A&A 368, 760-765 (2001)
DOI: 10.1051/0004-6361:20010061
J.-Ch. Hamilton1 - K. M. Ganga1,2
1 - Physique Corpusculaire et Cosmologie,
CNRS-IN2P3,
Collège de France,
11 place M. Berthelot,
75231 Paris Cedex,
France
2 -
Infrared Processing and Analysis Center,
California Institute of Technology,
Pasadena, CA 91125,
USA
Received 11 October 2000 / Accepted 8 January 2000
Abstract
We present a correlation between the ACME/SP94 CMB anisotropy
data at 25 to 45 GHz with the IRAS/DIRBE data and the Haslam
408 MHz data. We find a marginal correlation between the dust
and the Q-band CMB data but none between the CMB data and the
Haslam map. While the amplitude of the correlation with the dust
is larger than that expected from naive models of dust emission,
it does not dominate the sky emission.
Key words: cosmic microwave background - cosmology: observations
The study of Cosmic Microwave Background (CMB) anisotropies has recently proven to be a powerful tool for observational cosmology (de Bernardis et al. 2000; Lange et al. 2000; Hanany et al. 2000; Balbi et al. 2000). One of the most important aspects of CMB analyses is to check whether the anisotropies observed are due to CMB temperature fluctuations or to foreground contamination, such as diffuse Galactic emission.
Diffuse Galactic emission is dominated at high frequency (above
100 GHz) by thermal emission from dust. High quality tracers
of this emission are given by the IRAS/DIRBE 100
m maps
and have been made available in a user-friendly way (Schlegel et al. 1998). At
lower frequencies, Galactic emission is dominated by synchrotron and
free-free radiations. Our best tracer of the synchrotron emission of
the Galaxy is given by the Haslam 408 MHz map (Haslam et al. 1981). Free-free
emission is traced by H
emission, but maps of this emission
are not yet publicly available.
Characterizing the correlations between these different Galactic
components and data taken in the microwave is important in order to
understand the spectral behaviour and the origin of Galactic emission
which may contaminate CMB measurements. The first significant,
high-|b| cross-correlation between the COBE/DMR maps and dust
templates was found by (Kogut et al. 1996a; Kogut et al. 1996b). Significant
correlations were found at each DMR frequency, but with a spectral
behaviour in better agreement with free-free emission than with
vibrational dust. These results have been confirmed by different
experiments in various parts of the sky:
Saskatoon (de Oliveira-Costa et al. 1997), OVRO (Leitch et al. 1997) and
19 GHz (de Oliveira-Costa et al. 1998). At high Galactic latitudes, however,
Python V (Coble et al. 1999) did not see any correlation. The regions of
the sky covered by these experiments are shown in Fig. 1.
As noted above, free-free emission should correlate with H
maps. Unfortunately, correlations found between H
maps and the
CMB indicate that the H
-traced emission is too small to
explain all of the observed correlation between CMB data and
100
m data.
Draine & Lazarian (1998a, 1998b) have suggested an alternate explanation for the correlation between CMB data and dust maps, namely that this emission may be the result of rotational dust emission from elongated grains. This emission could be compatible with the observed spectrum of the dust-correlated emission in the microwave frequencies.
The sum of dust components, both rotational and vibrational, should show a local minimum at roughly 70 GHz, increase to a peak around 10 GHz, and drop off at lower frequencies. Such behaviour has been observed by de Oliveira-Costa et al. (1999) in correlating the Tenerife 10 and 15 GHz data with the IRAS/DIRBE maps. This has been put forth as evidence supporting spinning dust as the origin of the dust-correlated emission. A recent analysis of yet more Tenerife data (Mukherjee et al. 2000) reports, however, that this result should be considered with care, as it originates mainly from a small, high Galactic latitude region. They finally say that the data does not allow any conclusion concerning the origin of the dust-correlated emission.
