ABSTRACT

The first observations of the cosmic microwave background (CMB) from NASA's Wilkinson Microwave Anisotropy Probe (WMAP) led to finding ‘alignment’ anomalies not expected from fluctuations in the isotropic cosmological model. We study the data of all 8 full-sky public releases since then to test for anomalous alignments and shapes of the first 60 multipoles, i.e. over the range |$2\le l \le 61$|⁠. We use rotationally invariant and covariant statistics to test isotropy of all subsequent WMAP data releases, along with those from the ESA’s Planck mission. Anomalous alignments among the multipoles |$l=1, 2, 3$| are very consistent and robust. More alignments are detected, some of them new, while significance is diluted by the large range of the search. Power entropy, a measure of the randomness of the multipoles, is consistently anomalous at about |$2\sigma$| level or better across all data releases. It appears that the CMB is not as random as the cosmological principle predicts on large angular scales.

1 INTRODUCTION

The cosmological principle is a foundational assumption of modern cosmology. Though merely a simplifying assumption initially, the assumption became a principle when its far-reaching implications became appreciated. A large body of current cosmological data, and particularly observations of the cosmic microwave background (CMB), invite testing the assumption of isotropy. Since isotropy is a symmetry, it is beautifully well defined to enable model-independent tests. Tests began with release of the first year data from NASA’s Wilkinson Microwave Anisotropy Probe (WMAP) space mission, when full-sky high-resolution cleaned CMB maps were made publicly available for the first time (Bennett et al. 2003a,b).

It is important to know that the CMB ‘power’ statistic (conventionally |$C_{l}$|⁠) is a rotationally invariant number that itself has no information about rotational invariance (statistical isotropy) of the data. All directional information is summed out in computing |$C_{l}$|⁠. As a result, other statistics are needed to test the directional features of the CMB. Anomalous alignments among low multipoles of CMB temperature sky were one of the first instances of isotropy violation seen in the CMB sky (Copi, Huterer & Starkman 2004; de Oliveira-Costa et al. 2004; Ralston & Jain 2004). The phenomena gained significant attention from the cosmology community by potentially indicating a preferred direction for our Universe (Bielewicz, Górski & Banday 2004; Schwarz et al. 2004; Bielewicz et al. 2005; Land & Magueijo 2005; Abramo et al. 2006; Copi et al. 2006, 2015; Samal et al. 2008, 2009; Gruppuso & Gorski 2010; Pinkwart & Schwarz 2018; Oliveira, Pereira & Quartin 2020). As new full-sky CMB maps from WMAP and later from ESA’s Planck space probe became available, many of the anomalies were found to still persist. See, for example, Schwarz et al. (2016), Bull et al. (2016), and Aluri et al. (2023) for a review and current status of various instances of isotropy violation seen in cosmological data including CMB. The WMAP and Planck collaborations themselves made a dedicated analysis of these anomalies and found them to be at a similar significance (Bennett et al. 2011; Planck Collaboration XXIII 2014; Planck Collaboration XVI 2016; Planck Collaboration VII 2020). No interpretations are agreed, and some attributed the observations to chance occurrences. Possible correlations between some of these anomalies were explored, for example, in Muir, Adhikari & Huterer (2018). The current status of some of the anomalies in (E-mode) polarized CMB sky vis-a-vis the anomalies originally seen in CMB temperature data were studied, for example, in Shi et al. (2023).

In this paper, we are particularly interested in testing statistical isotropy of CMB modes across all full-sky CMB data releases. The maps available include WMAP’s 1 yr to (full) 9 yr data, and Planck’s nominal, full, and legacy mission data sets. Unless otherwise specified, a multipole is ‘anomalous’ if the p-value of an associated statistic is less than 5 per cent. We treat all releases uniformly, while determining significance with exhaustive case-by-case simulations for each release. From each data set, we study multipoles in the range |$2\le l \le 61$|⁠. We note that a statistical penalty will exist for conducting extensive random searches. So, rather than tuning the range of study, we decided to accept the penalty of reviewing a wide range of multipoles for the sake of uniformity. Our results shed light on the nature and robustness of anomalous features of CMB modes with the accumulation of data over the years. In brief, some statistics give no evidence against the isotropic null hypothesis. Yet too many other statistics too often contradict isotropy, which simply does not fit the data.

2 ANALYSIS PROCEDURE

In this section, we outline the methods and statistics used here to probe anisotropy and alignments among CMB multipoles. We primarily use the power tensor (PT) method (Ralston & Jain 2004) that is briefly described below.

2.1 Power tensor

CMB anisotropies are akin to signal on a sphere, and are thus expanded in terms of spherical harmonics, |$Y_{lm} (\hat{n})$|⁠, which form a suitable basis as

(1)

where |$\hat{n}=(\theta ,\phi)$|⁠, being the position coordinates on a sphere. Here, |$\Delta T(\hat{n})$| represents CMB temperature anisotropies and |$a_{lm}$| are the coefficients of expansion in that basis. The contributions of |$l=0, \, 1$| are conventionally treated separately, while we will return to |$l=1$| in another section.

Power tensor ‘|${\bf{A}}_{ij}$|’ is then defined as the quadratic estimator involving |$a_{lm}$| as

(2)

where |${\bf{J}}^i$| and |${\bf{J}}^j$| are the |$(2l+1)$| dimensional angular momentum operator matrices: |$\lbrace \bf{J}^x,\, \bf{J}^y,\, \bf{J}^z\rbrace$|⁠. Thus, |${\bf{A}}_{ij}$| is a |$3\times 3$| matrix whose eigenvalues and eigenvectors inform us of the nature of a particular multipole ‘l’ we are interested in. The purpose of the PT is to develop directional statistics for every multipole. We refer to the eigenvector corresponding to the largest eigenvalue as the principal eigenvector (PEV or PT-PEV) and assign this as an axis of anisotropy for a multiple. When needed, we will use the symbol |$\tilde{\boldsymbol{ e}}_l$| to denote a PEV corresponding to a multipole ‘l’. Note that eigenvectors are headless, meaning that they do not represent a vector with a signed direction, but instead represent an axis.

PT in equation (2) is defined so that when isotropy holds the expectation value is given by

(3)

where |$C_l$| is the underlying angular power spectrum of the CMB temperature anisotropies. Thus, the eigenvalues add up to the total power, |$C_l$|⁠, in a multipole ‘l’. In terms of its eigenvalues and eigenvectors, PT can thus be written as

(4)

where |$\Lambda ^\alpha$| and |${\boldsymbol{ e}}^\alpha$| (⁠|$\alpha =1,2,3$|⁠) are the three eigenvalues and eigenvectors respectively, and |$i,j=\lbrace 1,2,3\rbrace$| denotes components of the eigenvectors, |${\boldsymbol{ e}}^\alpha$|⁠.

Let us denote the normalized eigenvalues as |$\lambda _\alpha = \Lambda _\alpha /(\sum _\beta \Lambda _\beta)$|⁠. To characterize anisotropy of a multipole ‘l’, we use what is called the power entropy (PE) defined as

(5)

This is the same entropy defined by von Neumann and Shannon. When extracted from a density matrix (a normalized positive definite matrix, such as PT), it is the entropy of quantum information theory (Ballentine 2015). Thus, PE is a true information entropy measuring the randomness of the eigenvalues of PT.

Here are some of its properties: In essence, PT maps the intricate pattern on the sphere corresponding to a multipole ‘l’ on to an ellipsoid. The (normalized) eigenvalues of PT tell us how deformed the ellipsoid is, and the direction of the largest eigenvalue can be taken to represent a preferred direction for that multipole. When isotropy holds, all eigenvalues are equal, viz. |$\lambda _\alpha =1/3$|⁠, as is obvious from equation (3). This represents a perfectly symmetric case for a multipole that is mapped to a sphere. On the other hand, when a multipole is highly anisotropic, it is mapped to an ellipsoid that is highly deformed (like a prolate spheroid) along its semimajor axis that naturally reveals an axis of anisotropy. Thus, following equation (5), PE of a CMB mode falls in the range |$0\le S(l) \le \ln (3)$|⁠. If |$S(l)$| reaches the upper limit, the multipole is maximally isotropic with no preferred orientation. The lower limit represents maximal anisotropy indicating a preferred single axis given by a PEV with eigenvalue ‘1’, and a pattern of eigenvalues {0, 0, 1}.

