A&A 493, 835-857 (2009)
DOI: 10.1051/0004-6361:200810514
J. Delabrouille1 - J.-F. Cardoso1,2 - M. Le Jeune1 - M. Betoule1 - G. Fay1,3 - F. Guilloux1,4,5
1 -
Laboratoire AstroParticule et Cosmologie (APC), CNRS: UMR 7164,
Université Paris Diderot - Paris 7,
10 rue A. Domon et L. Duquet, 75205 Paris Cedex 13, France
2 -
Laboratoire de Traitement et Communication de l'Information (LTCI), CNRS: UMR 5141, Télécom ParisTech, 46 rue Barrault, 75634 Paris Cedex, France
3 -
Laboratoire Paul Painlevé, CNRS: UMR 8524, Université Lille 1,
59655 Villeneuve d'Ascq Cedex, France
4 -
Modélisation Aléatoire de Paris X (MODAL'X), Université Paris Ouest -
Nanterre-la-Défense,
200 avenue de la République, 92001 Nanterre Cedex, France
5 -
Laboratoire de Probabilités et Modèles Aléatoires (LPMA),
CNRS: UMR 7599, Université Paris Diderot - Paris 7,
175 rue du Chevaleret, 75013 Paris, France
Received 3 July 2008 / Accepted 18 October 2008
Abstract
Context. The WMAP satellite has made available high quality maps of the sky in five frequency bands ranging from 22 to 94 GHz, with the main scientific objective of studying the anisotropies of the Cosmic Microwave Background (CMB). These maps, however, contain a mixture of emission from various astrophysical origin, superimposed on CMB emission.
Aims. The objective of the present work is to make a high resolution CMB map in which contamination by such galactic and extra-galactic foreground emissions, as well as by instrumental noise, is as low as possible.
Methods. The method used is an implementation of a constrained linear combination of the channels with minimum error variance, and of Wiener filtering, on a frame of spherical wavelets called needlets, allowing localised filtering in both pixel space and harmonic space.
Results. We obtain a low contamination low noise CMB map at the resolution of the WMAP W channel, which can be used for a range of scientific studies. We obtain also a Wiener-filtered version with minimal integrated error.
Conclusions. The resulting CMB maps offer significantly better rejection of galactic foreground than previous CMB maps from WMAP data. They can be considered as the most precise full-sky CMB temperature maps to date.
Key words: cosmology: cosmic microwave background - methods: data analysis
The WMAP satellite is one of the most successful experiments dedicated to mapping the Cosmic Microwave Background (CMB). The all-sky maps obtained in the WMAP five frequency bands, in temperature and polarisation, offer the best data set to date for making a sensitive all-sky map of the CMB anisotropies.
The CMB, however, is not the only source of emission at WMAP frequencies. Diffuse galactic emission from several processes contaminates the maps with an amplitude roughly proportional to the cosecant of the galactic latitude, compromising the observation of the CMB close to the galactic plane. In addition, a background of radio and infrared compact sources, galactic or extra-galactic, contributes to the total emission even at high galactic latitudes. Component separation consists of separating one or more of these sources of emission from the others in the data.
One of the main objectives of CMB experiments is the measurement of the CMB angular power spectrum
which, with the assumption of statistical isotropy, describes the second order distribution of the CMB and can be estimated on a fraction of the sky. For this reason, many ground-based and balloon-borne experiments have concentrated their observations in ``clean'' regions of the sky, where galactic emission is low enough to negligibly impact the observations. For power spectrum estimation from full-sky observations, a safe approach consists of masking regions at low galactic latitude, and estimating power spectra on the cleanest regions of the sky. The impact of extragalactic point sources (evenly spread on the sky) on power spectrum estimates can be evaluated and corrected for using ancillary data (catalogues of known point sources and priors on the statistical distribution of sources).
Besides the power spectrum, the CMB map itself is interesting for several additional purposes:
All available maps suffer from limitations, some of which result from specific choices in the way the CMB map is produced. Several of these maps, for instance, do not fully exploit the resolution of the original observations. Some focus on cleaning the CMB of foreground at high galactic latitude, and are significantly contaminated by foreground in the galactic plane. Some are not full sky CMB maps. Finally, not all of the available maps have well characterised noise and effective beam. All these limitations impact on their usefulness for accurate CMB science.
In this paper, we address the problem of making a CMB temperature map which has the following properties:
This paper considers only temperature maps.
We start with a review of the requirements above, and on the implication on the method to be used.
WMAP data are full sky. We wish to devise a method which allows recovery of an estimate of CMB emission everywhere, including in the galactic plane, and even (as much as possible) in the galactic centre as well as in pixels strongly contaminated by compact sources.
The large scale correlation properties of the CMB make it possible to estimate the CMB emission even in unobserved regions, by some kind of interpolation. This is what is also obtained with the Gibbs sampling technique of Eriksen et al. (2007). Equivalent in spirit although quite different in implementation is the use of an ``inpainting'' method such as that of Elad et al. (2005) and Abrial et al. (2008). Such interpolation methods alone are not fully satisfactory, as they discard information. In particular they do not allow the recovery of small scale CMB features in the mask. This is obvious, for instance, in the Gibbs-sampling average map of Eriksen et al. (2007).
At the opposite extreme, one may try to separate components in the galactic plane independently of what is done at higher galactic latitudes, since levels and properties of foreground emission depend strongly on sky direction. Hinshaw et al. (2007) and Tegmark et al. (2003) divide the sky into several independent regions, perform component separation independently in these regions, and then make a composite map by stitching together these independent solutions. Such approaches discard information (zone-to-zone correlations) and require careful treatment at the zone borders to avoid discontinuities and ringing.
A good method should perform well on both counts: localised processing and full exploitation of large scale correlations of the CMB and of galactic foreground emissions. This can be achieved with a spherical wavelet or needlet analysis of the maps (using the tools developed in Marinucci et al. 2008 and Guilloux et al. 2008), which is our approach in the present work.
Recovery of a CMB map can be conducted following various objectives, quantified by different ``figures of merit''. In this work, we choose, as do most authors, to minimise the variance of the difference between true and recovered CMB (this is the overall error; it includes additive noise, foreground emissions, and even multiplicative errors affecting the CMB itself).
This choice alone does not fully characterise the method to be used. The best theoretical solution also depends on the model of the data. An overview of existing methods can be found in the review by Delabrouille & Cardoso (2007).
In this paper, contrarily to other approaches which rely heavily on the structure of the data as described by a model, for instance a noisy linear mixture of independent components (Delabrouille et al. 2003), we assume as little as possible about the foreground emissions and the noise. In fact, we assume nothing except the following:
The WMAP data comes in five frequency channels with varying resolution. To make the best of the data, we need a method which uses the smallest scale information from the W band, and information from additional bands (V, then Q, then Ka, and finally K) at increasingly larger scales. Multi-scale tools are well suited for this purpose.
The ``best possible resolution'' is not a well defined concept (and not necessarily the resolution of the W band). Indeed, there is a conflict between best possible resolution and minimum variance, as one can smooth or deconvolve a map arbitrarily in harmonic space, reducing or increasing the total noise variance in the process. Here, we make a map at the resolution of the W channel over the full sky, leaving open the option to filter this map if needed to reduce the noise - or deconvolve it for better angular resolution. Note that additional global filtering or deconvolution does not change the signal to noise per mode (only the integrated S/N).
The minimum variance map is obtained with a Wiener filter, which smoothes the map depending on the signal to noise ratio. As the noise and the contaminants are inhomogeneous, there is a strong motivation for the smoothing to depend on the location on the sky (the optimal solution to the resolution-variance trade-off depending on the contamination level, which is local). If we relax the constraint about beam homogeneity, again, spherical needlets offer a natural way to obtain such location-dependent smoothing. In the present, however, in order to preserve the constancy of the effective beam over the sky, we implement the Wiener filter in harmonic space.
A fully accurate characterisation of the beam and noise is not
straightforward, in particular because of the limited knowledge about
the original frequency maps, which automatically propagates into the
final CMB map. This work makes several approximations about beams and noise.
Beams are assumed to be symmetric and therefore described by the
transfer functions provided by the WMAP team.
The instrumental noise is assumed uncorrelated, although non stationary.
Analyses and Monte-Carlo simulations are used to
characterise the residual noise of the final map, as well as to estimate the
contribution of residual foregrounds, and biases if any. This is detailed further below.
Throughout this paper, the term ``noise'' refers to all sources of additive error, i.e. instrumental noise and foreground emissions.
