r-1 to the
-component, resulting in the modified Parker field
.
Taking the differential rotation of the Sun's surface into account, Fisk (1996) modeled the motion of the HMF footpoints at the Sun. Due to that motion, the so-called Fisk field
also has a
-component
that is not present in the other two described HMFs. Because the Fisk
field is restricted to a constant solar wind speed, Schwadron (2002); Schwadron et al. (2008)
extended it to the case where the solar wind speed can be
latitude-dependent, i.e. for high-speed streams at high latitudes,
and low-speed flow in the ecliptic. The latter is called the modified
Fisk field
.
The Fisk field is used in the hybrid representation by Burger & Hitge (2004),
where a Parker-like field dominates in the ecliptic and over the poles,
while in between a Fisk-like field contributes most to the HMF.
The analytic representations of these fields are given by:
- -
- the Parker field
:
- -
- the modified Parker field
(
10-2):
- -
- the hybrid Fisk field
:
- -
- and its modification by Schwadron (2002)
where the solar wind speed can be a function of latitude:
with b0=B(r0)r02, B(r0) the magnetic field strength in







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||
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||
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(5) |
describes the relative contributions of the Fisk and Parker fields to the HMF; e.g., for Fs = 0 it is a pure Parker field, while for Fs= 1 it is a pure Fisk field as defined by Burger & Hitge (2004), but see also Burger et al. (2008) for a different definition. The values for the angle between the rotational axis and the so-called virtual axis of the Sun





The function Fs and its derivative - required for the divergence-free constraint of the magnetic field - is presented in Fig. 1, where it can be seen that the derivative is large close to the poles and the ecliptic, so, the -component
of the hybrid Fisk fields only vanishes directly at the poles and in
the ecliptic. For a Parker field with constant solar wind speed
km s-1, the parameter
AU-1, while for a Fisk field a constant solar wind speed
km s-1 is commonly taken (Fisk 1996; Burger & Hitge 2004; Burger 2005; Burger et al. 2008), and at 1 AU the value
.
![]() |
Figure 1:
The transition function
|
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![]() |
Figure 2:
The Hammer projection (view from the Sun outwards) of the angle |
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![]() |
Figure 3:
Left panel: the north (left) and south (right) pole of the
angle |
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The low-speed solar wind typically has
km s-1, while the high-speed wind in polar regions (i.e. at latitudes above/below
)
has twice that value
(800 km s-1). Thus during solar minimum conditions the k at high latitudes has to be reduced by a factor two. To avoid an unsteady sharp transition at
,
we introduce the following function
:
where




In the next section we discuss the differences between these fields.
3 The angle with respect to the Parker field
The Parker-like fields and the modified hybrid Fisk field are
calculated using high/low-speed streams, while a constant solar wind
speed
km s-1
is chosen for the hybrid Fisk field. To compare three-dimensional
vectors we can either do it by components or use the angle relative to
a known structure. Other options may exist, but we prefer the latter
and will use the Parker field as the known structure, because it
consists of Archimedian spirals with winding
angles decreasing towards the heliospheric poles. In Figs. 2 and 3 we have plotted the angles
between the Parker field
and the other three fields
and
,
i.e.,
(with




With the procedure described above we lose the information on field
vector orientations. To maintain the three-dimensional
information, the scalar product can be calculated with respect to the
unit vectors, for instance in spherical coordinates
,
which will be helpful when studying the three-dimensional propagation
of cosmic rays, e.g. the elements of the corresponding
diffusion tensor.
In both panels of Fig. 2, the modified Parker field is shown in the middle column. For small heliocentric distances, the Smith-Bieber term in the -component is large enough to contribute to the scalar product in Eq. (7), while at greater distances, it vanishes, and both magnetic field vectors
and
mainly have a
-component,
hence are parallel. Therefore, the small non-zero angles faintly
visible in the top four panels of the middle columns of Figs. 2 vanish with increasing distances. Because the modified Parker field
behaves almost like the Parker field
,
it is not further discussed in the following.
