To derive
,
we adopted two methods:
the iterative power-law fit (Schaye et al. 1999,
2000)
and the smoothed b power-law fit
(Bryan & Machacek 2000). From these two power-law
fit methods, we derived
and
of
Eq. (1) for
k = i or s, where
subscripts "i'' and "s'' indicate the
iterative power-law fit and the smoothed b power-law fit,
respectively. For the iterative power-law fit,
100 bootstrap realizations were averaged with an exclusion
threshold of 0.5 absolute
mean deviation (AMD)
. For the smoothed b power-law fit,
a smoothing constant of 3 km s-1 was used for each
subsample having 30 lines and the robust power-law fit was applied.
Schaye et al. (2000) used the iterative
power-law fit for
at
2 < z < 3.7 and for
at
3.7 < z < 4.4. Lines with
,
however, suffers from
incompleteness due to line blending. For example, at
,
lines with
are affected by incompleteness and this threshold
increases with z (cf. Hu et al. 1995; Kim et al.
1997, 2001a, 2001b). Incompleteness causes a
bias in the measurements of
.
Due to the lack of
lines with
below this threshold and
km s-1 (cf. Kim et al. 2001a),
an observationally measured
value becomes flatter
than its true value.
We have defined different lower
fitting thresholds at
the various redshifts in order to avoid this bias
(see Fig. 1) and to obtain
a stable estimate of
and
at the
fixed column density
,
.
Figure 1 shows the
-b diagram at
,
3.3 and 3.8 for Sample A.
The fitted parameters
are listed in Table 2, as well as the
ranges
used in the fit.
At higher z, several lines show
a b value smaller than
at
(shaded area).
In fact,
from the both power-law fits
increases as z decreases.
The slopes
at
and 3.8
are similar within errors, while the slope
at
is flatter than
the one at
more than
.
Both
slopes shows the lowest value at
(see Table 2). Note that, however, the errors from
the bootstrap method are likely to be underestimated (cf.
Schaye et al. 2000).
The close examination of Fig. 1 suggests
that
at
might well be overestimated and that the
real
might be inbetween
and
.
We visually compared our
with the results of Schaye et al. (2000; their Fig. 1),
although their sample corresponds to our Sample B.
As shown in Table 2, their
values are larger than our
values
at similar z with the differences larger at smaller z.
Their
values appear to be flatter than our values
at all z, likely caused by their lack of accounting for
incompleteness of observed lines.
![]() |
Figure 2:
Slopes
![]() ![]() ![]() ![]() ![]() |
Figure 2 shows
and
as a function of the lower
threshold
for Sample A.
The lack of lines due to incompleteness results in flatter
at lower
.
When the lower
threshold increases so that incompleteness
does not affect the
-b distribution severely,
becomes stabilized (the lower
at
and 3.3, and the lower
at
). If the available
lines in the fit, however, become too small for higher
,
becomes rather ill-defined. On the other hand, the
lower
does not affect the
values since
at
behaves more like a pivotal point. The slopes
and
from the smoothed b power-law fit
also show similar behaviors.
Figure 3 shows
and
as a function of z for the individual
members of Sample B (open symbols), the averaged values from Sample B
(filled triangles) and Sample A (filled symbols).
The members of Sample B show the large fluctuation of
and
even at the similar z (see Table 2).
With more lines
available to sharpen the lower cutoff envelope,
becomes steeper than the ones derived from the individual
members using a smaller number of lines,
possibly approaching asymptotic values (Sample A: filled circles, filled
squares and filled diamonds). For both Sample A and Sample B averaged (filled
triangles),
shows the lowest value at
,
although uncertainties for Sample B averaged are
rather large at
and 3.8.
While the 1
is 0.037 at
,
it becomes twice
as large as that at
and 3.8. This larger fluctuation
at z > 3 is caused in part by a smaller data size and in part by
the cosmic variance. The fluctuation
at
is mostly caused by different sightlines.
A single,
long
sightline does not show any significant difference between the lower-zpart and the higher-z part, such as HE1122-1648 and
HE2217-2818. On the other hand,
at
and 3.8, even a single, long sightline shows
a difference between the lower-z part and the higher-z part more
than 3
(see Sect. 3.3 for more discussions).