We briefly discuss here the tools used for characterising and comparing CMB temperature maps.
A pixelised map is fully characterised by the specification of:
![]() |
(1) |
Throughout this paper, the beam is assumed symmetric. Although this is an approximation, most pixels of the WMAP map are ``visited'' by any particular detector through a wide range of intersecting scans. The average beam in that pixel then is an average of the physical beam over many orientations, which makes the symmetry assumption reasonable.
In addition, in the absence of any specific localised processing, the beam is assumed to be invariant over the sky.
With the above two assumptions, the effect of beam convolution is best represented in harmonic space, with a multiplicative coefficient
,
independent of m, applied to the harmonic coefficients
of the map. We assume perfect beam knowledge as well as perfect calibration, so that no multiplicative uncertainty is attached to the map description (the beam integral, approximated as
,
is equal to unity independently of p, or, equivalently, the value of
for
is assumed to be exactly unity).
The noise np of the original WMAP maps, for each frequency channel and each differencing assembly, is assumed uncorrelated from pixel to pixel, i.e.
.
The variance
is pixel dependent because of uneven sky coverage. Noise is non-stationary, but assumed to be Gaussian distributed.
The comparison of CMB maps is meaningful only if the maps are at the same resolution. As long as the beam transfer function does not vanish at any
useful
(which is always the case for Gaussian beams), the resolution of any map can be changed to anything else by harmonic transform and multiplication by the ratio of the beam transfer functions. In the present work, we approximate WMAP beams by their symmetric fit (i.e. azimuthally averaged beams), which is justified by the large range of scanning directions at any point in the sky.
This convolution - deconvolution property is widely used throughout this paper.
We define ``tapered'' regions of the sky for map comparison at varying galactic latitude. In particular, we define a Low Galactic Latitude (LGL) region and a complementary High Galactic Latitude (HGL) region. The LGL region, used to evaluate results in the galactic plane, completely excludes all data above 30 degrees galactic latitude (and below -30 degrees), and has a 15 degree transition zone with a cosine square shape. All pixels at absolute galactic latitudes below
15 degrees are kept with a coefficient of 1. The HGL region is the complementary, i.e. HGL =
.
These ``tapered'' regions allow the computation of local power spectra with negligible spectral leakage of large scale power into small scales.
For a given beam (i.e. multiplicative response as a function of
), the comparison of the total map power as a function of
(i.e. of the power spectra of the maps) is a direct figure of merit. The lower the power spectrum, the better the map.
Indeed, for fixed
,
two distinct maps contain the exact same contribution from CMB, but different noise levels. CMB and noise being assumed to be uncorrelated, power spectra are the sum of a CMB term (
)
and a noise term (
). The CMB term being the same for both spectra, any difference in total power spectrum can be interpreted as a difference in noise level.
Power spectra are computed independently for different regions of the sky (e.g. inside or outside the galactic plane). To minimise aliasing due to sharp cuts, we use masks with smooth transitions, defining the LGL and HGL regions described above.
The power spectrum of a map is evaluated as:
![]() |
(2) |
Power spectra estimated directly in this way from a masked sky are unreliable for modes corresponding to angular sizes larger than the typical size of the zone of the sky retained for computation.
We now give a brief introduction to the two main methods used in this paper (ILC and Wiener filtering). Many other methods exist for CMB cleaning (or component separation in general), which assume varying degrees of prior knowledge about sky emission, and model the data in different ways. These methods are not discussed nor used in this paper. For a review, see Delabrouille & Cardoso (2007).
The data are modelled as
| (3) |
The ILC provides an estimator
of s as follows:
Note that the ILC solution of Eq. (4) is the linear filter which minimises the total variance of the output map, under the condition that the filter has unit response to the signal of interest (the signal with the emission law given by vector
).
The details of the method for its implementation in the context of this work are further discussed in Sect. 4.
Given a single CMB map of known beam (assumed to be constant over the
sky), it is possible to minimise the contamination by noise and
foreground by (one-dimensional) Wiener filtering. The data is
modelled as x=s+n, where now x is a single map, s the true CMB
and n the noise. The Wiener filter gives to individual ``modes'' a
weight proportional to the fraction of signal power in that mode, i.e.
Wiener filtering in harmonic space minimises the variance of the error in the map if signal and noise are Gaussian and stationary. For non-stationary contaminants, the Wiener filter (5) is still meaningful, but is no longer optimal. Here, the Wiener filtering is applied after the ILC. Foreground contamination, strongly reduced by the ILC, is no longer dominant. Instead, instrumental noise is the major source of error on all scales where the Wiener filter is useful (departs from 1). A harmonic space implementation of the Wiener filter disregards this non-stationarity, applying the same coefficient to a given scale, whether it is in a region of deeper integration or not.
Better efficiency may be obtained by an implementation in another domain than the harmonic space (e.g. needlets), but this is not investigated further in this paper, as the consequence is a non stationary equivalent beam.
Before describing how to make yet another CMB map from WMAP data, we review the existing maps and evaluate in what respects they can be improved.
We start with a discussion of the existing methods, identifying for each of them the strengths and weaknesses of the approach, and their foreseeable consequences. Available CMB maps obtained from WMAP data are compared in terms of resolution, of the estimated contamination by foreground emission, and of noise level. In the absence of an absolute reference, discrepancies between available maps are also evaluated. This comparison permits an estimate of typical uncertainties, and to outline the ``difficult regions'' for CMB cleaning (which, unsurprisingly, are mostly located close to the galactic plane). We also look specifically for residuals of galactic contamination by comparing the power spectrum of the reconstructed CMB map at high and at low galactic latitudes. Significant discrepancies between the two are interpreted as indicative of a residue of foreground emission.
The ILC maps obtained by the WMAP team (denoted as WILC1, WILC3 and WILC5 hereafter, depending on whether they are obtained using one year, three year or five year data) are described in Bennett et al. (2003), Hinshaw et al. (2007), and Gold et al. (2008) respectively.
For the three year and five year maps, the original frequency maps are smoothed to a common resolution of one degree. The sky is subdivided into 12 regions. One large region covers most of the sky at moderate to high galactic latitudes. The rest of the sky, concentrated around the galactic plane, is divided into 11 regions of varying galactic emission properties (amplitude and colour). An internal linear combination (ILC) is performed independently in each of these regions. A full sky composite map is obtained by co-adding the maps of the individual regions (with a
1 degree transition between the zones to avoid sharp edge effects). Finally, a bias (inevitable consequence of empirical CMB-foreground correlation) is estimated by Monte-Carlo simulations, and subtracted from the composite map, to yield the final CMB map.
The three year and five year ILC maps differ from the one year map in several respects. The most significant is the recognition of the existence of a bias, and the attempt at correcting it using simulations. The limitations of the maps include their resolution (one degree), and the use of small regions in the ILC, which is bound to cause more bias than necessary on large scales (comparable to patch sizes)
, as well as edge effects. This results in discontinuities between regions, obvious for instance in the estimated bias map shown in Hinshaw et al. (2007).
In the method used by the WMAP team, the coefficients of the linear combination used over most of the sky (region 0, which corresponds to the largest part of the sky at high galactic latitudes and a few low galactic latitude patches, and region 1, in the galactic plane but away from the galactic center) are set using only a small subset of the data inside the Kp2 cut (where the galactic emission is the strongest). This choice favours the rejection of galactic contamination, at the price of sub-optimal weighting of the observations in regions where the error is dominated by noise. It also assumes that the emission laws and relative power of the different foregrounds are the same in these regions, which is a strong (and probably wrong) assumption.
Furthermore, the ILC weights are set by minimising the variance of the map at one degree resolution. Modes at higher
get very sub-optimal weighting, as they do not contribute significantly to the total variance of the one degree map. The K and Ka bands, in particular, contribute respectively about 0.156 and -0.086 to region 0 (the largest one) for WILC3. As a consequence, the final
ILC map cannot be meaningfully deconvolved to better resolution than about 1 degree (because this would amplify dramatically small scale noise coming from the lowest frequency channels).
Finally, there is also an unsatisfactory degree of arbitrariness in the choice of the regions, which depend on priors about foreground emission, and are somewhat elongated across the galactic plane for no particular reason. Although none of these choices is unreasonable, the impact of this arbitrariness on the final map is difficult to evaluate.
For all these reasons, the WILC maps leave considerable margin for improvement. We aim, in particular, at obtaining a CMB map with better angular resolution, and with a better handling of non-stationarity and scale dependence of the contamination (foregrounds and noise).