The hybrid Fisk field
is shown in the left columns of both panels of Fig. 2, while the modified hybrid Fisk field
is presented in the right columns. In Fig. 3 the north pole (i.e.
)
and south pole (
)
are displayed for the hybrid Fisk
and the modified hybrid Fisk
field, respectively.
At 1 AU, the angles
between the Fisk-like fields
at low latitudes and the Parker field
are small except in some confined regions close to the equator. These
differences are due to the longitudinal structure of the former which
is amplified by the derivative term of the transition function near the
equatorial plane, see also Fig. 1. The areas at the poles with large angles
(see also Fig. 3) increase with increasing heliocentric distance r up to an asymptotic size of about
.
The highest values of
occur at distances of approximately 50 AU. The angle is slightly
greater for the modified Fisk field. Due to the similarity of the
Fisk and the Parker fields at small heliocentric distances and high
latitudes (see also Sternal et al. 2008b)
for distances r<5 AU. At heliocentric latitudes below
the angles
are generally limited to about
for all distances. The modified Fisk-field
shows bands around the transition regions at
in which the angle
shows a
``chaotic'' behavior, i.e. varies strongly on small spatial scales.
With increasing distances, the Fisk-like fields show stripes from pole
to pole in which they are almost parallel to the Parker field,
i.e.
.
As a consequence of the radial variation of the longitudinal
structure of the Fisk-like fields, these stripes ``rotate''
anti-clockwise with increasing heliocentric distance r; i.e. with increasing distance the parallelism is shifted to different longitudes. In the right panel of
Fig. 3 it can be seen that such a ``
-rotation'' exceeds
per AU for the hybrid Fisk field
and is a little less for the modified hybrid Fisk field
.
In this figure the polar regions of the fields
are
shown, the south and north poles of
in the left two columns of each panel, and those of
in the two right columns. These fields exhibit a north-south asymmetry
at a given distance as a consequence of the tilt of the magnetic axis
relative to the rotational axis. To illustrate the radial
variation of the angle
,
a distance range around the polar termination shock is shown in 1 AU steps in the right panel of Fig. 3. One can easily see the strong radial dependence of
implying an equally strong dependence of the injection efficiency on
the location and dynamics of the termination shock.
As a further illustration, the
large scale variation in
is visualized with a meridional cut displayed in Fig. 4.
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Figure 4: The angle between the hybrid Fisk- and Parker-field in a meridional plane, the large spatial variation in the regions where the Fisk-type field is dominant. |
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From the above discussion, one should expect a north-south as well as an east-west asymmetry for Fisk-like field configurations at the different positions of the termination shock, as observed by Voyager 1 and 2 spacecraft, i.e. at 94 and 84 AU, respectively (Stone et al. 2008,2005). Thus, the recent Voyager observations (Richardson et al. 2008), which suggest that the termination shock may be North-South-asymmetric, should not be a surprise.
The small asymmetry is interpreted by the cited authors as a deviation of the interstellar magnetic field vector from the inflow direction. However, the latter mainly affects the shape of the heliopause (Opher et al. 2009; McComas et al. 2009a; Schwadron et al. 2009) and that of the bow shock, but that of the termination shock only weakly (Pogorelov et al. 2008). In view of the above discussion, the observed asymmetry may partly be explained by that of the Fisk-type fields, which need to be incorporated into MHD models of the heliosphere-interstellar medium interaction. In any case, the termination shock is not only ``geometrically'' asymmetric - as observed by the Voyagers, see, e.g., Stone et al. (2008) - but it also shows a ``magnetic'' asymmetry, i.e. a north-south difference in the angle between the Fisk-like fields and the shock normal as is quantified in the following.
4 Representation of the heliospheric termination shock
For the shock surface we use the 3D-model of the solar wind and interstellar medium interaction during solar minimum by Borrmann & Fichtner (2005) including high speed streams over the polar regions. The intersections of the shock surface with the equatorial x-y-plane and the meridional x-z-plane are shown in Fig. 5.