| |
Figure 1: Regions of the sky (in Galactic coordinates) covered by the different experiments that have been correlated with dust. Saskatoon is the grey region around the North Celestial Pole. OVRO observed 36 small patches of the sky at 2 degrees from the Pole. The main part of the Python V coverage is the grey region in the center of the lower part of the map. Tenerife observed a strip of 10 degrees width around the North Celestial Pole (grey ring). COBE and 19 GHz both covered the whole sky. South Pole is at the right of Python V |
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In this article we present a similar analysis using the South Pole 1994 (SP94) data (Gundersen et al. 1995). As correlations in the North Celestial Pole region have recently been questioned, we would like to obtain another measure of the correlation in a different region of the sky. More precisely, as correlations were found at low Galactic latitude (North Celestial Pole) and no correlation was found at high Galactic latitude by Python V, we wanted to explore the correlations in the high latitude regions that will be important for MAP and Planck. SP94 was a CMB experiment that used the Advanced Cosmic Microwave Explorer (ACME) which looked at such a high-|b| region.
The SP94 data were taken in two different bands with 7 different channels: the Ka-band with four center frequencies (27.25, 29.75, 32.25 and 34.75 GHz) and the Q-band with three different frequencies (39.15, 41.45 and 43.75 GHz). A detailed description of the instrument can be found in Meinhold et al. (1993), while the detail of the 1994 observations and data reduction is described in Gundersen et al. (1995). Frequencies and beam width for these channels are given in Table 1.
| Channel | Frequency (GHz) | Beam FWHM (deg.) |
| Ka1 | 27.25 | 1.67 |
| Ka2 | 29.75 | 1.53 |
| Ka3 | 32.25 | 1.41 |
| Ka4 | 34.75 | 1.31 |
| Q1 | 39.15 | 1.17 |
| Q2 | 41.45 | 1.11 |
| Q3 | 43.75 | 1.05 |
In this analysis, we used two templates for each channel:
![]() |
Figure 2: The top panels shows the co-added SP94 data for the Q-band and for the Ka-band separately. The co-addition was performed using, for each pixel, the full covariance matrix (using the method explained at the end of Sect. 3). The third panel shows the simulated IRAS/DIRBE data (dust) and the bottom panel shows the simulated Haslam data (synchrotron). For both simulated signals, only the 27.25 GHz band is shown, the others are very similar |
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For each of the seven frequency bands we have N=43 data points,
all at a declination of
and ranging from
and
in right ascension (see Fig. 1).
These data points were obtained using a sinusoidal
chop
with smooth, constant declination and constant velocity scans. We
directly follow in this section the notation of
de Oliveira-Costa et al. (1999). We assume that the data is a linear combination
of CMB anisotropies
and M foreground components
(including an unknown offset and gradient) that are given by simulated
observations of the template dust and synchrotron maps using the SP94
beam and scanning strategy. In a vector-like notation, one gets:
| (1) |
The noise and the CMB anisotropies are each assumed to be uncorrelated
Gaussian variables with zero mean. They each have non-trivial
covariance matrices and together a total covariance matrix of:
| C | = | (2) | |
| = | (3) |
The covariance matrix of the CMB is obtained through the window
function of the South Pole experiment
(Gundersen et al. 1995):
![]() |
(4) |
We are interested in measuring the correlation coefficients with the
various templates, we therefore want to measure
considering
and
as noise (but accounting for chance
alignment between CMB and the templates through the CMB covariance
matrix). We therefore construct the following
:
| (5) |
| (6) |
The best estimate of
is given through the
minimization along with its covariance matrix:
Equations (8, 9 and 10) implicitly suppose
that the dust-correlated component has a flat spectrum (i.e. has a
spectral index n=0). As was mentioned before, results from other
experiments tend to favor spectral indices close to
similar to free-free emission. In order to account for a non-zero
spectral index, we model the emission as:
![]() |
(11) |
| (12) |
We compute correlations between the SP94 and both dust and synchrotron templates shown in Fig. 2 and Table 2. Those results are also plotted as a function of the frequency in Fig. 3. The results we obtain show a marginal correlation of the Q-band data with the dust IRAS/DIRBE template whereas there is no correlation in the Ka-band. No significant positive correlation is found in either band with the Haslam template. The uncertainty on the combined Q-band and Ka-band correlation coefficients is not much smaller than that of the Q-band or Ka-band alone, as one might naively expect. In fact, this is due to the contribution of the CMB covariance matrix. For each channel, the CMB covariance matrix is comparable to the noise one and therefore combining the data reduces the noise contribution but not the CMB one, which becomes dominant.