For temperature power spectrum analysis, the WMAP team has used part-sky foreground-reduced maps. The processing for foreground removal for the three year and five year releases is described in Hinshaw et al. (2007). Model templates for galactic emission are fitted to the Q, V and W WMAP channels outside of the Kp2 mask. A linear combination of synchrotron, free-free and dust, based on this fit, is then subtracted from the full sky Q, V, W maps.
In this procedure, a first galactic template, supposed to correspond to a linear combination of synchrotron and free-free emission, is obtained from the difference between the K and Ka bands. This template is produced at one degree resolution. An additional free-free template is obtained from H
emission (Finkbeiner 2003) corrected for dust extinction (Bennett et al. 2003). A dust template is obtained from model 8 of Finkbeiner et al. (1999). ``Clean'' Q, V and W maps are obtained by decorrelation of these templates from the original Q, V and W observations.
The main limitation of this approach is that the model used is insufficient to guarantee a good fit of the total foreground emission simultaneously inside and outside of the Kp2 mask. As a consequence, the maps produced are heavily contaminated by foreground emissions in the galactic plane, the priority being given to higher galactic latitudes, with the objective of obtaining a part-sky high quality map on which high multipole CMB power spectra could be estimated reliably.
In addition, the maps are likely to depend significantly on the prior model assumed. Here, the WMAP team chooses dust model number 8 of Finkbeiner et al. (1999), and also ignores the plausible existence of anomalous dust emission. The exact impact of these a priori decisions is difficult to evaluate. Anomalous dust emission will come into the foreground reduced maps chiefly as a contaminant in the K-Ka synchrotron template, and hence lead to an erroneous extrapolation of this template to higher frequencies. Assumptions about the emission laws of the template correlated to H-alpha, and of the dust template, if inaccurate, will also result in inaccurate subtraction of free-free and dust. These errors in the estimate of foregrounds are bound to leave, after template subtraction, foreground residuals in the foreground reduced maps.
As an additional drawback, we note that the method generates correlated noise in the foreground-reduced maps, originating either from K and Ka channel noise or from a background of radio sources (see, e.g., Huffenberger et al. 2007; and Wright et al. 2008, for discussions on radio sources in WMAP data and their impact on the analysis of CMB observations with WMAP). Finally, on supra degree scales, the K and Ka bands, which are the most sensitive ones, are used only to subtract foreground emissions, whereas in the cleanest regions of the sky they would be more usefully used to estimate the CMB emission.
For all these reasons, WMAP foreground-reduced maps are not good CMB maps according to the criteria listed in the introduction.
Eriksen et al. (2004) have obtained a CMB map at 1 degree resolution with another implementation of the ILC. The map, denoted here EILC1, uses only one year data.
An interesting remark from Eriksen et al. is that the amount of residual dust is high in the ILC maps - the method being able to subtract only about half of the dust present in the W band. At scales larger than 1 degree, this lack of performance is likely to be due to the part of dust emission uncorrelated to low frequency galactic foreground. On the smallest scales, the situation is worse, as the low frequency WMAP channels do not have the resolution to help remove small scale dust emission from W band observations.
For this reason, in the present work, we improve on dust removal by using, as an additional measurement, the IRIS 100 micron dust template obtained from a combination of DIRBE and IRAS maps (Miville-Deschênes & Lagache 2005). As compared to the map of Eriksen et al., we also aim at better angular resolution - and, obviously, better sensitivity, achieved by using five year data sets.
Table 1: Available CMB maps.
![]() |
Figure 1: A selection of presently available CMB maps from WMAP data. Contamination by galactic emission is visible in all of them at various levels, except for the 3-degree resolution EGS3 map (for which a galactic cut was applied and then filled by a plausible CMB extrapolated from higher galactic latitude data). |
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Recently, Eriksen et al. (2007) have produced a low resolution (3 degree) CMB map from WMAP three year data, using a Gibbs sampling technique to explore the likelihood of a parametric model of CMB and foreground emissions. A CMB map is obtained as the average of 100 sample CMB maps each drawn at random according to the posterior distribution of the model parameters given the observations.
The free parameters in the model are spherical harmonic coefficients
of the CMB map, the CMB harmonic power spectrum
,
monopole and dipole amplitudes in each WMAP band, the amplitude
of a dust template in each band, and amplitudes f(p) and spectral indices
of a low-frequency foreground component, for each map pixel p.
The model is constrained by fixing the dust template at 94 GHz according to Finkbeiner et al. (1999), by a prior on the low-frequency foreground spectral index, assumed to be close to that of synchrotron radiation (
), and by the constraint that the monopole and dipole coefficients are orthogonal to the (noise-weighted) pixel-averaged foreground spectrum.
In spite of a good fit of the assumed model to the data at high galactic latitudes, there are some strong limitations to the resulting CMB map, and hence to its usage:
Park et al. (2007) provide their own version (hereafter the PILC3 map) of a one degree resolution CMB map obtained by an ILC on WMAP three year data. The originality of their approach lies in the fact that they cut the sky into 400 pixel ensembles, selected from a prior on their spectral properties. The 400 ensembles are defined from
spectral index bins (20 for K-V spectral index,
and 20 for V-W). This approach is motivated by the fact that ILC weights are expected to vary with varying foreground properties.
There is a weak point to this approach. The authors use, to define their pixel ``bins'', the MEM solution derived by the WMAP team. If the MEM solution is wrong for a given pixel, that pixel will automatically be classified in the wrong pixel ensemble, and be weighted using the weights of the wrong population of pixels. To some extent then, this binning forces the result of the ILC to match the prior assumptions given by the MEM results. In turn, the MEM solution uses as a prior the result of the WMAP ILC, which is subtracted from the WMAP observations prior to using the MEM method to separate galactic foreground emissions.
As a consequence, the connection of the CMB map of Park et al. to the original WMAP data is far from direct. The map is bound to bear the signature of any arbitrary choice made before, in particular the choice of WMAP ILC regions, the 3-component model for galactic emission, and the MEM priors. For instance, discontinuities at the boundaries between the 12 regions of the WMAP ILC are clearly visible in the map of K-V spectral index used by the authors, as well as their group index (see Figs. 3a and 4a of their paper).
Park et al. then investigate the error in their reconstructed map by Monte-Carlo simulations. However, they use as an input galactic emission template the very model obtained by the MEM. This means that in the simulations, the spectral index maps are ``exact''. Therefore, the simulations accurately investigate the errors only if the MEM solution is correct, which is not likely to be the case - at least not to the level of precision required to produce a CMB map useful for precision cosmology.
Our method described in Sect. 4 uses as little prior information as possible, and aims at better angular resolution than 1 degree.
The approach of Tegmark et al. (2003), on both one year and three year data, is the only work to date which aims at producing a CMB map with both full sky coverage and best possible resolution.
Tegmark et al. (2003) have performed a foreground analysis of
the WMAP one year maps, producing two high resolution maps of the
CMB. The first one, the ``clean'' map (hereafter TILC1), is obtained by
a variant of the ILC in which weights are allowed to vary as a
function of
,
and are computed independently in nine independent
regions. The second, the ``Wiener'' map, is a Wiener-filtered version
of the same map, in which the Wiener filter is applied in harmonic
space, but independently in each zone.
This work by Tegmark et al. is an early attempt at finding linear
combinations of the WMAP data which vary both in harmonic space and in
pixel space. The pixel variation of the weights is made using zones
which are defined according to the level of contamination by
foreground emission, as computed from WMAP map differences W-V, V-Q, Q-K and
K-Ka.
The authors do not specify exactly how the frequency range is divided
into
-bands. While the text seems to indicate that weights
are computed independently for each
,
figures hint that the
weights are actually band-averaged, in 50 logarithmic bands
subdividing the multipole range. It makes a difference for the ILC bias. For an ILC implemented
by
,
the number of modes at a given
is
,
and thus remains small for most of the useful range of scales, yielding significant bias (of the order of 10% at
,
and 1% at
,
for a full sky ILC; for a part sky ILC, the bias is multiplied by a factor of the order of the inverse of the sky fraction). For band averages, the effect would be less dramatic, because of the higher number of modes per individual ILC.
In the end, the authors obtain a CMB ``clean'' map with a ``beam corresponding to the highest-resolution map band'', i.e. the beam of the W band.
The original paper describes the work done on the one year WMAP data. However maps for three year data are available on Max Tegmark's web site (see Table 1). We use the three year map (TILC3) for comparison with our own solution.