The significance of any deviation from isotropy of a multipole is assessed by comparing its PE observed in the data, |$S_{\rm obs}(l)$|⁠, with the PE distribution from simulations, {|$S_{\rm sim}(l)$|}. Generating simulated data release by release, incorporating the instrument properties appropriately, is a demanding task that will be described later.

2.2 Alignment statistic for testing low-l alignments

Independent of the eigenvalues of PT of a particular multipole, PEVs from different multipoles can themselves be used to compare alignments among multipoles. A natural way to do so is to define the quantity ‘|$x_{l l^{\prime }}=1-\cos (\alpha _{ll^{\prime }})$|’ as an alignment statistic where  |$\tilde{\boldsymbol{ e}}_l$||$\cdot$||$\tilde{\boldsymbol{ e}}_{l^{\prime }}$||$= \cos (\alpha _{ll^{\prime }})$|⁠, and |$\alpha _{ll^{\prime }}$| is the angular separation between the PEVs of any two multipoles l and |$l^{\prime }$|⁠. We can replace symbol |$x_{l l^{\prime }} \rightarrow x$| when the context is clear.

The standard model of cosmology defines the null model. In this model, CMB temperature anisotropies come from an isotropic Gaussian random field on a sphere. The statistic ‘|$x=1-\cos \alpha$|’ follows a uniform distribution in the range [0, 1] in the standard cosmological model. To show this, compute the area of a spherical cap subtended from an arbitrary z-axis to a polar angle |$\alpha$|⁠. The result is then multiplied by a factor of ‘2’ because PEVs are headless, i.e. undirected axial quantities.

2.3 Alignment tensor

Collective alignments over a range of multipoles are tested using what is called an alignment tensor (AT) ‘|$\bf{X}$|’. It is constructed from PEVs (⁠|$\tilde{\boldsymbol{ e}}_l$|⁠) of power tensor, whose decomposition is shown in equation (4). It is defined as (Samal et al. 2008)

(6)

Here, the sum is over the selected range of multipoles |$l=[l_{\mathrm{ min}}, l_{\mathrm{ max}}]$|⁠, |$\tilde{e}^i_l$| are the components of PEVs, and |$N_l$| is the number of multipoles in the sum. AT can also be computed for a chosen set of multipoles to find their collective alignment axis.

Let |$\zeta _\alpha$| and |${\boldsymbol{ f}}_\alpha$| (⁠|$\alpha =1,2,3$|⁠) be the three (normalized) eigenvalues and eigenvectors of AT, respectively. The eigenvector corresponding to the largest eigenvalue of AT will be referred to as AT-PEV, denoted by |$\tilde{\boldsymbol{ f}}$|⁠. This eigenvector can be taken to represent the collective alignment axis for any set of multipoles.

Information about the eigenvalues of AT is found in the alignment entropy (AE), defined as

(7)

Just as PE, AE also varies in the range |$0\le S_X\le \ln (3)$| where the lowest value, 0, indicates perfect alignment of PEVs and the highest value, |$\ln (3)\approx 1.1$|⁠, implies perfect isotropy. When |$S_X\rightarrow 0$|⁠, then |$\tilde{\boldsymbol{ f}}$| represents a collective alignment axis that has been repeated with little variation in the ensemble. It is tempting but false to assume that small |$S_X$| would be a direct measure of statistical significance of the direction of |$\tilde{\boldsymbol{ f}}$|⁠. This is because the eigenvalues and eigenvectors of AT are independent. In the null model, the eigenvectors of AT are distributed isotropically independent of the eigenvalues. In a model representing anisotropy, different samples might have a consistent and statistically significant AT-PEV whether the AT entropy is small or not. More discussion of this appears in Section 4.8 where it is applied to data.

2.4 Comparing multiple statistics

Much of the study follows a standard procedure of choosing a threshold p-value, denoted by |$\mathbb {P}$|⁠, as the criteria to determine when an observed p-value of some statistic will be deemed anomalous. (We will postpone criticism of this procedure for later.) We generally choose |$\mathbb {P}=0.05$|⁠, i.e. probability of random chance occurrence of 5 per cent or less (corresponding to a |$2\sigma$| significance or better). Suppose we find |$k_*$| anomalous modes with |$p\le \mathbb {P}$| out of n multipoles being analysed. Then, the cumulative binomial probability with respect to this threshold p-value is

(8)

This is a much more refined estimate than assuming that ‘k’ instances of an event with a probability |$\mathbb {P}$| would occur with probability |$\mathbb {P}^{k}$|⁠. Its weakness, however, is that an artificial threshold ‘|$\mathbb {P}$|’ is chosen to begin with, which creates a bias against counting the most significant statistics. Section 4.2 discusses a more complete statistic based on the likelihood of the data in the null distribution. Section 4.3 discusses how the distribution of p-values is used in a classic test of the null distribution.

In some cases, we also test an entire distribution of statistics against the corresponding null distribution. If |$P(x)$| is the theoretical probability distribution function of some statistic ‘x’, then the corresponding theoretical cumulative probability distribution function (tCDF) is |$\mathcal {P}(x)=\int _0^x P(x^{\prime })\, \mathrm{ d}x^{\prime } $|⁠. Let the empirical cumulative probability distribution function (eCDF) be denoted by |$\mathcal {P}_i$|⁠. It is obtained by sorting the statistic ‘x’ in ascending order and assigning |$\mathcal {P}_i = i/N$|⁠, where N is the number of elements in the set. Then, the Kuiper statisticV’ is used to compare a tCDF with an eCDF. It is defined as (D’Agostino & Stephens 1986)

(9)

where |$D_+ = \max \lbrace \mathcal {P}_i-\mathcal {P}(x_i)\rbrace$| and |$D_- = \max \lbrace \mathcal {P}(x_i)-\mathcal {P}_{i-1}\rbrace$|⁠, each representing the maximum positive deviation of eCDF above the tCDF and maximum negative deviation of eCDF below the tCDF, respectively.

3 OBSERVATIONAL DATA AND SIMULATIONS

In this study, we analyse CMB maps cleaned using internal linear combination (ILC) method from 1, 3, 5, 7, and 9 yr WMAP data, and smica-cleaned CMB maps from 2015 and 2018 public data releases of Planck satellite mission. We also study cleaned CMB sky derived from Planck’s 2013 data, as explained later. WMAP data are available from Legacy Archive for Microwave Background Data Analysis (LAMBDA)1 and the Planck data are available from Planck Legacy Archive (PLA).2 Results are consistently reported in the order of their release. All results are evaluated over a consistent range |$2\le l \le 61$|⁠, unless otherwise specified.

All the WMAP’s ILC-cleaned CMB maps (WILC maps) are provided at a pixel resolution of healpix3|$N_{\rm side}$| = 512 whose beam window function is given by a Gaussian smoothing kernel of full width at half-maximum |$(\mathrm{ FWHM})= \!\! 1^\circ$| (degree). WILC maps are derived using a cleaning procedure in real (pixel) space by taking linear combinations of multifrequency raw satellite maps such that ‘cosmic’ microwave background signal remains untouched while (nearly) eliminating any foregrounds in the resulting cleaned CMB map (Bennett et al. 2003b; Eriksen et al. 2004). The Planck  smica-derived CMB maps also employ a similar approach, but the cleaning of raw satellite data maps from different frequency channels is performed in multipole space by taking linear combinations of their spherical harmonic coefficients (Delabrouille, Cardoso & Patanchon 2003; Cardoso et al. 2008). Planck provided much higher resolution CMB maps, owing to its better detector capabilities at  |$N_{\rm side}$| = 2048, with a Gaussian beam of |$\mathrm{ FWHM}=5 \ \mathrm{ arcmin}$|⁠. For the sake of this analysis, all the CMB maps – data and simulations – were generated or downgraded to have |$N_{\rm side}$| = 512 and smoothing level given by a Gaussian beam with |$\mathrm{ FWHM}=1^\circ$|⁠. More details on these are provided in Appendix A1.

Ideally, any cleaning procedure aims to remove the microwave foregrounds completely. However, in practice, there are still some (visible) foreground residuals present in the cleaned CMB maps thus obtained. Such residuals will lead to biased estimates for the quantities of our interest (e.g. statistics being computed) from the cleaned CMB maps. In order to minimize such effects due to galactic residuals, we use a single mask obtained by combining WMAP’s 9 yr Kp8 mask (available at |$N_{\rm side}$| = 512) and Planck’s 2018 common inpainting mask (provided at |$N_{\rm side}$| = 2048).Since each of these masks is available at different healpix resolutions, they are processed as detailed in Appendix  B to obtain a unified mask at healpix  |$N_{\rm side}$| = 512, with a non-zero sky fraction of |$f_{\rm sky}$|  |$\approx 0.929$|⁠. The mask thus obtained is shown in Fig. 1. Regions excised by this combination mask are inpainted using the isap4 package, which is a sparsity-based technique to fill those regions of the sky omitted due to masking in a statistically consistent manner with the rest of the available sky.