In Table 2, we also show the result for the analysis
allowing the spectral index to vary as a free parameter. Combining
the Ka channels did not lead to any realistic value for the
spectral index (the best fit, n=5.0, was at the edge of the range we
searched). Combining the Q-band data leads to a best fit for the
spectral index of
.
Combining all Ka and Q data
together leads to
.
It is there fare clear that positive
values are preferred. This is not a surprise, however, as the Q-band
data obviously correlate with the IRAS data better than the Kadata does.
![]() |
Figure 3: Correlations coefficients between the SP94 data and the templates (top: with IRAS/DIRBE and bottom: with Haslam 408 MHz). The combined correlation coefficient assume a spectral index n=0 for the correlated component |
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We summarize in Fig. 4 the measurements performed up to
now of the correlation with the vibrational dust traced by IRAS/DIRBE
100
m: SP94 corresponds to the present article, the
Tenerife measurements have been published in two different articles
(de Oliveira-Costa et al. 1999; Mukherjee et al. 2000) reporting slightly different results
obtained with almost the same data. We plot both measurements; the
lower values were obtained by de Oliveira-Costa et al. (1999) and considered as
possible evidence for the presence of spinning dust because of the
fall at 10 GHz. The upper measurements (Mukherjee et al. 2000) were
published more recently and mitigated the enthusiasm for spinning
dust. As the values in this region are under question now, we plotted
a square around these points. OVRO measured one point in this region
at 14.5 GHz (Leitch et al. 1997) that seems to favour upper values of the
correlation. Saskatoon data are taken from de Oliveira-Costa et al. (1997) and
show a
detection in the Ka-band (not significant) and a
detection in the Q-band. The 19 GHz (whole sky survey)
data were taken from de Oliveira-Costa et al. (1998). The result from PythonV at 41 GHz was taken from Coble et al. (1999) and is fully compatible with no
detection (the best fit is negative and does not appear in the plot).
The COBE data points are from Kogut et al. (1996b). The results quoted in
the article were obtained by fitting DIRBE 140
m to the
DMR data. We therefore corrected them by the average ratio DIRBE
140
m/DIRBE 100
m to have them in the same
units as the other data points. The FIRS point at 167 GHz was obtained
by Ganga (1994). We also overplotted in Fig. 4
the predicted spectrum (in terms of ratio to IRAS/DIRBE
100
m) for vibrational dust in green (we assumed a
spectral index of 2.0) normalised with IRAS/DIRBE
100
m, and for spinning dust in blue. We also added the
spectrum for free-free emission in light blue (arbitrary normalization
and spectral index -2.1). For the spinning dust, we follow
Draine & Lazarian (1998a) for the mixing between Warm Ionised Medium (WIM),
Warm Neutral Medium (WNM) and Cold Neutral Medium (CNM) models using a
respective fraction of 0.14, 0.43 and 0.43. The respective
normalization of these models was also taken from
Draine & Lazarian (1998a). The sum of both contributions is shown in
Fig. 4 in red. The width of the curves for the spinning
dust model is due to the galactic latitude dependance of the optical
depth of the spinning dust components. We used all the latitudes more
than
from the Galactic equator. The normalization is that
given by Draine & Lazarian (1998a). As it clearly yields too little emission
to match the data, we have also done a fit to the points and
arbitrarily raised the model curves by this amount. This is indicated
by the dotted curve.