Although the approach of Tegmark and collaborators is quite good at
high galactic latitudes, we can see in Fig. 1 that
it performs poorly in the galactic plane. Also, the authors have not
removed detected point sources from the WMAP data before making the
ILC. As a result, their CMB map contains obvious point source
residuals, for instance around galactic longitude 305
and
latitude 57
,
where a 5 mK peak can be seen.
Our method, although bearing some similarity to that of Tegmark and collaborators, aims at significantly improving the error characterisation, as well as the quality of foreground cleaning in the galactic plane.
In addition to their TILC map, Tegmark et al. (2003) publish a Wiener map (hereafter TW map), obtained from the TILC map by independent Wiener filtering in the 9 regions. This results in reduced integrated error in all regions, at the price of pixel-dependent extra smoothing. The consequence of this filtering is an effective zone-dependent beam.
Because of this extra smoothing, it is difficult to compare the TW map with other maps. The most meaningful figure of merit for the Wiener map, though, is the actual power of the error (output map minus true CMB). This is unavailable for any useful up-to-date real data set. Additional discussion about Wiener-filtered maps is deferred to Sect. 6.
More recently, Kim et al. (2008) have made a CMB map from
WMAP five year data, using a ``harmonic'' ILC method (KILC5 hereafter).
Their method performs an ILC in the pixel domain but with
pixel-dependent weights.
The ILC weights are not constant over predefined zones on the sky but
are computed as smooth weight maps defined in terms of a harmonic
decomposition (hence the qualification of the method).
More specifically, the weight maps are determined by minimising the
total output CMB map variance with the constraint that these maps have
no multipoles higher than
.
For stability
reasons, the KILC5 map is obtained with
.
Prior to computing ILC weights, all maps are deconvolved from their
beam (effectively blowing up noise on small scales, in particular for
the lowest frequency channels). Then, the channels are combined using
map modes for
.
With the above choices, the reconstructed map cannot be good on small
scales. As the authors notice themselves, using small scale modes
results in minimisation of noise rather than foreground (and,
obviously, rejecting the low-frequency observations, which are the
noisiest on small scales after deconvolution from the beam). Better
results could probably be obtained by estimating weight maps for
different bands of
.
In essence, this is what our needlet
ILC method permits us to achieve.
Limiting the number of modes of the
weight maps to
,
apparently for reasons of singularity of
the system to be solved, results in spatial coherence of the weights
on scales of about 35 degrees. The galactic ridge, however, is about
1 degree thick. Hence, the spatial variability of the ILC weights
achieved by Kim et al. (2008) is not quite adapted to the
actual scale of foreground variation. The needlet ILC method
presented in our paper, as will be seen later on, solves this issue in
a very natural way.
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Figure 2:
Top: the standard deviation, per pixel for nside = 512, of the EILC1, TILC3, PILC3, WILC5 and KILC5 maps, at 1 |
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Other authors have performed various foreground cleaning processes in the WMAP observations, producing a number of CMB maps for several different models of the foreground emission. Bonaldi et al. (2007) perform component separation on WMAP data using the CCA method described in Bonaldi et al. (2006). Maino et al. (2007) obtain also several CMB maps, using the FastICA method (Maino et al. 2002). None of the CMB maps obtained is full sky, nor publicly available yet. They are not considered further in this analysis.
Finally, some foreground cleaning has also been performed by Saha et al. (2007). Their paper also includes an interesting analysis of the ILC bias. The primary goal of that work, however, is to compute the CMB power spectrum, rather than producing a CMB map.
Figure 1 shows six available maps, all displayed on the same colour scale. It illustrates the resolution and foreground contamination of the various maps. Table 1 summarises the main properties of the maps. Only the TILC1 and TILC3 maps are high resolution attempts at component separation everywhere, including the galactic plane, combining all WMAP observations. All other maps (WILC maps, EILC1, EGS3, PILC3, KILC5) are at reduced resolution.
CMB maps produced from WMAP one year data have been compared by
Eriksen et al. (2004), showing quite large differences, ranging from -100 to 100
K.
Similarly, Park et al. (2007) compare their PILC3 map with the WILC3 and TILC3 maps at 1.4 degree resolution,
showing differences in excess of 40
K.
In the following, discrepancies between these various solutions are
further investigated.
As a first step, we evaluate by how much the various maps at one degree resolution disagree over the full sky. The top panel of Fig. 2 shows the pixel based standard deviation of five such maps. In this evaluation, we exclude the EGS3 map (which is at 3 degree resolution, and is the source of additional variance in the Kp2 sky mask, where the CMB is estimated at even lower resolution).
All maps are obtained from observation of the same sky (sometimes starting from the same data set) and are smoothed to
the same resolution (one degree) where noise is small. Discrepancies originate essentially from
systematic differences in the methods. In the central
regions of the galactic plane, discrepancies are significantly higher
than 50
K (with bright spots above 90
K). In other sky
regions, they are typically in the 10-20
K range, except on
compact spots again, where they are above 50
K. The latter are
probably due to residuals of the emission from strong compact
sources. The discrepancy between the maps is greater in the ecliptic
plane, which is a signature of the impact of the instrumental noise, uneven because
of the WMAP scanning strategy. This is due to the different attention
given to minimising the contribution of instrumental noise on small scales (rather than foreground emissions) in the final map (and to a much lesser extent to the difference of noise level between the various WMAP releases).
The bottom panel of Fig. 2 focuses the comparison to larger scales (3 degree beam). At high galactic latitudes, the discrepancies are below 10
K except for a few localised regions (LMC, Ophiuchus complex) where they reach about 30
K. Differences in the North Polar Spur, at the level of 10-15
K, are also clearly visible. Close to and inside the galactic plane, systematic discrepancies significantly exceed 30
K.
Including the EGS3 map in the comparison at high galactic latitudes does not change these conclusions. Pairwise comparisons of the available maps typically show the same level of discrepancies, which indicates that the variance of the solutions is not due to one single map being in strong disagreement with the others.
The conclusion of this comparison is that foreground residuals exist in the published CMB maps at the level of about 50 to 100
K in the galactic ridge,
20 to 50
K at low galactic latitudes, and 10 to 20
K at higher galactic latitudes (above 30 degrees).
This observation calls for localised weightings, adapted to local properties of the foreground and the noise. This, however, is not easily compatible with the recovery of the largest modes of the CMB map, as pointed out before by Eriksen et al. (2004), and as demonstrated by the discontinuities observed between the CMB solutions in the different regions when the sky is cut, as in the TILC, EILC1, and WILC maps.
Our approach, then, will be to vary the relative weightings on small scales for small scale CMB reconstruction, and keep the weighting uniform over large regions of the sky for the recovery of the largest scales. This can be achieved quite straightforwardly by using the spherical needlets discussed in Sect. 4.
It is striking that all the presently available full sky CMB maps derived from an analysis of the WMAP data have been obtained by an implementation of the ILC method.
The ILC, indeed, has many advantages:
The existence of a ``bias'' in maps obtained by an ILC method is a well established fact. The derivation of this bias (which is, in fact, the systematic cancelling of a fraction of the projection of the CMB map onto the vector space spanned by the noise realisations for all the considered input maps), is given in the Appendix.
The order of magnitude to keep in mind is that about (m-1) ``modes'' of the original CMB, out of Np, are cancelled by the ILC, where m is the number of channels used, and Np the number of independent pixels or modes in the regions for which the ILC is implemented independently. Note however that when the signal is strongly correlated between pixels, the bias can be significantly larger - see the appendix for details.
The practical consequences are:
A frame is a collection of functions with properties close to those of a basis. Tight frames share many properties with orthonormal bases, but are redundant (see Daubechies 1992, for details).
Needlets were introduced by Narcowich et al. (2006) as a particular construction of a wavelet frame on the sphere. They have been studied in a statistical context (e.g. Baldi et al. 2007,2008) and have also been used recently for cosmological data analysis problems (e.g. Pietrobon et al. 2006). The most distinctive property of the needlets is their simultaneous perfect localisation in the spherical harmonic domain (actually they are spherical polynomials) and potentially excellent localisation in the spatial domain.
We recall here the definition and practical implementation of the needlet coefficents, following the generalised formulation by Guilloux et al. (2008). Let
be a collection of window functions in the multipole domain, indexed by j. Suppose that for each scale j,
is a grid of points (indexed by
)
which satisfies an exact
quadrature condition with weights
.