4.1 Analytic triaxial ellipsoid
![]() |
Figure 5: The fit (red crosses) to the model results (green crosses) by Borrmann & Fichtner (2005). The equatorial plane is shown in the left panel and in the right the meridional one. |
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To study the effects of the different fields
qualitatively at the termination shock, we first use an analytical representation of the shock surface. Therefore, we follow the
description by Scherer & Fahr (2009)
and only briefly repeat the main idea that the three-dimensional
termination shock surface is described as a triaxial ellipsoid
(Fig. 5). The parameters of the ellipsoid are a=195, b=170,
,
so that the eccentricities are given by
,
,
and the semi-axes a,b,c are oriented along the x,y,z-axes in a Cartesian coordinate system, respectively. The interstellar medium flows from the positive to the negative x-axis, with the ecliptic in the x-y-plane, and the polar regions are directed along the z-axis. In this analytic approach it is straightforward to calculate the normal vector
to the shock surface needed for the computation of the magnetic tilt angle.
4.2 Numerical model
The deviations of the fitted ellipsoid from the actual shock surface are relatively large in the tail regions, see Fig. 5.
Therefore, we calculated the normal vector
to the numerically determined shock surface in the following way: we
computed the local orientation of the surface using a midpoint and
pairs of its neighboring points. From eight neighbors of a given
surface point, we obtained eight representations of the normal vector.
After averaging these representations, we derived a good approximation
of the normal vector
at this location.
In the following we compare the magnetic tilt angles for the large-scale magnetic field structures using both the analytically and numerically obtained normal vectors.
![]() |
Figure 6: The magnetic tilt angle of the Fisk ( left) and the modified Fisk field ( right) at the analytically approximated termination shock. |
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Figure 7: The tilt angle for the Parker field in the analytic representation is shown in the upper left panel. For the numerical case the tilt angle of the Parker field is shown in the upper right, for the Fisk field in the lower left, and for the modified Fisk field in the lower right. |
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5 The magnetic tilt angle
We determine the tilt angles
as the scalar product between the shock normal
and the Fisk-like magnetic fields
at the shock surface, while those for the Parker
field are discussed in detail in Scherer & Fahr (2009). The former are presented in Fig. 6 for the analytically and in Fig. 7 for numerically calculated normal vectors, respectively. In Fig. 6 it can be seen that a strip from the poles through the nose direction around
,
like in the Parker field, exists for the Fisk-like fields where it takes values about
.
As was shown by Scherer & Fahr (2009) the magnetic tilt angle
can be as low as
in the heliospheric flanks for the Parker field
,
and exhibits a modest ``east-west'' asymmetry as a result of the different orientation of the field and
the shock normal. A similar behavior can be observed in Fig. 6 for the Fisk-like fields. The tilt angles for the fields
show a ``background'' variation related to the
varying distances r
to the ellipsoid surface. The ``filamentary'' structures obtained for
the analytical representation of the shock surface are a consequence of
the complicated field geometry, however, it is only weakly visible
in the numerical case, because the resolution of the underlying
numerical model is limited. In that case, the differences between
the hybrid Fisk field
and the Parker field
are small (see upper left panel of
Fig. 7) and are only visible in the analytical case as a fine structure. The modified hybrid Fisk field
shows
an additional band of highly varying tilt angles in the transition
region from the slow to the fast solar wind in bands around
.
The tilt angle of the Fisk-like fields is quite similar to that of the Parker field, so, the injection efficiency of the PUIs into the ACR acceleration process is quite similar to what is described in Scherer & Fahr (2009). The exception is the modified hybrid Fisk field, which shows the band-like structure, in which the magnetic tilt angle changes strongly on small spatial scales, allowing for alternating higher or lower injection efficiencies in this structure (see Fig. 7, right panel).