Unified mask obtained by merging WMAP’s 9 yr Kp8 mask and Planck’s 2018 common inpainting mask, both corresponding to CMB temperature data. This mask has a non-zero sky fraction of $f_{\rm sky}$  $\approx 0.929$.
Figure 1.

Unified mask obtained by merging WMAP’s 9 yr Kp8 mask and Planck’s 2018 common inpainting mask, both corresponding to CMB temperature data. This mask has a non-zero sky fraction of |$f_{\rm sky}$|  |$\approx 0.929$|⁠.

In order to generate simulations corresponding to WMAP’s cleaned CMB maps, viz. ILC-like CMB maps for various years, we use the weights as published by the WMAP team in the suite of papers accompanying each data release to combine simulated frequency-specific noisy CMB maps (Bennett et al. 2003b, 2013; Hinshaw et al. 2007; Gold et al. 2009, 2011). The generation and processing of frequency-specific CMB maps with appropriate beam and noise levels, to obtain mock ILC CMB maps for each of the WMAP’s data releases, are explained in Appendix A2.

Simulated CMB maps corresponding to Planck-employed smica cleaning procedure are provided by Planck collaboration as part of each data release from Planck Legacy Archive. They are referred to as Full Focal Plane (FFP) simulations. We use the FFP smica CMB simulations from 2015 and 2018 data releases as provided by Planck collaboration. In case of Planck 2013 data release (public release 1/PR1), corresponding simulations are currently not available as they are superseded by Full mission (2015/PR2) and Legacy data (2018/PR3) releases. Hence, we process the Planck 2013 data using ILC method in pixel space, hereafter, referred to as PR1 ILC. The downgrading procedure of Planck provided simulated smica CMB maps from 2015 and 2018 data releases, as well as deriving the PR1 ILC CMB map and corresponding simulations are described in Appendices A1 and A2. All these maps are then inpainted using isap in the same way as WILC maps, using the same mask shown in Fig. 1.

In generating appropriate mock maps to complement ILC-cleaned CMB maps from WMAP’s all data releases and Planck PR1 observations, we found that some care is required in handling the circular beam transfer functions (⁠|$b_l$|⁠) of low-frequency maps in both missions at high l as provided by respective collaborations. These additional details are presented in Appendices  C and  D.

4 RESULTS

4.1 Anisotropically distributed multipoles

The current cosmological model based on (statistical) isotropy predicts a null distribution of the eigenvalues of power tensor. To reiterate, the power entropy ‘|$S(l)$|’ (equation 5) is a rotationally invariant statistic for each mode ‘l’, which summarizes information on the distribution of eigenvalue sizes. We computed |$S(l)$| for all the data sets used in this study, and compared the results with the corresponding simulations.

Results are shown in Fig. 2. The solid grey line at the top of each figure indicates the maximum value |$S(l)$| can take, representing a completely isotropic case. The olive green line is the 95 per cent confidence level (CL) for the PE estimated from simulations for each multipole in the range of our interest |$l=[2,61]$|⁠.

Power entropy of each multipole, $S(l)$ (as per equation 5), of CMB maps from WMAP mission obtained using ILC method on 1, 3, 5, 7, and 9 yr data, as well as from Planck PR1 data cleaned using ILC method (Planck PR1 ILC), and smica-cleaned CMB maps from Planck’s 2015 and 2018 data releases. The olive green lines delineate $2\sigma$ confidence level (95 per cent) mode by mode derived from simulations.
Figure 2.

Power entropy of each multipole, |$S(l)$| (as per equation 5), of CMB maps from WMAP mission obtained using ILC method on 1, 3, 5, 7, and 9 yr data, as well as from Planck PR1 data cleaned using ILC method (Planck PR1 ILC), and smica-cleaned CMB maps from Planck’s 2015 and 2018 data releases. The olive green lines delineate |$2\sigma$| confidence level (95 per cent) mode by mode derived from simulations.

Since early suggestions of anisotropy were found in modes of rather small ‘l’, extending to a search over 60 total modes might create a penalty favouring the isotropic null. However, Fig. 2 shows that modes with anomalous PE are not confined to low l, but in some cases appear across the whole range. Open circles show anomalous cases with random chance occurrence probability of |$p\le 0.05$|⁠. Filled circles have |$p>0.05$|⁠. Table 1 summarizes the anomalous cases.

Table 1.

List of multipoles (second column) whose power entropy has a p-value of 5 per cent or less, as found in WILC CMB maps from 1, 3, 5, 7, and 9 yr WMAP data, and Planck 2013 data (PR1) cleaned using ILC method, and the smica CMB maps from Planck probe’s 2015 (PR2) and 2018 (PR3) data releases (mentioned in first column). The last column denotes the cumulative binomial probability to find the observed number of anomalous multipoles or more by random chance in the entire set over the multipole range |$l=[2,61]$|⁠.

Data setMultipoles, lCumulative binomial probability
WILC 1 yr13, 14, 16, 17, 30, 35, 480.030
WILC 3 yr13, 17, 30, 40, 560.180
WILC 5 yr13, 16, 17, 30, 35, 40, 560.030
WILC 7 yr13, 14, 16, 17, 30, 40, 560.030
WILC 9 yr13, 14, 16, 17, 30, 35, 400.030
PR1 ILC13, 14, 17, 30, 34, 560.079
PR2 smica13, 14, 16, 17, 30, 560.079
PR3 smica13, 14, 16, 17, 30, 40, 560.030
Data setMultipoles, lCumulative binomial probability
WILC 1 yr13, 14, 16, 17, 30, 35, 480.030
WILC 3 yr13, 17, 30, 40, 560.180
WILC 5 yr13, 16, 17, 30, 35, 40, 560.030
WILC 7 yr13, 14, 16, 17, 30, 40, 560.030
WILC 9 yr13, 14, 16, 17, 30, 35, 400.030
PR1 ILC13, 14, 17, 30, 34, 560.079
PR2 smica13, 14, 16, 17, 30, 560.079
PR3 smica13, 14, 16, 17, 30, 40, 560.030
Table 1.

List of multipoles (second column) whose power entropy has a p-value of 5 per cent or less, as found in WILC CMB maps from 1, 3, 5, 7, and 9 yr WMAP data, and Planck 2013 data (PR1) cleaned using ILC method, and the smica CMB maps from Planck probe’s 2015 (PR2) and 2018 (PR3) data releases (mentioned in first column). The last column denotes the cumulative binomial probability to find the observed number of anomalous multipoles or more by random chance in the entire set over the multipole range |$l=[2,61]$|⁠.

Data setMultipoles, lCumulative binomial probability
WILC 1 yr13, 14, 16, 17, 30, 35, 480.030
WILC 3 yr13, 17, 30, 40, 560.180
WILC 5 yr13, 16, 17, 30, 35, 40, 560.030
WILC 7 yr13, 14, 16, 17, 30, 40, 560.030
WILC 9 yr13, 14, 16, 17, 30, 35, 400.030
PR1 ILC13, 14, 17, 30, 34, 560.079
PR2 smica13, 14, 16, 17, 30, 560.079
PR3 smica13, 14, 16, 17, 30, 40, 560.030
Data setMultipoles, lCumulative binomial probability
WILC 1 yr13, 14, 16, 17, 30, 35, 480.030
WILC 3 yr13, 17, 30, 40, 560.180
WILC 5 yr13, 16, 17, 30, 35, 40, 560.030
WILC 7 yr13, 14, 16, 17, 30, 40, 560.030
WILC 9 yr13, 14, 16, 17, 30, 35, 400.030
PR1 ILC13, 14, 17, 30, 34, 560.079
PR2 smica13, 14, 16, 17, 30, 560.079
PR3 smica13, 14, 16, 17, 30, 40, 560.030

From Table 1, we see that the multipoles |$l=$| 13, 17, and 30 stand out consistently as anomalous in all of the five ILC maps from WMAP, as well as in Planck’s PR1 ILC map, and the smica-cleaned CMB maps from PR2 and PR3 data. More anomalous (more rare) entropies are smaller, corresponding to eigenvalues that are further from being equal.