The needlets are axisymmetric functions defined by
Any square integrable function f on the sphere can be analysed by the scalar products
of the function f with analysis needlets. All the needlet coefficients of scale j are advantageously computed in the spherical harmonic domain, as the evaluation at points
of a function whose multipole moment are simply
.
These needlet coefficients, denoted
,
are given by:
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A key feature of the needlet decomposition follows from the localisation of the analysis functions which allows for localised processing (such as denoising, signal enhancement, masking etc.) in the needlet coefficient domain, i.e. applying some non-uniform transforms to the coefficients
.
Other types of wavelets (for instance, the steerable wavelets of Wiaux et al. 2008, or the wavelets, ridgelets and curvelets of Starck et al. 2006) could also be used for localised processing on the sphere, although the quality of the localisation depends much on the details of the wavelet design. Needlets are compactly supported in the multipole domain and can be further designed to be well localised in the direct domain according to various criteria. This permits one to work on full sky data without real need for masking the galactic ridge.
The method implemented in this work, and applied both to simulations and to the real WMAP data sets (for all releases), consists of the following steps:
Strong point sources in the input data set typically leave detectable residuals in the output ILC map, and modify at the same time the estimation of the background, leading to less rejection of other contaminants. On the other hand, their specific shape usually allows effective estimation and removal by other methods. For the purpose of this study we used information from the WMAP source catalogue (Hinshaw et al. 2007) which provides characterisation for all point sources detected above a
threshold away from the galactic plane.
For all sources identified, we subtract from the input maps a Gaussian profile at the given position and with the given flux. Conversion factors between flux density and Gaussian amplitude, as well as the FWHM of the Gaussian profile are taken from Table 5 of Page et al. (2003) for one year data, and corresponding updates for the more recent releases.
For the simulated data set, the subtraction of detected point sources is mimicked by removing from the simulation all sources above 1 Jy (independently in all channels).
In addition to the point sources subtracted above, some compact regions of strong emission (mostly in the galactic plane) exceed the rejection capabilities of the method used in this analysis, because they are too local and/or too specific. Their contribution in the wings of the needlets also contaminates the solution far from the centre of the sources. Those sources cannot be satisfactorily subtracted in the same way as the previous ones, either because they are not strictly speaking point-like, or because they are bright enough that small departures of actual beam shapes from the Gaussian model used in the subtraction step leave significant residuals. As they represent only a very tiny fraction of the sky (we single out eleven such sources), we blank out these regions in all WMAP channels, cutting out circular patches adapted to the size of the beam and of the source. Table 2 gives the list of those regions with their main characteristics.
To reduce local pollution of the needlet coefficients by the sharp cut, the small blanked regions are filled in by a smooth interpolation, so that fluctuations at a larger scale than the hole size are at least coarsely reconstructed. More precisely, interpolation is made by diffusion of the boundary values inside the hole.
Although this masking and interpolation has no reason to be optimal, it is an efficient way of reducing the impact of very strong sources on their environment. The CMB inside the masked patches is recovered (to some extent) both by the interpolation of original maps (which avoids sharp discontinuities) and by the needlet decomposition and ILC reconstruction. The masked region is tiny: 0.058% of the sky in the K channel (the most affected).
The original observations (WMAP and IRIS) are decomposed into a set of filtered maps represented by their spherical harmonic coefficients:
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For each scale j, the coefficients
are computed on a HEALPix grid at some value of nside, compatible with the maximum value of
of
band j. We use for nside(j) the smallest power of 2 larger than
,
with a maximum of 512. Details about the bands used are given in
Table 3 and Fig. 3.
Table 2: List of compact regions blanked in the pre-processing step.
Table 3: Spectral bands used for the needlet decomposition in this analysis.
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Figure 3: The spectral bands used in this work for the definition of the needlets. |
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The general idea is to independently implement the ILC on subsets of the needlet coefficients
.
For a given scale, these coefficients come in the format of a set of HEALPix maps (one per frequency channel). The ILC is implemented locally in space and locally in
as follows.
Covariance matrices
for scale j at pixel k are estimated as the average of the product of the computed needlet coefficients over some space
domain
.
Because of this, there is a trade-off between localisation and accuracy of estimation. A better estimate of the true covariance is obtained by averaging the products of needlet coefficients between all pairs of maps over a large area, but this provides an estimate of the average covariance over that area.
In practice, for the present analysis, we make use of the hierarchical property of the HEALPix pixelisation, and compute covariance matrices as the average in larger pixels, corresponding to a HEALPix pixelisation with nside = nside(j)/32. This provides a computation of the statistics by averaging
322 = 1024 samples, which results in a precision of the order of 3 per cent for all entries of the
matrix. It implies an ILC bias of order 5/1024 (for m=6 channels and Np=1024 coefficients per domain on which the ILC filter is estimated independently (see Appendix for details). Choosing a smaller area results in excessive error in the covariance estimates, and hence excessive bias. Choosing a larger area results in less localisation, and hence some loss of efficiency of the needlet approach.
We denote as
the estimate of
obtained by averaging the value of
in domain
.
On the largest scales (
), the typical angular extent of a needlet is larger than 5 degrees, and the value of nside for the map of needlet coefficients is less than 32. Covariance matrices are then computed on the full sky rather than on the largest possible HEALPix grid, i.e.
is the complete sky, rather than one of the 12 basis Healpix pixels.
Using these covariance matrices, the ILC is implemented using Eq. (4) for each domain. The estimated CMB needlet coefficients are:
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The full CMB map reconstructed from this set of needlet coefficients is our basic needlet ILC (NILC) CMB map.
For a number of purposes, in particular subtraction of an estimate of the CMB to study other emissions, it is interesting to use, instead of our ILC map at the resolution of the WMAP W channel, a map with minimal error. Such a map is obtained from the ILC map by one-dimensional Wiener filtering.
As a last processing step towards a minimum variance CMB map, we thus Wiener-filter our CMB map, to get rid of the large noise contamination at high
.
The Wiener filter is performed in harmonic space as described in 2.3.2.
The harmonic Wiener filter is given by formula 5, i.e.
.
For its implementation, we need to know the relative power of CMB and noise. We assume that the best fit CMB power spectrum of the WMAP team is correct, hence
is known. The beam factor
is assumed perfectly known as well. The denominator
can be estimated directly as the power spectrum of our output needlet ILC map.
In practice, we smooth the power spectra with
to lower the variance of the power spectrum estimator on the output needlet ILC map. Even with this, the filter is poorly estimated for low modes, because of the large cosmic variance. As can be seen in Fig. 5, the signal to noise ratio of our reconstructed map is expected to be quite high at low
.
Therefore, the Wiener filter for low modes is expected to be very close to 1. For this reason, we set
for
,
and use a linear interpolation between
and
.
The level of noise contamination (variance per pixel, and average power spectrum) in the output map is estimated by Monte-Carlo simulations, using the average of 100 realisations of the WMAP noise maps. For each initial set (i) of five noise maps (one noise map per WMAP channel), a single output noise map np(i) is obtained by performing the needlet decomposition of the initial noise maps, and filtering needlet coefficient maps with the same filter as that used on the single full simulated data set.
Denoting as np(i) and
respectively the pixel value and the harmonic space value of the noise map number i, we compute:
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The impact of the ILC bias is estimated by Monte-Carlo simulations on simulated data sets. The corresponding error is of the order of
of the CMB.
The practical implementation of this processing pipeline is made essentially using the octave language (the free software version of Matlab). The analysis is done in the framework of the pipeline tool developed by the ADAMIS team at the APC laboratory. This tool provides a flexible and convenient web interface for running our data analysis on simulations or real data with easy handling and tracing of the various pipeline options
. Single runs of the full pipeline require less than half an hour on a single processor of a standard desktop computer (dominated by harmonic transforms), whereas numerous pipelines on simulated data sets for Monte-Carlo are run on the ADAMIS 88-processor cluster, optimised for efficient I/O.
We start with a validation of our method on simulated data sets. For this experiment, synthetic observations of the sky emission are generated using the Planck Sky Model (PSM). The PSM is a flexible software library, designed for simulating the total sky emission in the 10-1000 GHz frequency range, and developed as part of the foreground modelling activities of the Planck working group on component separation (Planck WG2). Sky emission comprises galactic components of four origins (free-free, synchrotron, thermal dust, and spinning dust, with spectral emission laws for dust and synchrotron varying from pixel to pixel), CMB, kinetic and thermal SZ effects, and the emission from a population of galactic and extragalactic point sources which includes radio sources, infrared sources, and an infrared background. Although not perfect, the model sky is thought to be sufficiently representative of the complexity of the real sky emission for our simulations to be meaningful.