| Band | n | 100 |
sig. | 408 MHz | sig. |
| Ka1 | - |
|
-0.0 |
|
0.4 |
| Ka2 | - |
|
1.2 |
|
-0.3 |
| Ka3 | - |
|
0.3 |
|
-0.6 |
| Ka4 | - |
|
1.7 |
|
-1.1 |
| Ka | -2.0 |
|
-0.8 | - | - |
| Ka | 0.0 |
|
0.6 |
|
-0.5 |
| Ka | 0.8 |
|
1.2 | - | - |
| Ka | 2.0 |
|
1.9 | - | - |
| Ka | 2.1 |
|
2.0 | - | - |
| Q1 | - |
|
1.3 |
|
-0.9 |
| Q2 | - |
|
1.7 |
|
-1.3 |
| Q3 | - |
|
1.5 |
|
-1.0 |
| Q | -2.0 |
|
1.4 | - | - |
| Q | 0.0 |
|
1.6 |
|
-1.2 |
| Q | 0.8 |
|
1.6 | - | - |
| Q | 2.0 |
|
1.6 | - | - |
| Q | 2.1 |
|
1.6 | - | - |
| All | -2.0 |
|
-1.4 | - | - |
| All | 0.0 |
|
0.6 |
|
-0.9 |
| All | 0.8 |
|
1.7 | - | - |
| All | 2.0 |
|
2.3 | - | - |
| All | 2.1 | 54.2 |
2.3 | - | - |
![]() |
Figure 4: CMB/IRAS correlation coefficients as measured by various experiments. We overplot the spectra for vibrationnal dust, spinning dust and the sum of the two. The vibrationnal dust spectrum assumes a spectral index of 2.0 and was normalized to match averages of DIRBE at Galactic latitudes higher than 20 degrees. The spinning contribution is normalized following (Draine & Lazarian 1998a). To guide the eye, we also plot the best fit of the models to the data in dotted lines. We also added a free-free emission spectrum with a spectral index of -2.1 and an arbitrary normalization |
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The signal to noise ratio for the Q-band detection is only 1.6 (
confidence level) so this would not be considered a detection, as most
CMB experiments require at least 2
.
We note however
that, as opposed to normal CMB anisotropy analyses, here we are
comparing the data to a template and it is difficult to imagine
systematic effects or analysis errors that would cause a random
correlation with 100
m dust emission. The correlation
could arise from random alignment between the CMB anisotropies and the
dust template. This, however, should be taken into account in our
analysis if our covariance matrices for the data and the CMB are
correctly estimated. If these covariance matrices were underestimated,
the error bars we compute on the correlation coefficient (with
Eq. (7)) would be too small and therefore the significance of
our result would be overestimated. In order to check the validity of
our error bars, we correlated the SP94 data with template dust maps
obtained by rotating the initial template maps around the Galactic
poles and by inverting North and South. The Galaxy was either rotated
and/or inverted in 36 different ways (10 degrees each) to make
36 different simulations. We found a zero average correlation and the rms
of the correlations normalized by the error bars (calculated with
Eq. (7)) appears to be 1.1. This shows that the covariance
matrices of the CMB and the data and therefore our error bars are
correctly estimated, confirming the significance of the correlation
coefficients we obtain.
We do, however, find the following points interesting: As seen
previously (de Oliveira-Costa et al. 1997) the correlation between the Q-band and
the 100
m emission is stronger than the correlation
between the Ka-band and the 100
m emission. If the
correlation we found is to be believed, the ratio of the rms of the
100
m template times the fitted correlation coefficient
to the implied sky rms is 0.38 (in the Q-band). This result
indicates that roughly
of the power seen on the sky by
ACME/SP94 Q-band could be due to Galactic emission. The
could
go down by
and the amplitude by
.
This however does not
apply to the Ka-band. This result is in qualitative agreement with
Gundersen et al. (1995) and Ganga et al. (1997), both of whom found different spectral indices for the Ka- and Q-band data, though again, with
low statistical significance.
We have also done the above analysis using as a template not the raw
100
m data but rather the extrapolations recommended by
Schlegel et al. (1998) (model 8) to 500 GHz and 40 GHz. The
for the fit
decreased by a very small amount. The differences in the
were
not significant and do not change the conclusions drawn above. This is
not surprising as the SP94 data covers only a small region and the SFD
model was designed to cope with the whole sky.
In conclusion, we have shown that there is a very marginal correlation between the SP94 Q-band data and vibrational dust tracers, while no such correlation exists with the 408 MHz map. The amplitude of the correlation in the Q-band is larger than that seen by de Oliveira-Costa et al. (1997).
Acknowledgements
The authors would like to thank J. O. Gundersen and the ACME team for making the SP94 data available. We would also like to thank F. X. Désert for fruitful discussions.