The last column of Table 1 indicates the cumulative probability of finding the number of anomalous modes with|$p\le \mathbb {P}$| as observed in data, given the total number of modes analysed (i.e. |$l=2$|–61). For example, the cumulative binomial probability (equation 8) of observing 7 items with |$p \le 0.05$| in a random search of 60 cases is |${\approx} 0.030$|⁠. Enough cases are highly significant that the data do not support the isotropic null distribution. Many more multipoles would be deemed anomalous if the threshold p-value was chosen to be |$\mathbb {P}=0.1$|⁠. The large number of cases shown in Fig. 2 where the observed p-values are borderline, or just inside the cut-off curve, indicate that the arbitrary threshold of |$\mathbb {P} = 0.05$| creates a bias against detecting anisotropy.

4.2 A log-like statistic

To deal with a definite bias against rare events caused by choosing a threshold p-value ‘|$\mathbb {P}$|’, we investigated a likelihood-based statistic. Let |$f(x_l)$| be the known (simulated) distribution for the statistic ‘|$x_l$|’ for each multipole ‘l’. We then define a global statistic |$\Pi _x$| as

(10)

where |$F(x_l)$| is the (null) cumulative distribution corresponding to |$f(x_l)$|⁠. The value of this global statistic in data is then compared to the same global statistic from simulations. By making use of the null distribution of the statistic ‘|$x_l$|’, there are no arbitrary cut-offs and conclusions are not sensitive to that choice.

In Table 2, we summarize the results of |$\Pi _S$| for the PE statistic, i.e. |$x_l=S(l)$|⁠, along with the corresponding p-values for the multipole range |$l=2$|–61. One can readily see from p-value column of Table 2 that the multipoles in this range are collectively anomalous at about |$2\sigma$| level or better in almost all data sets. However, using the threshold |$\mathbb {P}=0.05$| might cause one to conclude that only few multipoles were anomalous from Table 1. Thus, we conclude that the multipoles, not just few but collectively, indicate an intrinsic anisotropy of the data sets.

Table 2.

Values of the log-likelihood statistic |$\Pi _S$|⁠, defined in equation (10) based on the null distribution of the power entropy, |$S(l)$|⁠, are listed in second column for various data sets listed in first column. The statistic values mentioned against different data releases were evaluated using the distribution obtained from a corresponding simulation ensemble of 1000 mocks. The p-values of |$\Pi _S$| thus obtained are given in the third column. The likelihood-based p-values are smaller than those of Table 1, which are evaluated with a cut-off of |$p \le 0.05$|⁠. This is evidence that using a hard cut-off on assessing multiple p-values tends to create a bias against detecting a signal.

Data set|$\Pi _S$|p-value
WILC 1 yr75.5100.033
WILC 3 yr72.7790.067
WILC 5 yr74.9400.042
WILC 7 yr78.6640.018
WILC 9 yr75.6030.028
PR1 ILC78.8240.013
PR2 smica74.7360.035
PR3 smica77.4830.019
Data set|$\Pi _S$|p-value
WILC 1 yr75.5100.033
WILC 3 yr72.7790.067
WILC 5 yr74.9400.042
WILC 7 yr78.6640.018
WILC 9 yr75.6030.028
PR1 ILC78.8240.013
PR2 smica74.7360.035
PR3 smica77.4830.019
Table 2.

Values of the log-likelihood statistic |$\Pi _S$|⁠, defined in equation (10) based on the null distribution of the power entropy, |$S(l)$|⁠, are listed in second column for various data sets listed in first column. The statistic values mentioned against different data releases were evaluated using the distribution obtained from a corresponding simulation ensemble of 1000 mocks. The p-values of |$\Pi _S$| thus obtained are given in the third column. The likelihood-based p-values are smaller than those of Table 1, which are evaluated with a cut-off of |$p \le 0.05$|⁠. This is evidence that using a hard cut-off on assessing multiple p-values tends to create a bias against detecting a signal.

Data set|$\Pi _S$|p-value
WILC 1 yr75.5100.033
WILC 3 yr72.7790.067
WILC 5 yr74.9400.042
WILC 7 yr78.6640.018
WILC 9 yr75.6030.028
PR1 ILC78.8240.013
PR2 smica74.7360.035
PR3 smica77.4830.019
Data set|$\Pi _S$|p-value
WILC 1 yr75.5100.033
WILC 3 yr72.7790.067
WILC 5 yr74.9400.042
WILC 7 yr78.6640.018
WILC 9 yr75.6030.028
PR1 ILC78.8240.013
PR2 smica74.7360.035
PR3 smica77.4830.019

For completeness, we report that in three cases (WMAP 1 yr, WMAP 7 yr, and Planck PR1) the 1000-run simulations found no cases of PE lower than the data for |$l=30$|⁠. An upper limit of |$p=10^{-3}$| was used to make an estimate of the |$\Pi _S$| statistic. A very long re-simulation of one of these cases (WILC7) convinced us that this order of magnitude is consistent.

4.3 p-value distributions

An issue in this type of data analysis is that not all statistics and not all data sets are independent. While some of that is controlled by the penalties of the cumulative binomial search over 60 multipoles, a considerable amount of information tends to be wasted. For each study of 60 cosmological multipoles across 8 data releases, we have 480 p-values, of which the vast majority do not pass a test based on significance of |$\mathbb {P}=5~{{\ \rm per\ cent}}$|⁠. Nevertheless, the distribution of these p-values has interesting information.

The problem of evaluating a large number of p-values for a given set of data was confronted in the classic paper by Schweder & Spjøtvoll (1982). In their words, ‘We consider a situation in which a large number of tests are made on the same data or are related to the same problem. A classical example is the one-way layout in the analysis of variance when all pairs of means are compared’. Italics are ours. The relevance of the method (and the quote) is that no assumptions are made about data elements being independent. The key observation is that the p-values of a true null distribution are uniformly distributed on the interval [0, 1]. If they are not uniformly distributed, it indicates that the null distribution does not fit the data. To illustrate this, Schweder & Spjøtvoll (1982) introduced a device called a p-value plot. The plot shows the number of cases ‘|$N(p_{*})$|’ with |$p{<}p_{*}$| as a function of ‘|$1-p_{*}$|’, which the null distribution predicts to follow a straight line (if the null is correct).

In Fig. 3, we show such a plot for the 480 p-values of PE for 60 multipoles from all the 8 data releases. The first 50 or so cases in the plot near |$1-p_{*} \sim 0$| (large p-values) are consistent with the null. The remaining points deviate greatly below the line, which means that there are too many small p-values to be consistent with the null. The Anderson–Darling (AD) test statistic for the data p-value distribution to come from the null distribution is |$10^{-6}$|⁠. Keeping in mind that the eight data sets are attempting to represent the same physical quantities, one might take that with a grain of salt. The result of eight similar but individual tests made on each data release using AD statistic returns a p-value of 0.05, 0.09, 0.08, 0.17, 0.09, 0.1, 0.05, and 0.02, in the order listed in the tables. Whether the different data sets are considered to be practically the same, or significantly independent, they repeatedly disfavour the null distribution.

The number of cases of $p{<}p_{*}$ denoted by ‘$N(p_{*})$’ as a function of ‘$1-p_{*}$’ for the power entropy are plotted as a blue curve. Data from the null distribution tend to be on the black straight line. The $1\sigma$ and $2\sigma$ confidence levels are shown in dashed salmon and dash–dotted green lines, respectively. As discussed in Schweder & Spjøtvoll (1982) and Section 4.3, the deviation of the data from the null around 50 of 480 cases (y-axis) indicates that the null model fits about 10 per cent of the data p-values.
Figure 3.

The number of cases of |$p{<}p_{*}$| denoted by ‘|$N(p_{*})$|’ as a function of ‘|$1-p_{*}$|’ for the power entropy are plotted as a blue curve. Data from the null distribution tend to be on the black straight line. The |$1\sigma$| and |$2\sigma$| confidence levels are shown in dashed salmon and dash–dotted green lines, respectively. As discussed in Schweder & Spjøtvoll (1982) and Section 4.3, the deviation of the data from the null around 50 of 480 cases (y-axis) indicates that the null model fits about 10 per cent of the data p-values.