Sky maps are produced at WMAP central frequencies for the K, Ka, Q, V and W band, and convolved in harmonic space with approximate WMAP instrumental beams (Gaussian symmetric beams are used for these simulations). Uncorrelated, non-stationary Gaussian noise is added, with a pixel variance deduced from the WMAP sensitivity per channel and effective hit count. To mimic the subtraction of the brightest point sources detected by WMAP, we remove from the model sky, at each frequency, all sources with flux above 1 Jy (assuming they would have been detected, and can be subtracted from the data set). The 11 compact regions listed in Table 2 however, being specific to the real sky, are not blanked for the simulations.
Although these simulations provide only an approximation of the real WMAP data sets, they are representative enough that the simulated data offer a component separation challenge close to that of the real data set. The IRIS map is used as part of the full set of data for the ILC implementation on simulations.
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Figure 4: Top: the simulated input CMB map. Middle: the reconstructed CMB. Bottom: the difference (output-input), displaying the residuals left by the method. All three maps share the same colour scale, and are at the resolution of the WMAP W channel. |
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Figure 4 shows the input simulated CMB, the output CMB, and the difference of the two for one particular simulation. The reconstruction is visually good except in regions of local strong galactic emission (in the galactic ridge, for example). This is to be expected: not only can the method not remove foreground emission perfectly, but in addition the price to pay to remove the foreground (even imperfectly) is more noise (because of sub-optimal weighting of the observations as far as noise contamination is concerned).
A more quantitative estimate of the level of contamination of the CMB map by foreground emissions and noise is obtained by looking at power spectra. Figure 5 shows the input simulated CMB power spectrum (dotted line), the spectrum of the output CMB (solid black line), and the spectrum of the map of residuals (difference between output and input, dashed line), both full sky (top panel) and in the HGL region (bottom panel). The angular power spectrum of the residual map is seen to be small compared to the CMB power on large scales, the two being comparable at
.
Noise dominates on smaller scales. The residuals due to the presence of galactic emission are seen to contribute power essentially below
,
where the power of the difference map is seen to be slightly higher in the full sky power spectrum than in the HGL power spectrum (this is visible, in particular, at the top of the first acoustic peak).
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Figure 5: Top: for simulated data sets, full sky power spectra of the output CMB map (plain line), and the difference map (dashed line). The CMB model used in the simulation is over-plotted as a dotted line. Bottom: same at high galactic latitude only (HGL region). |
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As discussed in 4.2, we expect a (small) bias in the ILC map, due to empirical correlations between the CMB emission and contaminants (including noise and foreground emission). This is not particular to our approach, and is expected for any ILC method. For better characterisation of our output map, we evaluate the effect both theoretically (in the Appendix) and numerically.
Although a general analytic estimate of the bias is complicated, Appendix A shows that (to first order at least and for reasonable assumptions about the CMB, foreground emissions, and noise) the amplitude of the effect does not depend much on what the actual foreground emissions are in detail, but is set essentially by the geometry of the domains considered (through a number of effective modes). It is then possible to estimate the amplitude of the effect by Monte-Carlo simulations on synthetic data sets resembling the actual WMAP observations.
Figure 6 illustrates an estimate of the bias
as a function of the harmonic mode, computed as a fractional error:
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Figure 6:
The fractional bias in the ILC map as a function of |
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We now turn to the description of the results obtained on the real WMAP data sets. In order to facilitate the comparison with existing maps, we process independently one year, three year and five year data, to obtain three CMB maps (hereafter NILC1, NILC3 and NILC5). For each year, we use the beam estimates, noise level, and point source catalogue provided with the corresponding release.
The improvement of CMB reconstruction with consecutive data releases is illustrated in Fig. 7, which shows the full sky power spectra of the NILC CMB maps obtained with one year, three year, and five year WMAP data. The power spectra displayed are the raw power spectra of the output map, computed for the full sky, and smoothed with a variable window in
of 10% width. While the lower part of the spectrum, cosmic variance limited and CMB dominated, does not change much, the high
spectrum of the map, dominated by noise, decreases substantially with increasing observation time - as expected. The excellent agreement at low
(up to
)
between the power spectra and the model is striking. The bumps in the spectrum due to the first and second acoustic peaks are clearly visible on the five year map spectrum.
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Figure 7: Power spectra of the NILC map for one year, three year, and five year WMAP data. |
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Figure 8: Top: the NILC5 reconstructed WMAP CMB at the resolution of the W channel. Middle: the harmonic Wiener NILC5 CMB map. Bottom: the NILC5 CMB map at 3 degree resolution. |
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Figure 9:
Power spectrum of the reconstructed WMAP
CMB map. For each of the two panels, the CMB best fit model is shown as a solid black line, and power spectra computed at low galactic latitudes (using the LGL mask), on the full sky (no mask), and at high galactic latitudes only (HGL mask) are displayed as dashed lines. Note that the map spectra plotted here are directly those of the maps, without any correction for the beam. Top panel: ILC map of (Tegmark et al. 2003, TILC3). Bottom panel: this work, with five year WMAP data. The power spectrum of the needlet ILC CMB is significantly more homogeneous than the power spectrum of the TILC3 map. We interpret this difference as an indication that the TILC3 map is significantly more contaminated by residuals of galactic emission. Note the different scales of the y-axis, and the improvement on small scales, with a noise power of about 0.024 mK2 at
|
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Our full-sky reconstructed CMB map for the five year observations, at the resolution of the W-channel, is displayed in the top panel of Fig. 8.
A full comparison of our needlet ILC maps (for all data releases) with all the other available maps would be too long for the present discussion. Rather, we decide to compare our five year result only with the TILC3 map on small scales (choice is motivated by the fact that the TILC is the only other full sky high resolution map available), and with the EGS3 map on large scales. This is of particular interest, as the EGS3 is the only map obtained with a method not based on the ILC, and also is a method specifically implemented for the recovery of the largest scales.
On the smallest scales, we compare our needlet ILC map with the TILC and with the WMAP foreground-reduced W band. Figure 10 shows local regions of the foreground-reduced map, the NILC5 map, and the TILC3 map, in the galactic plane and at the galactic pole. Our needlet map is clearly less contaminated by galactic emission than the other two. At high galactic latitude, the NILC5 and TILC3 are visually comparable, while the foreground-reduced map appears to be more noisy, as expected.
The power spectrum of the output map for the five year data (NILC5 map), for three different sky coverages, is shown in the bottom panel of Fig. 9. On the same panel, we plot the angular power spectrum
corresponding to the WMAP best fit model, corrected for the W-channel beam. On the top panel of the same figure, we show the same power spectrum estimates for the TILC3 map. This shows the improvement achieved by our method close to the galactic plane. This improvement is due both to the needlet approach and to the use of the IRIS map to help with dust subtraction. As seen in Fig. 7, the difference in quality between NILC5 and TILC3 cannot be explained solely by reduced noise (NILC5 and NILC3 being very close in quality for all scales except the smallest ones).
Figure 11 gives a visual comparison of NILC5 (this work) and the EGS3 (Eriksen et al. 2007), as well as of NILC5 and KILC5 (Kim et al. 2008). In the top row, we display the EGS3 and KILC5 at a resolution of 3 degrees, and degraded to nside = 64. The bottom row shows the difference between our needlet ILC solution (displayed on the bottom panel of Fig. 8) and these two maps.
The most striking difference between the five year needlet ILC map and the EGS3 is in the galactic plane, where the EGS3 does not recover the intermediate angular scales. The difference, however, shows no particular clear structure, as expected if it is the random realisation of a Gaussian random field. It is thus probably essentially due to the difference between our CMB reconstruction on scales larger than 3 degrees, and the CMB on larger scales that can be inferred from the CMB reconstructed by Eriksen et al. outside of their galactic mask. At higher galactic latitude, the two maps are in good agreement, with no obvious feature which could be correlated to foreground emissions or to the CMB itself, with the exception of a hot spot in the large Magellanic cloud (which might be residual emission of the LMC in our map, as Eriksen et al. (2007) actually mask the centre of the LMC and obtain a solution in the direction of the LMC by extrapolation from nearby pixels).
