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Figure 10:
PUI ENA H flux as a function of direction for 16 keV H
(![]() ![]() |
The post-shock PUI distribution cannot as yet be observed in situ. One possibility is an indirect observation using as messengers the energetic neutral atoms (ENA), into which the PUI are converted by capturing electrons from the atoms of the background at the occasion of charge-exchange collisions (the first discussion of the heliospheric ENA was given by Hsieh et al. 1992). Below we calculate the flux of ENA corresponding to the PUI distributions derived above.
The flux of ENAs observed at the point
from the direction
:
,
can be obtained integrating along the
line-of-sight
the
flux of pick-up ions relative to the neutral component
multiplied by the density of the background
neutral atoms and by the charge-exchange cross section. The neutral
components move at low speed in the fixed frame, so that we can use as
a good approximation the PUI flux in the fixed
frame:
and neglect the difference between the velocity
relative to the observer and that relative
to the neutral background:
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(26) |
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Figure 11:
PUI ENA H flux as a function of direction for 16 keV H
(![]() ![]() |
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Figure 12:
ENA flux: the data points show the flux
(units (cm2 s sr keV)-1) of
![]() ![]() ![]() ![]() |
The PUI ENA hydrogen flux corresponding to the model pick-up proton
distributions is presented in Figs. 8-12. The calculations were done
for the case of observations from the inner solar system
(e.g. Earth's orbit) with the line-of-sight directed radially away from
the Sun. Figures 8 and 9 show the PUI ENA spectrum for the cases
and
,
respectively. Note that the pre-shock ENA
flux is negligible compared to the post-shock contribution in the
normal turbulence (
)
case. This is obviously due
in part to the effect of plasma motion (if the pre-shock PUI velocity
distribution in the plasma frame would be cut off at the solar wind
energy there would be no sunward ENA flux at all). In the
case the result is opposite due to strong pre-acceleration: this case
is, however, unrealistic.
Figures 10, 11 illustrate the directional dependence of the ENA flux for
the sample energy value of 16 keV (the flux for 63 keV for the case
is shown in Fig. 12). In the normal turbulence case
(
)
there is a pronounced peak in the flux from the anti-apex
direction, provided the energy is not too low (see also Fig. 9). The
peak is due to the concentration of the PUI in the heliotail (Figs. 4
and 5) due to convection by the plasma flow and to the asymmetric shape of
the heliopause. The position of the minimum of the flux is away from the
apex. The (unrealistic)
case, where the flux is dominated by
the contribution from the pre-shock region, behaves differently, with the
maximum flux coming from the apex direction.
The first detection of what may be the ENA of heliospheric origin
is due to CELIAS/HSTOF (Hilchenbach et al. 1998).
The acronym denotes the High-energy Suprathermal Time-of-Flight
sensor (HSTOF) of the Charge, Element and Isotope Analysis System
(CELIAS). It is operating on board of the SOHO spacecraft, situated near
the Lagrangian point L1 between Earth and the Sun.
The instrument has the line-of-sight directed
west off the Sun,
with the field-of-view
wide in longitude and
in
latitude. During the course of one year it scans over all directions
in the ecliptic plane.
The observations of ENA are possible only during the periods of relatively
low ion flux intensity, the "quiet times''. For these periods, the
events in the low energy channels (58-88 keV) were interpreted as neutral
hydrogen atoms. The results are shown in Fig. 12. These include the
changes due to in-flight new calibration of the instrument (Hilchenbach et al. 2000) which raised the previous estimations of the
flux by a factor of 10. Note that there are many data points for the two
first years of observations (1996 and 1997) which were characterized by
low solar activity. The quiet time
flux in the 55-80 keV range
peaked during the periods near
,
close to the time (
)
when
the instrument's line-of-sight was directed towards anti-apex of the LISM.
In 1998 the contact with SOHO was lost for a period of time including DOY
200. The high solar activity during 1999 reduced the quiet time periods,
and in 2000 the situation was even worse due to a big solar flare
("Bastille Day flare'' of June 14th).
The observations are compared with the calculated ENA hydrogen flux
from the pick-up proton distribution for the
case, at 63 keV
(which approximates the average energy of the observed particles in
the 58-88 keV range). With no adjustments in the model parameters, the
calculated flux intensity is close to the observed flux. Note a small
shift of the observed flux peaks from the anti-apex position. This is not
necessarily inconsistent with the PUI ENA model, because the direction
towards the heliotail may be different from the anti-apex due to the
interstellar magnetic field (Fahr et al. 1988; Ratkiewicz et al. 1998; Czechowski & Grzedzielski 1998).
Figures 13 and 14 present the results for the ENA energy spectrum. To derive the spectrum from the SOHO data one must subtract the flux of protons which penetrate into the instrument from the measured total mass=1 flux. The uncertainty in the quiet time proton flux (assumed to follow a power law of E-2.5) and in the probability of proton transmission would introduce a systematic error in the ENA flux. Only for the three lowest energy data points this error is expected to be small (<10%, Hilchenbach et al. 2000). The calculated spectrum is clearly steeper than the data.
Copyright ESO 2001