4.4 Volume statistic

One of the interesting coincidences in the study of CMB low multipole alignments is the close proximity between CMB dipole, quadrupole, and octopole. While the CMB dipole is (predominantly) a consequence of our relative motion with respect to CMB rest frame, and therefore not cosmological, the alignment of |$l=2,3$| modes with |$l=1$| has gathered significant attention to understand their unexpected correlations (see, for example, Ralston & Jain 2004; Schwarz et al. 2004, 2016). Here, we use a simple statistic, the volume of the parallelepiped formed by their axes, to test their alignment with each other. When they are closely aligned, we have a collapsed parallelepiped with nearly zero volume and large otherwise.

The direction of the CMB dipole is taken to be |${\boldsymbol{ d}} = (\ell ,b)\approx (264^\circ ,48^\circ)$| for the CMB dipole5 in galactic coordinates. In Fig. 4, we exhibit the volume of the parallelepiped |$= \!\! {\boldsymbol{ d}} \cdot (\tilde{\boldsymbol{ e}}_2 \times \tilde{\boldsymbol{ e}}_3)$| formed by CMB dipole (⁠|$l=1$|⁠), and the |$l=2,3$| PEVs. It is evident from the figure that these modes are well aligned at about |$2\sigma$| level or better depending on specific data release. See, for example, de Oliveira-Costa & Tegmark (2006), Bielewicz et al. (2005), and Aluri et al. (2011) that probed the stability of these large angular modes against foregrounds and varying galactic sky cuts (masks).

p-values corresponding to the alignment of CMB dipole, quadrupole, and octopole as quantified by the volume formed by respective axes ${\boldsymbol{ d}}$, $\tilde{\boldsymbol{ e}}_2$, and $\tilde{\boldsymbol{ e}}_3$ are shown as blue circles joined by a line using $y1$-axis and the value of the statistic, viz. the volume of the parallelepiped formed by these axes $= \!\! {\boldsymbol{ d}} \cdot (\tilde{\boldsymbol{ e}}_2 \times \tilde{\boldsymbol{ e}}_3)$ is shown using the $y2$-axis with red diamond point type joined by a line for all the data releases that we studied. The significance of their alignment is evidently about $2\sigma$ level or better.
Figure 4.

p-values corresponding to the alignment of CMB dipole, quadrupole, and octopole as quantified by the volume formed by respective axes |${\boldsymbol{ d}}$|⁠, |$\tilde{\boldsymbol{ e}}_2$|⁠, and |$\tilde{\boldsymbol{ e}}_3$| are shown as blue circles joined by a line using |$y1$|-axis and the value of the statistic, viz. the volume of the parallelepiped formed by these axes |$= \!\! {\boldsymbol{ d}} \cdot (\tilde{\boldsymbol{ e}}_2 \times \tilde{\boldsymbol{ e}}_3)$| is shown using the |$y2$|-axis with red diamond point type joined by a line for all the data releases that we studied. The significance of their alignment is evidently about |$2\sigma$| level or better.

4.5 Multipoles aligned with |$l=2$|

Alignment with high significance between the modes |$l=$| 2 and 3 was initially observed in CMB maps derived from WMAP 1 yr data. Similar alignments were later found among higher multipoles also (Tegmark, de Oliveira-Costa & Hamilton 2003; Copi et al. 2004; de Oliveira-Costa et al. 2004; Eriksen et al. 2004; Schwarz et al. 2004; Samal et al. 2008). Interestingly, |$l \geq 2$| modes were also aligned with the CMB dipole and other preferred axes found in various astronomical data (Ralston & Jain 2004). Here, we extend the study of alignments with |$l=2$| to the entire range of our study. The test statistic is ‘|$x:=1-\tilde{\boldsymbol{ e}}_l\cdot \tilde{\boldsymbol{ e}}_{2} = 1-\cos \alpha _{l2}$|’, where |$\tilde{\boldsymbol{ e}}_l$| and |$\tilde{\boldsymbol{ e}}_{2}$| are the PEVs of multipoles ‘l’ and ‘2’.

The results are presented in Fig. 5. A |$2\sigma$| anomaly |$(p\le 0.05)$| is denoted by an olive green line in each subplot. The octopole mode is anomalously aligned with the quadrupole mode in all CMB maps analysed in this study. Multipoles that are spuriously aligned with the quadrupole are listed in column 2 of Table 3. Third column of Table 3 denotes the cumulative null probability of finding the observed number of multipoles or more in the data set. The last column of Table 3 reports the p-value of the Kuiper statistic (equation 9) of the alignment measure ‘x’ for the entire set compared to a uniform distribution. Readers can assess the meaning of these results for themselves. The very high significance of early studies discovering the alignments of |$l=$| 1, 2, 3 has not changed. When the same data are immersed in a search over 60 multipoles, with |$l=1$| excluded, |$l=2$| given, and |$l=3$| contributing, the estimated significance is greatly reduced.

p-values corresponding to the alignment of quadrupole with higher order multipoles, i.e. alignment between the said PEVs in each CMB map from various data releases.
Figure 5.

p-values corresponding to the alignment of quadrupole with higher order multipoles, i.e. alignment between the said PEVs in each CMB map from various data releases.

Table 3.

List of multipoles that are aligned with the quadrupole with a p-value |$\le \!\! 5{{\ \rm per\, cent}}$| as found for the eight data releases. The third column denotes the cumulative binomial probability of finding the observed number of anomalous modes or more with |$p\le 0.05$|⁠. The fourth column gives the probability of the observed Kuiper statistic (V) for the set. The dipole (⁠|$l=1$|⁠) has been excluded by convention. Including it makes little difference to significance dominated by making 60 searches.

Data setMultipoles, lCumulative probabilityp-value of V
WILC 1 yr3, 16, 420.5710.192
WILC 3 yr3, 16, 400.5710.915
WILC 5 yr3, 160.8010.796
WILC 7 yr3, 16, 21, 440.3410.412
WILC 9 yr3, 16, 210.5710.659
PR1 ILC3, 16, 40, 440.3410.116
PR2 smica3, 21, 440.5710.531
PR3 smica3, 42, 440.5710.673
Data setMultipoles, lCumulative probabilityp-value of V
WILC 1 yr3, 16, 420.5710.192
WILC 3 yr3, 16, 400.5710.915
WILC 5 yr3, 160.8010.796
WILC 7 yr3, 16, 21, 440.3410.412
WILC 9 yr3, 16, 210.5710.659
PR1 ILC3, 16, 40, 440.3410.116
PR2 smica3, 21, 440.5710.531
PR3 smica3, 42, 440.5710.673
Table 3.

List of multipoles that are aligned with the quadrupole with a p-value |$\le \!\! 5{{\ \rm per\, cent}}$| as found for the eight data releases. The third column denotes the cumulative binomial probability of finding the observed number of anomalous modes or more with |$p\le 0.05$|⁠. The fourth column gives the probability of the observed Kuiper statistic (V) for the set. The dipole (⁠|$l=1$|⁠) has been excluded by convention. Including it makes little difference to significance dominated by making 60 searches.

Data setMultipoles, lCumulative probabilityp-value of V
WILC 1 yr3, 16, 420.5710.192
WILC 3 yr3, 16, 400.5710.915
WILC 5 yr3, 160.8010.796
WILC 7 yr3, 16, 21, 440.3410.412
WILC 9 yr3, 16, 210.5710.659
PR1 ILC3, 16, 40, 440.3410.116
PR2 smica3, 21, 440.5710.531
PR3 smica3, 42, 440.5710.673
Data setMultipoles, lCumulative probabilityp-value of V
WILC 1 yr3, 16, 420.5710.192
WILC 3 yr3, 16, 400.5710.915
WILC 5 yr3, 160.8010.796
WILC 7 yr3, 16, 21, 440.3410.412
WILC 9 yr3, 16, 210.5710.659
PR1 ILC3, 16, 40, 440.3410.116
PR2 smica3, 21, 440.5710.531
PR3 smica3, 42, 440.5710.673

Before leaving this section, we report that neglecting the effects of small p-values does not seem to be the cause of these results. Repeating the whole analysis with likelihood statistics developed from the simulations (as in Section 4.2) did not find significantly different outcomes.

4.6 Pairwise alignments among multipoles

Extensive random searches can dilute statistical significance. That was certainly not a problem in the early history, which was confined to alignments of low multipoles l = 1, 2, 3. For thoroughness of this study, we nevertheless decided to explore all pairwise combinations of PEVs from all data releases with the statistic ‘|$x:=1-\tilde{\boldsymbol{ e}}_l\cdot \tilde{\boldsymbol{ e}}_{l^{\prime }}$|’. For the multipole range studied, i.e. |$l=[2,61]$|⁠, there are |$n=60 \times 59/2=1770$| possible combinations to consider for each release. This creates a correspondingly large penalty from the cumulative binomial distribution for whatever anomalies might be found. The results are summarized in Table 4. Nothing of significance is indicated by this search.