Above 30 degree absolute galactic latitude, the rms of the difference
between our 3 degree map and the EGS3 map is 5.7
K. The two maps are in much better agreement than the EGS3 and the WMAP MEM model maps (see Fig. 3 in Eriksen et al.). Note however that theoretically, if there were no foreground in the WMAP data, the noise standard deviation
on a 3 degree map obtained by noise-weighted averaging using all WMAP channels would be about 3.2
K for three year data. If instead we assumed that only the three highest frequency channels are free of foreground contamination,
would be 4.4
K.
The difference between our map and the KILC5 map is more systematic with, in particular, stronger differences in the galactic plane, in spite of the fact that the two methods work on the same input data set. A careful visual inspection of the CMB maps themselves gives the impression that the KILC5 map is probably systematically negative towards the galactic central regions. There is, however, no secure way to be certain which map is best.
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Figure 10:
CMB maps from WMAP three year data obtained with three techniques:
left column: WMAP foreground reduced, W channel;
middle column: our needlet ILC map;
right column: the TILC map. The top line corresponds to a patch located in the galactic plane, centred around coordinates
|
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Figure 11: Top left: the EGS3 map. Top right: The KILC5 map, smoothed at 3 degree resolution. Bottom left: the difference NILC5-EGS3; we see is a clear difference in the galactic plane with no particular structure, compatible with a smooth Gaussian field, where the EGS3 solution poorly estimates intermediate scales; a patch in the difference map at the location of the Large Magellanic Cloud is clearly visible also. Bottom left: the difference NILC5-KILC5; a clear structure aligned with the galactic plane is clearly visible, with a large difference towards the galactic center. |
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The effective beams of the reconstructed maps are plotted in Fig. 12, for both the full resolution five year needlet
ILC map, and for the Wiener-filtered version. The map has been reconstructed for the range
,
with a smooth transition of the response, between
of 1024 and 1200, from the nominal W band beam value to 0. This smooth transition allows us to avoid ringing effects which happen in the case of a sharp cut-off in
.
The ratio of the Wiener beam (dashed line) and ILC beam (solid line) gives a measure of the signal to noise ratio in each mode.
Given the ILC filter computed on the real data set, the level and properties of the instrumental noise can be straightforwardly computed by applying the same filter to simulated WMAP noise maps. From 100 noise realisations, we compute the average full-sky noise power spectrum (Fig. 13), as well as the noise standard deviation per pixel (Fig. 14). Noise properties are not as simple as one may wish: the noise is non stationary, because of both the uneven sky coverage and of the localised processing. It is also somewhat correlated pixel-to-pixel, in particular close to the galactic plane. This is unavoidable, but fortunately our pipeline allows us to make as many Monte-Carlo realisations of the instrumental noise as needed for any scientific study made using our needlet ILC map. One hundred such simulations are made available as part of our main data products.
More problematic is the evaluation of the contamination of the CMB map by foreground residuals. It requires prior information about the foregrounds, which the ILC method avoids using. An indication of the level of systematic uncertainty is obtained from the comparison of the various solutions (Fig. 2). An other option consists of checking the contamination on simulations. Figures 4 and 5 give an idea of the expected contamination from such simulations. This, however, is good only as long as the simulations are representative enough.
The comparison of the power spectrum of the output CMB map computed at high and low galactic latitude (Fig. 9), and a visualisation of the output CMP map at high and low galactic latitude (Fig. 10) also give an idea of the amount of galactic residuals, but none of these estimates is fully satisfactory for careful CMB science. This is, however, not particular to our map. No published CMB map is available with a good estimate of foreground contamination. Although this, clearly, is not fully satisfactory, we leave further investigations on this question for future work.
In the present work, we have obtained a CMB map which has been shown to be significantly less contaminated by foreground and noise than the other existing maps obtained from WMAP data. A natural question is whether we can do even better.
In the following, we outline where there is margin for improvement, and explain why we have stopped the analysis at its present state.
First, the present analysis uses only limited external information and data sets: WMAP point source detections, and the IRIS 100 micron map. It is likely that something could be gained by using additional observations to help constrain the galactic emission.
Second, there is a trade-off between localisation of the estimation of covariance matrices, and bias in the ILC. The estimation of covariance matrices
over sets of
needlet coefficents results from a compromise which has been made based on varying Np in simulations, but has not been optimised in any way. In addition, the optimal solution is probably different at high galactic latitudes, where weights given to different channels probably do not vary much and thus require less localisation, and at low galactic latitudes, where the complexity of galactic emission calls for more localisation. We have tried to use
(more localised ILC filters, but more bias) and
(less localised ILC filters, but less bias). Our choice of
seems, in simulations, not worse than anything else (nor much better either). The bias error has been verified to remain below the reconstruction error due to the contribution of the noise for small scales, and below cosmic variance uncertainty for large scales (see Fig. 13), and remains below an acceptable level of a few percent.
Similarly, the choice of the spectral window functions used on this data set has not been the object of specific optimisation. At low
,
we follow a ``dyadic'' scheme, where each window reaches an
of about twice the previous one. Wide spectral window functions allow for more localisation in pixel space, but narrow window functions allow for more accuracy in the harmonic domain. At
high
,
because of the variation of the beams with
,
the relative noise levels of the different channels change quite fast with
,
which calls for more localisation in
space. Here again, the optimal window functions are probably not the same at high and at low galactic latitudes. In practice, we chose a small number of bands to limit the number of harmonic transforms in the pipeline and allow reasonable localisation of the analysis.
The choice we have made results from the principle of simplicity. We have tried to devise a pipeline which depends as little as possible on external data, on priors, or on fine tuning. A very simple scheme has permitted us to obtain a CMB map convincingly better than other maps available. This does not preclude any attempt at more optimisation for future work if needed.
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Figure 12: Harmonic response of the beam of the NILC5 CMB map and of the Wiener-filtered version. |
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Figure 13:
Plot of the power spectrum of the noise (solid line). The spectrum for the WMAP best fit model is shown as a solid line, for comparison. The dashed line is 2% of the WMAP best fit |
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Figure 14: Map of the standard deviation of the noise, per pixel at nside = 512, for the five year needlet ILC map at the resolution of the W channel. The adaptation of the filter to local contamination is obvious from the uniform noise level in large healpix pixels, in particular in the galactic plane. These large healpix pixels correspond to nside = 16, which is the size used to compute the average filter for the smallest scales. This illustrates the impact of the compromise between subtracting foreground emissions and increasing the noise with the use of the lower frequency channels, which have poor sensitivity on small scales. |
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It is certainly possible to tune our pipeline, changing some of its parameters. It would be possible also to use methods other than an ILC, for instance Independent Component Analysis (ICA) methods such as SMICA (Delabrouille et al. 2003; Cardoso et al. 2008), or more generally maximum likelihood methods fitting parametric models of the foreground emissions in the data sets. Such methods extract information about the foreground from the data directly, possibly with the help of ancillary data sets, and use this information to clean the observations in some way.
In the present case however, it is not very likely that such attempts would give much better results than what is obtained here, unless one uses a very significant number of additional data sets and safe prior information. Indeed, the WMAP data consists of five channels only, from which a component separation method based on a meaningful model of foreground emission needs to extract CMB, synchrotron, free-free, spinning dust, thermal dust (i.e. five templates), and possibly also point sources, and variations of the spectral indices of some of the components - not to mention special regions of galactic emission such as cold cores and H-II regions, nor particular objects such as nearby resolved galaxies or galaxy clusters. Any component separation method based on the estimation of parameters for such a rich model would almost certainly be confronted with indeterminacy issues. Methods based on a precise model are expected to be effective when the data are very redundant as compared with the number of ``parameters'' of the emission model, which would not be the case here. Hence, the ILC is probably one of the best approaches for performing component separation on WMAP data. It is not surprising, then, that all methods producing full sky CMB maps from WMAP, or nearly so, implement some variant of the ILC.
Incidentally, ICA methods could benefit from the needlet framework.
In this paper, we have described a new approach to implement CMB extraction in WMAP data, using the ILC method on a needlet frame. Tests on simulations show excellent performance of the method, thanks to localisation both in pixel space and in harmonic space. Localisation in pixel space allows the ILC weights to adapt themselves to local conditions of foreground contamination and instrumental noise (this is essentially the reason why the NILC performs better than the TILC, in particular in the vicinity of the galactic plane). Localisation in harmonic space allows us to favour foreground rejection on large scales (where foreground emissions dominate the total error) and instrumental noise rejection on small scales (where foreground emissions are negligible but where, after beam deconvolution, the relative noise level between the various WMAP channels varies a lot as a function of scale). Needlets permit us to vary the weights smoothly on large scales, and rapidly on small scales, which is not possible by dividing the sky in zones prior to any processing.