Similarly,
derived from a larger number of lines
is smaller,
possibly approaching asymptotic values
(Sample A: filled circles, filled squares and filled diamonds). Both
the
values from Sample A and
Sample B averaged (filled triangles)
increase as z decreases, although the uncertainties for Sample B
averaged are rather large. Note again that the larger fluctuation
of
at
and 3.8
(keep in mind the smaller sample sizes at z > 3 at the same time).
The smoothed b power-law fit also produces the large fluctuations
of
and
for the individual
members
of Sample B (see Table 2).
Our
and
for Sample A
are not consistent with the Schaye et al. values by more than
.
Our
and
for Sample B, however,
are completely in agreement with theirs.
This result shows that
deriving
and
depends largely on the number of lines in the fit and is
subject to the cosmic variance.
Experiments with the fitted line parameters show that in general
more than 200 lines in the fit stabilizes the results (cf. Schaye et al.
1999).
The large fluctuation found from sightline to sightline in similar
redshift
ranges using the number of lines smaller than 200
could explain in part the previous contradictory conclusions
on the evolution of
and
,
which
were usually based on a small number of lines and of sightlines.
There are several known voids (or regions devoid of
absorption lines with
)
in the present data.
One void (
)
towards Q0302-003,
two (
and 3.3) towards Q0055-269
and three (
,
2.2 and 2.3) towards HE2217-2818
have been identified.
The regions containing voids of Q0302-003 and
Q0055-269 show a flatter
by more than 7
(two lower squares at
in the upper panel of Fig. 3)
and a higher
by more than
(two higher
squares at
in the lower panel of Fig. 3) compared to
the ones derived from Q0055-269 without the voids.
The forest of HE2217-2818, however, does not
show any significant difference between the regions with the voids
and without the voids. Similarly, the HE1122-1648 forest
without any recognizable voids does not show any significant
difference between the lower-z part and
the higher-z part of the spectrum.
Even though voids are produced by the enhanced radiations from
local sources, the increase
of the H I photoionizing photons in voids
does not increase significantly the
temperature of the forest as whole (Haehnelt & Steinmetz 1998).
A fixed
,
however,
corresponds to a higher overdensity due to the increased
photoionization.
From the equation of state, a higher overdensity means a
higher temperature. Therefore, if voids are produced by enhanced
ionizations, there should be an increase of
and a decrease of
compared to the
forest without any extra heating sources at similar z (Haehnelt & Steinmetz
1998; Schaye et al. 1999).
The lack of a significant
difference in
and
from the HE2217-2818 forest at
suggests
that the origin of the voids towards HE2217-2818
is different. This could be due to a density fluctuation (Heap et al.
2000) and/or due to a shock heating by galactic infalls or
by galactic winds (Theuns et al. 2001a).
Simulations often show that some Ly
lines are
broadened by shock heating (Bryan & Machacek 2000;
Theuns et al. 2001a).
They also show that shock heating is not very
important at z > 2 for the lower column density forest considered
here.
In addition, the cutoff b method
is less sensitive than other methods to shock-heated gas
(cf. Theuns et al. 2001b).
One of the other main candidates for the fluctuations of
and
is
the He II reionization at
(Haehnelt & Steinmetz 1998; Songaila 1998;
Schaye et al. 1999).
There have been various claims
on a possible He II reionization at from observations
(Reimers et al. 1997; Songaila 1998;
Heap et al. 2000; Kriss et al. 2001).
One of the consequences of the He II reionization
is an increase of the temperature of the Ly
forest
(Haehnelt & Steinmetz 1998).
In fact, various theoretical models have predicted
a
(thus
a flatter
)
and a higher
(thus a higher
)
when the He III bubbles surrounding the ionizing sources
overlap and increase the radiations in the IGM
(Haehnelt & Steinmetz 1998; Ricotti et al. 2000;
Schaye et al. 2000).
To study the effect on the Ly
forest caused by the
He II reionization, we re-grouped the individual members
of Sample B. For each z bin, individual members were divided into two
subgroups according to their redshift ranges, i.e. a lower-z part and
a higher-z part. This method of grouping has been
taken since the absorption
lines from the same sightline might be correlated. The number of lines at
each subgroup is sampled to be similar (see Table 2).
There is no significant difference in
and
between
and
.
There is, however, a significant difference
by more than
3
between the lower-z and the higher-z parts at
and at
.
The slope
decreases at lower z for each bin at z > 3,
while the
increases. In short, along each line of sight at z > 3,
decreases and
increases
at z decreases, as expected from the He II reionization
at
.