Because the Parker field
is the prevailing heliospheric magnetic field for solar maximum conditions, solar activity effects are not considered here. Scherer & Fahr (2009)
already showed, however, that the injection conditions are fairly good
across the entire termination shock surface during solar maximum.
5.1 Implications for cosmic ray propagation
The influence of Fisk-like fields
on
the propagation of energetic particles in the heliosphere, and
especially on the acceleration processes in the heliosheath,
is not easily accessible, because these fields change with
heliocentric distance, longitude, and latitude and, therefore, the
corresponding diffusion tensor will change analogously. In order
to quantitatively treat the cosmic ray transport for which gradient and
curvature drifts, as well as spatial
diffusion are significant processes, it is necessary to calculate
a supposedly fully anisotropic diffusion tensor and to re-derive the
drift terms for the different field configurations. This would go far
beyond the scope of this paper, so the reader is referred to Burger et al. (2008) and Sternal et al. (2008b).
Instead, we briefly address possible effects that an enhanced PUI
production may have on the global distribution of Energetic Neutral
Atoms (ENAs).
5.2 Implications for ENA fluxes
The injection efficiency describes the fraction of PUIs at the termination shock, which can be accelerated to ACRs. As discussed above, the injection efficiency of PUIs into the Fermi-I process producing the anomalous component is expected to be structured only weakly depending on the magnetic field configuration (see Fig. 7).
If the injection efficiency in a given direction is sufficiently high, there might be lower ENA fluxes at PUI energies from there because of the ``extraction'' of PUIs to the ACR component. The effect of the above-mentioned fine structure, however, might be too small to be detected with the IBEX mission (McComas et al. 2009b).
6 Conclusions
We calculated the angles
between the modified Parker field
,
the Fisk field
,
the modified Fisk field
and the Parker field
and discussed their variations and deviations from each other with heliocentric distance, latitude, and longitude. The largest
occur at high latitudes. Due to the longitudinal structure of the
Fisk-like fields there are, however, also stripes at certain longitudes
reaching from pole to pole, where the fields are parallel to the
Parker field (i.e.
). These stripes rotate anti-clockwise with increasing heliocentric distance.
We continued to expand our previous large scale three-dimensional semi-analytic approach to study the tilt angle between the vectors of different magnetic fields and the shock surface normal. The main result is that the differences in the injection efficiency for the Parker field and for its modification, as well as for the hybrid Fisk field are negligible. We want to point out that the hybrid Fisk field is only consistent with a constant solar wind speed, while all other fields studied here (Parker-like and modified hybrid Fisk fields) can take the fast solar wind streams into account at high latitudes during solar minimum conditions.
For the
fields
we conclude that, during solar minimum conditions, the favorable
acceleration regions are always the flanks of the 3D-heliosphere. This
finding is consistent with the measurements by both Voyager spacecraft,
which did not find any evidence
of ACR acceleration closer to the upwind direction.
We summarize the main conclusions drawn from these above considerations of these magnetic fields in the following:
- 1.
- For Fisk-like fields
there exists an east-west and north-south asymmetry.
- 2.
- The deviations of the two Fisk-like fields
directions from that of the Parker field
can be significant at all heliocentric positions and large in polar regions.
- 3.
- For all fields discussed here, the efficiency of injection of PUIs into the Fermi-I acceleration process at the termination shock is expected to be essentially the same, because the deviations in the different tilt angles at the termination shock are only visible in a fine structure, which is most probably not accessible to observations. The only distinct features are relatively narrow bands of strong tilt angle variations occurring for the modified Fisk field in the transition region from a slow to a fast wind.
- 4.
- During solar minimum, the favorable acceleration regimes for ACRs are in the flanks of the heliosphere.
H.F. and K.S. are grateful to the Deutsche Forschungsgemeinschaft (DFG) for funding the Heliocauses project and to the Bundesministerium für Bildung und Forschung (BMBF) for supporting the bilateral cooperation with South Africa. R.A.B. acknowledge the partial financial support of the SA National Research Foundation.