Table 4.

Alignment statistic ‘|$x:=1-\cos \alpha$|’ for all pairwise combinations (⁠|$60\times 59/2=1770$| in total) for each release. Column 2 lists the number of anomalous alignments (⁠|$k_*$|⁠) found with |$p\le 0.05$|⁠. Column 3 lists the cumulative binomial probabilities to have found |$k_*$| modes that are spuriously aligned per |$\mathbb {P}=0.05$|⁠. Column 4 lists the cumulative Kuiper statistic (V) for the search.

Data set|$k_*$| (out of 1770)Cumulative probabilityp-value of V
WILC 1 yr820.7750.307
WILC 3 yr920.3660.562
WILC 5 yr810.8080.850
WILC 7 yr930.3270.417
WILC 9 yr810.8080.548
PR1 ILC880.5370.622
PR2 smica890.4940.920
PR3 smica910.4080.794
Data set|$k_*$| (out of 1770)Cumulative probabilityp-value of V
WILC 1 yr820.7750.307
WILC 3 yr920.3660.562
WILC 5 yr810.8080.850
WILC 7 yr930.3270.417
WILC 9 yr810.8080.548
PR1 ILC880.5370.622
PR2 smica890.4940.920
PR3 smica910.4080.794
Table 4.

Alignment statistic ‘|$x:=1-\cos \alpha$|’ for all pairwise combinations (⁠|$60\times 59/2=1770$| in total) for each release. Column 2 lists the number of anomalous alignments (⁠|$k_*$|⁠) found with |$p\le 0.05$|⁠. Column 3 lists the cumulative binomial probabilities to have found |$k_*$| modes that are spuriously aligned per |$\mathbb {P}=0.05$|⁠. Column 4 lists the cumulative Kuiper statistic (V) for the search.

Data set|$k_*$| (out of 1770)Cumulative probabilityp-value of V
WILC 1 yr820.7750.307
WILC 3 yr920.3660.562
WILC 5 yr810.8080.850
WILC 7 yr930.3270.417
WILC 9 yr810.8080.548
PR1 ILC880.5370.622
PR2 smica890.4940.920
PR3 smica910.4080.794
Data set|$k_*$| (out of 1770)Cumulative probabilityp-value of V
WILC 1 yr820.7750.307
WILC 3 yr920.3660.562
WILC 5 yr810.8080.850
WILC 7 yr930.3270.417
WILC 9 yr810.8080.548
PR1 ILC880.5370.622
PR2 smica890.4940.920
PR3 smica910.4080.794

4.7 Common set of anomalous multipoles shared by all releases

Table 5 lists multipoles that were anomalous at the 95 per cent level in every one of the eight data releases when employing a particular statistic. For example, the PE of l = 13, 17, 30 was never observed in any simulation to have a p-value exceeding 0.05. (This understates the information: The p-values for |$l=13$| were 0.016, 0.024, 0.018, 0.016, 0.038, 0.009, 0.014, and 0.014. The |$l=17$| case is also less likely by chance. For |$l =30$|⁠, the set was 0.0, 0.017, 0.001, 0.0, 0.004, 0.0, 0.001, and 0.001. These p-values are in the same order of data releases as mentioned in tables.)

Table 5.

Common set of anomalous multipoles across data sets corresponding to each statistic listed in column 1 are consolidated here, whose p-values for a particular statistic were found to be |$p\le 0.05$|⁠.

StatisticMultipole(s), l
Power entropy13, 17, 30
Aligned with quadrupole3
Aligned modes(2, 3), (3, 16), (6, 17), (7, 19), (7, 56),
 (8, 10), (10, 18), (11, 35), (13, 15),
 (16, 40), (21, 61), (22, 34), (23, 25),
 (29, 30), (34, 39)
StatisticMultipole(s), l
Power entropy13, 17, 30
Aligned with quadrupole3
Aligned modes(2, 3), (3, 16), (6, 17), (7, 19), (7, 56),
 (8, 10), (10, 18), (11, 35), (13, 15),
 (16, 40), (21, 61), (22, 34), (23, 25),
 (29, 30), (34, 39)
Table 5.

Common set of anomalous multipoles across data sets corresponding to each statistic listed in column 1 are consolidated here, whose p-values for a particular statistic were found to be |$p\le 0.05$|⁠.

StatisticMultipole(s), l
Power entropy13, 17, 30
Aligned with quadrupole3
Aligned modes(2, 3), (3, 16), (6, 17), (7, 19), (7, 56),
 (8, 10), (10, 18), (11, 35), (13, 15),
 (16, 40), (21, 61), (22, 34), (23, 25),
 (29, 30), (34, 39)
StatisticMultipole(s), l
Power entropy13, 17, 30
Aligned with quadrupole3
Aligned modes(2, 3), (3, 16), (6, 17), (7, 19), (7, 56),
 (8, 10), (10, 18), (11, 35), (13, 15),
 (16, 40), (21, 61), (22, 34), (23, 25),
 (29, 30), (34, 39)

In brief, we note that the number of multipoles with anomalous PE values is about |$2\sigma$| in almost all data releases that we studied. Expected number of alignments that would be outside |$2\sigma$| CL are |${\sim} 3$| when considering alignment between quadrupole and higher order modes that are 59 in number, and |${\sim} 88$| from among all possible pairwise alignments that are 1770 in number, for the multipole range |$l=[2,61]$|⁠. We find nearly the same number of multipoles to be aligned with a random chance occurrence probability of |$p\le 0.05$| in both the cases. So, the observed number of alignments are consistent with the expectations, which were further confirmed using a cumulative probability distribution function statistic (Kuiper test).

We also note in passing that though we did not find any collective alignments between |$l=2$| and rest of the multipoles or in pairwise alignment tests, a different kind of analysis using the same statistics employed here revealed an interesting pattern. Testing alignments among only even or odd multipoles separately, it was found that the odd multipoles from the same multipole range studied here (⁠|$l=[2,61]$|⁠) have an anomalous alignment entropy (equation 7) at |$\gtrsim \!\! 2\sigma$| level indicating less dispersion in the relative orientation of PT-PEVs (Aluri, Ralston & Weltman 2017).

4.8 Collective alignments of multipoles

The log-like statistic employed in Section 4.2 revealed that, collectively, the first 60 cosmological modes, viz. |$l=[2,61]$|⁠, are intrinsically anisotropic at greater than 95 per cent confidence level across data releases. Then, it is only natural to query whether there is any coherent alignment among these modes. Here, we test for the presence of any collective alignments among the first 60 multipoles in CMB maps from the 8 data releases. The test statistics are defined based on the alignment tensor (as per equation 6).

Reviewing this briefly, AT is an entirely directional statistic, which is independent of the eigenvalues of PT. AT is formed from the sum of the outer products of the PEVs over the multipoles |$l=2\ldots 61$| from each data release. The eigenvector corresponding to the largest eigenvalue of AT (the AT-PEV) probes any collective preferred alignment axis for the set of multipoles being studied. AT is isotropic (diagonal with equal entries) in the null model, i.e. the standard cosmological model based on cosmological principle.

AT has its own eigenvalues, which determine alignment entropy by equation (7). In an isotropic sky, AE is maximal. In that case, no correlation of PT-PEVs would be observed. Indeed, no correlations are observed by far, as is evident from the top panel of Fig. 6. AE from data are comparable to random chance, as indicated by these p-values. The directions of AT-PEVs are shown in the bottom panel of the same figure essentially pointing in the same direction with some scatter from all eight data releases. Here, we note that the entropies indicate that the ensembles of PEVs making the AT tend to be isotropic in a statistical sense. However, the AT-PEV is determined by whatever breaks the rotational symmetry of the ensemble. A few well-aligned PEVs can have minimal effects on the entropy of a set of 60 multipoles, while completely determining the AT-PEV.

Top: p-values of alignment entropy (listed in the order of the tables) are not unusually small. Bottom: Collective alignment axes, i.e. $\tilde{\boldsymbol{ f}}$ (AT-PEV) from the alignment tensors (equation 6) of multipoles $l=[2,61]$ for the eight data releases.
Figure 6.