This trend, however, does not continue at z < 3,
i.e. the HE1122-1648 forest and the HE2217-2818
forest do not show the similar behavior. Theuns et al. (2001b)
find a similar behavior of b values from the wavelet analysis
using the same data presented here.
This is interpreted as a result of HeII reionization at
.
They do find, however, a cold region, i.e. a region with
a lower average b values than the adjacent regions along HE2217-2818.
Deriving the cutoff Doppler
parameters using a small
number of lines introduces a large scatter (Fig. 3). Therefore,
a flatter
and a higher
shown at the lower-z part of the bins at z > 3 (
3.1 and
3.6)
might be an artifact of the small number of
lines in the fit. More available lines in the fit, however, tends to
increase
and to decrease
as seen in Sect. 3.2, contrary to this result.
The
-b distributions at
and
show a lack of lines with
and
km s-1with respect to the ones
at
and 3.9, while the
-b distributions
for higher-
lines are similar (the figures not shown).
This lack of
lower-
and lower-b lines results in a
flatter
and a higher
at
and 3.6.
This, however, can not be caused by incompleteness due to
line blending.
The number of lower-
lines are
similar at
and
,
and at
and
,
i.e. b values corresponding
to lower-
lines are higher at
and
than those at
and
.
In addition,
line blending is more severe at higher z and should have resulted in
a lack of lower-
and lower-b lines at
and
rather than at
and
as observed. What is observed at
and
shows the opposite behavior expected from line
blending. In fact, the lower-
and higher-b lines
seen at
and at
are expected from the He II reionization since it has a greater
effect on the lower-
forest than on the
higher-
forest (Theuns 2001, private communication).
Songaila (1998) found that there is
an abrupt, sharp discontinuity in the
ratio of Si IV column density to C IV column density,
/
,
at
,
below which
/
is always
less than
0.07.
The observed
/
by
Songaila (1998) suggests that the UV background is softer than
a QSO-dominated background at z > 3 and becomes harder as expected
from a QSO-dominated background at z < 3. This observation
has been interpreted
as the complete He II reionization by
,
i.e.
the overlap of the He III bubbles.
Figure 4 shows
/
of the
Ly
forest
at
as a function of z
from the QSOs in Table 1 except from
Q0000-263 (Kim et al. 2001, in preparation).
We only include the H I systems having higher Lyman lines
other than Ly
,
such as Ly
,
Ly
,
etc. This selection
enables us to estimate an accurate H I column density and to
assign Si IV and C IV to a H I line more reliably.
Note that there are no data points at
2.6 < z < 2.9 at which the discontinuity of
/
has been reported to be the largest. Although the bulk of the forest
shows lower
/
at z < 2.6, there are the forest lines with
/
larger than 0.07.
The similar results have been reported at z > 2 by
Boksenberg et al. (1998). Bear in mind that
no specific H I column density range used in
their Fig. 1 is given in their paper. In addition, note that their
results are based on the individual, fitted components, while ours are
based on the integrated absorption lines. Using
the component-by-component analysis introduces an additional scatter in the
diagram due to the different velocity structures in Si IV
and C IV. The number of components for one integrated system
in our data is in general from 1 to 3. The component-by-component
analysis on our data also shows the similar trend found in Fig. 4
from the integrated profiles.
Our observations do not suggest any abrupt change in
/
at
1.6 < z < 3.6, i.e. no abrupt change in the
softness parameter in general. This result suggests that
some forest clouds are exposed to a soft UV background at
z < 2.6. The lack of a sharp change
in
/
at
does not mean, however, that the He II reionization
did not occur at
.
Rather, our
/
indicates that
/
might not be a good observational
tool to probe the He II reionization. What it probes is
a softness parameter of the UV background. Increasing evidences
of the contribution to the UV background from local, high-z galaxies
would explain our high
/
at z < 2.6 without any
difficulty (Giroux & Shull 1997; Shull et al. 1999;
Bianchi et al. 2001;
Steidel et al.
2001). In addition,
the lack of strong z-evolution of
found
for
at z > 3is in agreement with the lack of strong evolution of
/
at
.
In short,
the He II reionization at
(Reimers et al. 1997; Heap et al. 2000;
Smette et al. 2002) shows its impact on the Ly
forest mainly at
and might be very inhomogeneous.
Its strength might not be as strong as previously suggested and
/
might not be a best observational tool
to probe the He II reionization.
Copyright ESO 2002