References
- Burger, R. A. 2005, Adv. Space Res., 35, 636 [NASA ADS] [CrossRef] [Google Scholar]
- Burger, R. A., & Hitge, M. 2004, ApJ, 617, L73 [NASA ADS] [CrossRef] [Google Scholar]
- Borrmann, T., & Fichtner, H. 2005, Adv. Space Res., 35, 2091 [NASA ADS] [CrossRef] [Google Scholar]
- Burger, R. A., Krüger, T. P. J., Hitge, M., & Engelbrecht, N. E. 2008, ApJ, 674, 511 [NASA ADS] [CrossRef] [Google Scholar]
- Burlaga, L. F., Ness, N. F., Wang, Y., & Sheeley, N. R. 2002, J. Geophys. Res., 107, 1410 [CrossRef] [Google Scholar]
- Ebert, R. W., McComas, D. J., Elliott, H. A., Forsyth, R. J., & Gosling, J. T. 2009, J. Geophys. Res., 114, 1109 [Google Scholar]
- Fahr, H. J., Kausch, T., & Scherer, H. 2000, A&A, 357, 268 [NASA ADS] [Google Scholar]
- Fahr, H. J., Scherer, K., Potgieter, M. S., & Ferreira, S. E. S. 2008, A&A, 486, L1 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Ferreira, S. E. S., Potgieter, M. S., & Scherer, K. 2007, ApJ, 659, 1777 [NASA ADS] [CrossRef] [Google Scholar]
- Fisk, L. A. 1996, J. Geophys. Res., 101, 15547 [Google Scholar]
- Forsyth, R. J., Balogh, A., & Smith, E. J. 2002, J. Geophys. Res., 107, 1405 [Google Scholar]
- Giacalone, J., & Jokipii, J. R. 2004, ApJ, 616, 573 [NASA ADS] [CrossRef] [Google Scholar]
- Giacalone, J., Jokipii, J. R., & Matthaeus, W. H. 2006, ApJ, 641, L61 [NASA ADS] [CrossRef] [Google Scholar]
- Heerikhuisen, J., Pogorelov, N. V., Florinski, V., Zank, G. P., & Le Roux, J. A. 2008, ApJ, 682, 679 [NASA ADS] [CrossRef] [Google Scholar]
- Hitge, M., & Burger, R. A. 2010, Adv. Space Res., 45, 18 [NASA ADS] [CrossRef] [Google Scholar]
- Izmodenov, V. V., Malama, Y. G., & Ruderman, M. S. 2008, Adv. Space Res., 41, 318 [NASA ADS] [CrossRef] [Google Scholar]
- Jokipii, J. R., & Kota, J. 1989, Geophys. Res. Lett., 16, 1 [NASA ADS] [CrossRef] [Google Scholar]
- McComas, D. J., Elliott, H. A., Schwadron, N. A., et al. 2003, Geophys. Res. Lett., 30, 24 [Google Scholar]
- McComas, D. J., Allegrini, F., Bochsler, P., et al. 2009a, Science, 326, 959 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- McComas, D. J., Allegrini, F., Bochsler, P., et al. 2009b, Space Sci. Rev., 146, 11 [NASA ADS] [CrossRef] [Google Scholar]
- Mordvinov, A. V. 2008, Cosmic Res., 46, 314 [NASA ADS] [CrossRef] [Google Scholar]
- Müller, H.-R., Florinski, V., Heerikhuisen, J., et al. 2008, A&A, 491, 43 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Murphy, N., Smith, E. J., & Schwadron, N. A. 2002, Geophys. Res. Lett., 29, 220000 [Google Scholar]
- Mursula, K. 2007, Adv. Space Res., 40, 1034 [Google Scholar]
- Opher, M., Stone, E. C., & Liewer, P. C. 2006, ApJ, 640, L71 [NASA ADS] [CrossRef] [Google Scholar]
- Opher, M., Richardson, J. D., Toth, G., & Gombosi, T. I. 2009, Space Sci. Rev., 143, 43 [NASA ADS] [CrossRef] [Google Scholar]
- Parker, E. N. 1958, ApJ, 128, 664 [Google Scholar]
- Pogorelov, N. V., Heerikhuisen, J., & Zank, G. P. 2008, ApJ, 675, L41 [NASA ADS] [CrossRef] [Google Scholar]
- Pogorelov, N. V., Borovikov, S. N., Zank, G. P., & Ogino, T. 2009, ApJ, 696, 1478 [NASA ADS] [CrossRef] [Google Scholar]