Top: p-values of alignment entropy (listed in the order of the tables) are not unusually small. Bottom: Collective alignment axes, i.e. |$\tilde{\boldsymbol{ f}}$| (AT-PEV) from the alignment tensors (equation 6) of multipoles |$l=[2,61]$| for the eight data releases.

4.9 Correlations with CMB dipole, Galactic plane, and ecliptic plane

Finally, we test for alignment of multipoles with some known directions/planes in the sky. Specifically, we test whether the multipole PEVs are spuriously aligned with the CMB dipole direction (⁠|$l=1$| mode), the Galactic plane, and the ecliptic plane. We remind that PEVs represent axes and not directed vectors. We use the alignment measure |$x:=1-\hat{\lambda }\cdot \tilde{\boldsymbol{ e}}_l=1-\cos \alpha _l$|⁠, where |$\alpha _l=[0^\circ ,90^\circ ]$|⁠, |$\hat{\lambda }$| is one of the three known directions/planes in the sky mentioned above, and |$\tilde{\boldsymbol{ e}}_l$| is the PEV of a multipole ‘l’. We take the three directions (⁠|$\hat{\lambda }$|⁠) to be |${\boldsymbol{ d}} = (\ell ,b)\approx (264^\circ ,48^\circ)$| for the CMB dipole as noted earlier, |$(\ell ,b)=(0^\circ ,90^\circ)$| for the Galactic (north) pole, and |$(\ell ,b)\approx (276.4^\circ , -29.8^\circ)$| for ecliptic (south) pole in galactic coordinates.6 We check for the instances when |$\lbrace x_{\rm sim}\rbrace$| are smaller than ‘|$x_{\rm obs}$|’ to test for alignment with CMB kinematic dipole, and when |$\lbrace x_{\rm sim}\rbrace$| are larger than ‘|$x_{\rm obs}$|’ to probe for multipole PEVs lying in Galactic/ecliptic plane. The threshold for significance is |$p \le 0.05$|⁠.

The results are presented in Table 6. Given that 60 multipoles have been searched, it is not surprising that little of significance is observed. Nevertheless, it is interesting that the multipoles |$l=$|21, 42, 44, and 61 were found to be consistently well aligned with the CMB dipole direction with |$p\le 5~{{\ \rm per\ cent}}$| in almost all CMB maps.

Table 6.

List of anomalous multipoles whose alignment measures have a probability of |$p\le 0.05$|⁠, cumulative binomial probability of having found the observed number of anomalous modes (using |$\mathbb {P}=0.05$|⁠), and test of random distribution of PEVs using Kuper's ‘V’ statistic with respect to CMB dipole (columns 2–4), Galactic plane (columns 5–7), and ecliptic plane (columns 8–10) when compared with simulations. Alignment statistic ‘x’ and Kuiper statistic ‘V’ are defined in the text.

 CMB dipole (⁠|$\parallel$|⁠)Galactic plane (⁠|$\perp$|⁠)Ecliptic plane (⁠|$\perp$|⁠)
Data setMultipoles, lCumulativep-valueMultipoles, lCumulativep-valueMultipoles, lCumulativep-value
  probabilityof V probabilityof V probabilityof V
WILC 1 yr2, 21, 41, 42, 610.1800.77147, 510.8080.67027, 29, 52, 540.3530.870
WILC 3 yr21, 42, 44, 610.3530.601510.9540.2548, 31, 470.5830.627
WILC 5 yr21, 42, 44, 610.3530.371550.9540.2328, 26, 31, 470.3530.927
WILC 7 yr21, 36, 42, 44, 610.1800.733510.9540.5868, 100.8080.752
WILC 9 yr21, 42, 44, 610.3530.768570.9540.7978, 31, 47, 490.3530.639
PR1 ILC3, 21, 42, 44, 610.1800.92110.80418, 470.8080.863
PR2 smica2, 21, 36, 42, 44, 610.0790.595550.9540.5702, 8, 470.5830.915
PR3 smica2, 21, 42, 44, 610.1800.909350.9540.5702, 8, 10, 470.3530.830
 CMB dipole (⁠|$\parallel$|⁠)Galactic plane (⁠|$\perp$|⁠)Ecliptic plane (⁠|$\perp$|⁠)
Data setMultipoles, lCumulativep-valueMultipoles, lCumulativep-valueMultipoles, lCumulativep-value
  probabilityof V probabilityof V probabilityof V
WILC 1 yr2, 21, 41, 42, 610.1800.77147, 510.8080.67027, 29, 52, 540.3530.870
WILC 3 yr21, 42, 44, 610.3530.601510.9540.2548, 31, 470.5830.627
WILC 5 yr21, 42, 44, 610.3530.371550.9540.2328, 26, 31, 470.3530.927
WILC 7 yr21, 36, 42, 44, 610.1800.733510.9540.5868, 100.8080.752
WILC 9 yr21, 42, 44, 610.3530.768570.9540.7978, 31, 47, 490.3530.639
PR1 ILC3, 21, 42, 44, 610.1800.92110.80418, 470.8080.863
PR2 smica2, 21, 36, 42, 44, 610.0790.595550.9540.5702, 8, 470.5830.915
PR3 smica2, 21, 42, 44, 610.1800.909350.9540.5702, 8, 10, 470.3530.830
Table 6.

List of anomalous multipoles whose alignment measures have a probability of |$p\le 0.05$|⁠, cumulative binomial probability of having found the observed number of anomalous modes (using |$\mathbb {P}=0.05$|⁠), and test of random distribution of PEVs using Kuper's ‘V’ statistic with respect to CMB dipole (columns 2–4), Galactic plane (columns 5–7), and ecliptic plane (columns 8–10) when compared with simulations. Alignment statistic ‘x’ and Kuiper statistic ‘V’ are defined in the text.

 CMB dipole (⁠|$\parallel$|⁠)Galactic plane (⁠|$\perp$|⁠)Ecliptic plane (⁠|$\perp$|⁠)
Data setMultipoles, lCumulativep-valueMultipoles, lCumulativep-valueMultipoles, lCumulativep-value
  probabilityof V probabilityof V probabilityof V
WILC 1 yr2, 21, 41, 42, 610.1800.77147, 510.8080.67027, 29, 52, 540.3530.870
WILC 3 yr21, 42, 44, 610.3530.601510.9540.2548, 31, 470.5830.627
WILC 5 yr21, 42, 44, 610.3530.371550.9540.2328, 26, 31, 470.3530.927
WILC 7 yr21, 36, 42, 44, 610.1800.733510.9540.5868, 100.8080.752
WILC 9 yr21, 42, 44, 610.3530.768570.9540.7978, 31, 47, 490.3530.639
PR1 ILC3, 21, 42, 44, 610.1800.92110.80418, 470.8080.863
PR2 smica2, 21, 36, 42, 44, 610.0790.595550.9540.5702, 8, 470.5830.915
PR3 smica2, 21, 42, 44, 610.1800.909350.9540.5702, 8, 10, 470.3530.830
 CMB dipole (⁠|$\parallel$|⁠)Galactic plane (⁠|$\perp$|⁠)Ecliptic plane (⁠|$\perp$|⁠)
Data setMultipoles, lCumulativep-valueMultipoles, lCumulativep-valueMultipoles, lCumulativep-value
  probabilityof V probabilityof V probabilityof V
WILC 1 yr2, 21, 41, 42, 610.1800.77147, 510.8080.67027, 29, 52, 540.3530.870
WILC 3 yr21, 42, 44, 610.3530.601510.9540.2548, 31, 470.5830.627
WILC 5 yr21, 42, 44, 610.3530.371550.9540.2328, 26, 31, 470.3530.927
WILC 7 yr21, 36, 42, 44, 610.1800.733510.9540.5868, 100.8080.752
WILC 9 yr21, 42, 44, 610.3530.768570.9540.7978, 31, 47, 490.3530.639
PR1 ILC3, 21, 42, 44, 610.1800.92110.80418, 470.8080.863
PR2 smica2, 21, 36, 42, 44, 610.0790.595550.9540.5702, 8, 470.5830.915
PR3 smica2, 21, 42, 44, 610.1800.909350.9540.5702, 8, 10, 470.3530.830

5 SUMMARY AND CONCLUSIONS

We analysed all full-sky CMB maps that are publicly available from NASA’s WMAP’s 1, 3, 5, 7, and 9 yr observational data, as well as CMB maps from ESA’s Planck’s 2013, 2015, and 2018 public releases. The eight data releases consist of the ILC method cleaned CMB maps from WMAP’s successive data releases and Planck’s nominal (PR1) data, and the smica-cleaned CMB maps from Planck’s full (PR2) and legacy (PR3) data releases. Our test statistics viz. the power tensor (PT) and alignment tensor (AT) are rotationally covariant and invariant measures of individual multipoles and collections of multipoles. A statistic is ‘anomalous’ if its p-value relative to extensive release-by-release simulations is less than 0.05. The effects of conducting multiple searches are controlled by evaluating statistics with a cumulative binomial null distribution and the distribution of log-likelihood statistics.