As a further improvement on previous work on WMAP data, we include a dust template in the set of analysed observations. This is motivated by the fact that on the smallest scales, observed with reasonable signal to noise ratio by the W channel only, dust emission contributes a significant fraction of the total reconstruction of the map. Using the IRIS 100 micron map as an additional observation enables the ILC to reduce the final contamination by dust -thanks to correlations of dust emission between the W channel and the 100 micron map. Special care was also taken to subtract a number of strong point sources from the data prior to the ILC.
As discussed at length in the main text and in the Appendix, the implementation of a filter (the ILC) based on empirical estimates of covariance matrices leads to a bias. This is not particular to our map, but is the case for any ILC map. We have estimated the level of this systematic effect, both analytically and numerically, to be at the level of a few per cent on all scales. Our simulation tool allows us to make accurate estimates of the amplitude of the effect, if needed for any scientific exploitation of the NILC5 map.
The application of the method to WMAP one year and three year data (in
addition to five year data) allows us to compare the needlet ILC solution
to previous work. Our map is seen to be at least as good as others on
large scales, while being significantly less contaminated by residual
foreground and noise than others on small scales, in particular in
the vicinity of the galactic plane. The application of the method to
WMAP five year data yields a CMB map which we believe to be the cleanest
full sky map of the CMB to date. Contamination by noise, and the power
loss due to the use of the ILC method, are characterised by means of
Monte Carlo simulations. The map is available for download on the
ADAMIS web
site
,
and can be used for a variety of science projects relying on accurate
maps of the CMB.
Acknowledgements
The ADAMIS team at APC has been partly supported by the Astro-Map and Cosmostat ACI grants of the French ministry of research, for the development of innovative CMB data analysis methods. We acknowledge the use of the Legacy Archive for Microwave Background Data Analysis (LAMBDA). Support for LAMBDA is provided by the NASA Office of Space Science. The results in this paper have been derived using the HEALPix package (Górski et al. 2005). The authors acknowledge the use of the Planck Sky Model, developed by the Planck working group on component separation, for making the simulations used in this work. Our pipeline is mostly implemented in octave (http://www.octave.org).
In this appendix, we compute the error made after CMB reconstruction with the ILC and some of its statistical properties. In particular, we derive the correlation of the error with the true CMB signal, which yields a non unit effective ``response'' of the ILC filter - and hence a bias in the reconstructed map and in the CMB power spectrum computed from it. This bias has to be accounted for properly for further use of the reconstructed CMB map.
We model the data as:
| (A.1) |
The ILC is best applied over domains of p where all coefficients have
(near) uniform expected signal and noise properties, so that the ILC
weights are optimal simultaneously for all p. In particular, the
rms values of all maps do not depend (much) on p in a given domain.
Hence, we concentrate on one given domain of p for which we assume
that the sequences sp and
are independent, Gaussian random
variables with distribution
and
,
with
the variance of sp (the
CMB) and
the covariance matrix of the noise (including
foreground emissions).
The ILC estimate of sp in domain
is given, for
all p, by
![]() |
(A.2) |
We are interested in the reconstruction error:
![]() |
(A.5) |
The ILC being constructed so that the response to the signal of interest is unity, only the filtered noise term contributes to the error dp, which can then be written as:
| dp | = | ![]() |
(A.7) |
| = | ![]() |
(A.8) |
![]() |
(A.9) |
![]() |
(A.10) |
| = | |||
![]() |
(A.11) |
![]() |
(A.12) |
From Eqs. (A.3) and (A.4), we can write
in the form:
![]() |
(A.14) |
![]() |
(A.15) |
![]() |
(A.16) |
![]() |
(A.17) |
The two last terms (small correction terms) in Eq. (A.13), being proportional to
,
can be decomposed each into the sum of three terms, proportional to
,
,
and
respectively. The signal and noise realisations enter the
term as products of terms of the form
only, the
term as products of terms of the form
.
On the contrary, signal and noise realisations enter the
term as the product of terms in the form
,
i.e. products of s and the second power of
.
Index q runs over domain
.
Assuming that s and
are centred variables, the mean value of the error is immediately seen to vanish:
| E(dp) = 0 . | (A.18) |
![]() |
(A.19) |
![]() |
(A.20) |
![]() |
(A.21) |
As mentioned previously, under the assumption that the signal of interest is not correlated to the noise and the foregrounds, the first term (main term) of the r.h.s. of Eq. (A.13) does not give rise to multiplicative errors (or correlation of dp with sp). Similarly, the corrective term proportional to
,
multiplied by s, gives terms which contain an odd power of s and an odd power of
,
and does not give rise to correlations. This assumption is correct, to excellent accuracy, when the signal of interest is CMB anisotropies
. We are left with:
| E(sp dp) | = | ![]() |
|
![]() |
(A.22) |
Although allowing the statistical derivation of the (anti-) correlation of the reconstruction error with the original CMB, the above derivation is not very illuminating about the mechanism giving rise to this CMB power loss. A geometrical reasoning gives better insight into what is actually going on.
For a given data set, the ILC works on one single realisation of all random fields. For an independent implementation of the ILC on Np pixels (or modes, or needlet coefficients) of the observations, each data set is represented by a vector in an Np-dimensional vector space W. The CMB
,
the observation
for each channel i, and each of the noise realisations
(including foreground emissions) are elements of W.
The collection of vectors
defines an m-dimensional subspace V of W. This is true irrespective of the nature of the foreground contaminants: indeed, although in principle vectors
could be linearly dependent, this happens in practice with vanishing probability (in particular if the observations are noisy).
Vector space W can thus be decomposed in two orthogonal subspaces, U and V, where V is the m-dimensional sub-space spanned by all vectors
,
and
is a (Np-m) dimensional vector space. The CMB itself can be decomposed into two components, one in U, and one in V:
| (A.27) |
| |
Figure A.1:
Geometric illustration of the ILC bias. The true CMB (blue) and the output CMB (red) are elements of
|
| Open with DEXTER | |
What happens when the ILC is made is the following: we look for weights wi for all channels, that minimise the variance of the reconstructed map, i.e. minimise the norm of vector
,
under the constraint that
.
We have:
| |
= | ![]() |
|
| = | (A.28) |
The noise contribution to
appears as a linear combination of vectors
.
For varying values of wi such that
,
this linear combination spans an affine subspace S of V. S is of dimension m-1 (an hyperplane). Defining K as the vector subspace of V spanned by linear combinations
such that
,
we obtain S as:
| (A.29) |
We note that the vector subspace K depends only on noise realisations, and not on
nor on the final ILC weights (the latter only defining a single point on S - and on K by orthogonal projection). Hence, the direction of the one-dimensional vector subspace H of V orthogonal to K is also independent
of
and of the final ILC weights.
For any element
of affine space S the norm of
is the sum of the norms of its projections onto K
and H.
Allowing weights wi to vary, vector
spans S, and hence only the norm of the projection of
onto K varies (and not its projection on H). The minimum is reached when the projection of of
onto K vanishes. When this happens, the ILC has cancelled completely the linear combination of projections of
and
onto the m-1-dimensional space K, and left untouched the projections of
and
onto the Np-m+1 dimensional vector space
.
Assuming the CMB to be Gaussian and statistically isotropic, its
coefficients in any orthogonal basis are Gaussian distributed random
variables with variance
(since the sum must have total
variance
). It follows straightforwardly that the
correlation of the recovered CMB map with the input CMB map is
(Np-m+1)/Np, and that the ``bias'' is due to the loss of m-1 modes
of the original CMB, which have been unlucky enough to ``live'' in the
(m-1) dimensional space K.
The above derivation in Sect. A.1 assumes the independence of coefficients
and/or of coefficients sp, i.e.
and/or
.
When this assumption does not hold, we have:
| E(sp dp) | = | ![]() |
|
| (A.30) |
![]() |
(A.34) |
![]() |
(A.35) |
Assuming that neither the noise level nor the CMB power vary much over the spectral window
,
and
are approximately independent of
,
and can be taken out of the integral. We get:
![]() |
(A.36) |
![]() |
(A.37) |
![]() |
(A.38) |
![]() |
(A.39) |
Hence, we define an effective number of modes,
,
where
![]() |
(A.41) |
![]() |
(A.42) |
![]() |
(A.43) |
![]() |
(A.44) |