- Ratkiewicz, R. 2006, ASTRA, 2, 11 [Google Scholar]
- Richardson, J. D., Kasper, J. C., Wang, C., Belcher, J. W., & Lazarus, A. J. 2008, Nature, 454, 63 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- Roberts, D. A., Giacalone, J., Jokipii, J. R., Goldstein, M. L., & Zepp, T. D. 2007, J. Geophys. Res., 112, 8103 [CrossRef] [Google Scholar]
- Scherer, K., & Fahr, H.-J. 2003, A&A, 404, L47 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Scherer, K., & Ferreira, S. E. S. 2005, ASTRA, 1, 17 [Google Scholar]
- Scherer, K., & Fahr, H. 2009, A&A, 495, 631 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Schwadron, N. A. 2002, Geophys. Res. Lett., 29, 140000 [Google Scholar]
- Schwadron, N. A., & McComas, D. J. 2003, Geophys. Res. Lett., 30, 110000 [NASA ADS] [CrossRef] [Google Scholar]
- Schwadron, N. A., & McComas, D. J. 2005, Geophys. Res. Lett., 32, 3112 [CrossRef] [Google Scholar]
- Schwadron, N. A., Owens, M., & Crooker, N. U. 2008, ASTRA, 4, 19 [NASA ADS] [Google Scholar]
- Schwadron, N. A., Bzowski, M., Crew, G. B., et al. 2009, Science, 326, 966 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- Smith, C. W., & Bieber, J. W. 1991, ApJ, 370, 435 [NASA ADS] [CrossRef] [Google Scholar]
- Sternal, O., Fichtner, H., & Scherer, K. 2008a, A&A, 477, 365 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Sternal, O., Burger, A., Heber, B., et al. 2008b, Proc. Int. Cosmic Ray Conf., 451 [Google Scholar]
- Stone, E. C., Cummings, A. C., McDonald, F. B., et al. 2005, Science, 309, 2017 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
- Stone, E. C., Cummings, A. C., McDonald, F. B., et al. 2008, Nature, 454, 71 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
All Figures
![]() |
Figure 1:
The transition function
|
Open with DEXTER | |
In the text |
![]() |
Figure 2:
The Hammer projection (view from the Sun outwards) of the angle |
Open with DEXTER | |
In the text |
![]() |
Figure 3:
Left panel: the north (left) and south (right) pole of the
angle |
Open with DEXTER | |
In the text |
![]() |
Figure 4: The angle between the hybrid Fisk- and Parker-field in a meridional plane, the large spatial variation in the regions where the Fisk-type field is dominant. |
Open with DEXTER | |
In the text |
![]() |
Figure 5: The fit (red crosses) to the model results (green crosses) by Borrmann & Fichtner (2005). The equatorial plane is shown in the left panel and in the right the meridional one. |
Open with DEXTER | |
In the text |
![]() |
Figure 6: The magnetic tilt angle of the Fisk ( left) and the modified Fisk field ( right) at the analytically approximated termination shock. |
Open with DEXTER | |
In the text |
![]() |
Figure 7: The tilt angle for the Parker field in the analytic representation is shown in the upper left panel. For the numerical case the tilt angle of the Parker field is shown in the upper right, for the Fisk field in the lower left, and for the modified Fisk field in the lower right. |
Open with DEXTER | |
In the text |
Copyright ESO 2010
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