5.1 Review of our results

  • The power entropy (PE) of multipoles is consistently anomalous across all releases. Fig. 2 shows p-values for each ‘l’ over all data releases that we studied. The olive green curve in the figure indicates |$p\le 0.05$|⁠. Tables 1 and 2 suggest probabilities of the null model to yield the statistics by chance that are of the order of a few per cent.

    In the course of this study, we discovered a bias that underestimates discrepancies from the null, yet which is very common. The bias consists of basing analysis on an arbitrary p-value threshold for significance, then generating many trials, and finally not taking into account p-values found to be smaller than the threshold. This is a feature of the pass/no pass binomial statistic, which has no information about how far below the |$2\sigma$| CL curve the points of Fig. 2 might be. The first version of the paper was restricted to using strict threshold and fell victim to that bias. Table 2 was generated using the log-likelihood of the entire set of statistics in the simulated null distribution. This method has no dependence on a p-value threshold, and showed that the probabilities of the null to pass the test had been overestimated by the 5 per cent cut-off. (This is not a trivial result: The number of large p-values affects the likelihood statistic just as well as the small ones.) Fig. 3 tells the same story graphically. The cumulative distribution of p-values of statistics coming from a distribution that fits the data is a straight line. The distribution of p-values compared to an inappropriate distribution deviates from a straight line, with the deviation of Fig. 3 showing that there are too many small p-values for the isotropic null distribution to fit the data.

  • Fig. 5 and Table 3 present test results for alignments of higher multipoles with the quadrupole, |$l=2$|⁠. The highly significant alignments observed in the CMB map from WMAP's first data release are seen in all releases. However, extending the search over the full range |$2\le l \le 61$| does not find enough more alignments to indicate a test violating the null hypothesis with high significance. Not unexpectedly, extending the search to all possible pairwise combinations involves so many combinations that nothing of significance is observed, as seen in Table 4.

  • We also tested for correlation among PT-PEVs with the CMB dipole (⁠|$l=1$|⁠) direction, the Galactic plane, and the ecliptic plane. While anomalous alignments are found (Table 6), they are distributed across 60 multipoles of the study, which overall suggest no extraordinary correlations.

  • Collective alignments are measured by AT, which is constructed entirely from eigenvectors of PT. There is no importance weighting by eigenvalues in AT. The entropies of AT across releases are unremarkable. The bottom panel of Fig. 6 shows AT-PEVs broadly pointing in the same direction with little scatter.

  • Fig. 7 shows the PEVs of |$l=2,\, 3$|⁠, the dipole direction, plus the directions of multipoles with anomalously low PE, viz. |$l=$| 13, 17, and 30. It is very remarkable that the PE p-values of this set are very anomalous across all releases (Table 5). We remind that PE is a measure of the invariants of PT and is completely independent of its eigenvectors. The power entropies of multipoles have no statistical relation to their directions in the isotropic model. PE does not at all suggest the clustering of |$l=1,2,3$| axes seen in the upper left panel of Fig. 7. This was quantified in Section 4.4 using a volume statistic and found that the CMB dipole, quadrupole, and octopole modes are well aligned at a significance of |$2\sigma$| level or better in all releases.

  • Some important comments regarding the methodology and procedures adopted in producing WMAP's ILC-cleaned (WILC) CMB maps and Planck’s smica-cleaned CMB maps are in order. First, the harmonic space methods are generally more efficient at cleaning raw maps, as they clean foregrounds not only by the level of their spatial distribution (Fig. A1), but also by angular size, i.e. ‘l’ (equations A5 and A7). Secondly, a foreground bias correction map is subtracted from WILC maps based on simulations that includes cleaning simulated raw satellite maps with CMB, foregrounds, and appropriate instrument beam and noise effects. This bias correction was shown to improve the alignment between quadrupole and octopole (Aluri et al. 2011), which is not applied to any of Planck’s component separated maps including smica CMB map. Further, substantial care is taken to handle systematics in Planck-produced CMB maps (see, for example, Das & Souradeep 2015; Planck Collaboration LVII 2020). Finally, we also note that correcting for (frequency-dependent) kinematic quadrupole was shown to improve the alignment between |$l=2,3$| modes (Notari & Quartin 2015). This correction is, however, not applied to any of the CMB maps studied here.

Top: The anisotropy axis of consistently aligned modes $l=2$, 3 along with CMB dipole ($l=1$) and the PEVs of multipoles $l=13$, 17, and 30 having consistently anomalous PE across all releases. Middle and bottom: Multipole patterns of $l=13$, 17, and 30 with anomalous PE in galactic coordinates from Planck’s 2018 smica CMB map whose random chance occurrence probability is $p\le 5~{{\ \rm per\ cent}}$.
Figure 7.

Top: The anisotropy axis of consistently aligned modes |$l=2$|⁠, 3 along with CMB dipole (⁠|$l=1$|⁠) and the PEVs of multipoles |$l=13$|⁠, 17, and 30 having consistently anomalous PE across all releases. Middle and bottom: Multipole patterns of |$l=13$|⁠, 17, and 30 with anomalous PE in galactic coordinates from Planck’s 2018 smica CMB map whose random chance occurrence probability is |$p\le 5~{{\ \rm per\ cent}}$|⁠.

5.2 Conclusions

Appendix reports on extensive painstaking simulations, which are heart of our analysis. Here are some observations from our results.

The unexpected alignment seen in WMAP’s first year data release between two of the largest scale multipoles, namely the quadrupole (⁠|$l=2$|⁠) and octopole (⁠|$l=3$|⁠), continues to be observed across all releases. This along with the dipole (⁠|$l=1$|⁠) alignment hints at a preferred direction for our Universe on large scales in the direction of the Virgo cluster. For a long time, the dipole component was assumed to be a kinematic effect of no cosmological significance. It was nearly forgotten that the isotropic cosmological model allows a non-zero dipole fluctuation to exist, which would add linearly to a kinematic component. It is curious that in the null model it would not matter either way whether the dipole is included among the statistics, or omitted. A habit of omitting in ‘by convention’ cannot be called objective. The interpretation of the CMB dipole has also become controversial recently in studies of galaxy distributions (see, for example, Singal 2011; Rubart & Schwarz 2013; Tiwari & Jain 2015; Secrest et al. 2022). In summary, the status of the dipole has not been settled, but the anomalous alignment of low-l multipoles cannot be doubted. It is unsurprising that extending the range over 60 multipoles does not turn up much of significance, while we are obliged to report it once we had done it.

Next, we have found strange outcomes we cannot explain. There are three modes |$l=13, 17$|⁠, and 30 whose PE is intrinsically anisotropic across all data sets, yet were not reported to be anomalous in earlier studies. The multipole pattern of |$l=13$| mode as shown in Fig. 7 reveals that most of its hotspots and cold spots lie along the ecliptic plane. That may suggest a non-cosmological nature. The multipole patterns of |$l=17$| and 30 modes, shown in the same figure, are not self-explanatory, though one might see in them some correlation with our Galactic north polar spur (seen more readily in low-frequency microwave/radio observations). We have no explanation for the rotationally invariant entropy to select multipoles whose totally independent directional orientations align as seen.

Finally, there are far too many multipoles with anomalously small PE to be consistent with the null model. The CMB power spectrum has averaged over information in order to make rotationally invariant statistics. Yet the power spectrum is not the only rotationally invariant quantity available. In everyday terms, the PE is the measure of the ‘shape’ of a multipole, visualized as a temperature distribution on a sphere. The most common, most likely PE in the isotropic model, is a shape that is as spherical as possible. A multipole of order ‘l’ has |$2l+1$| real components, which range from 3 components (the dipole) to 123 components (⁠|$l=61$|⁠). A typical multipole from the isotropic cosmological model has no discernible shape or orientation, but is more like a riot of random patches. The anomalous number of low-PE shapes observed in the data is more like the orderly patterns seen for single spherical harmonics. PE is a genuine information entropy, as defined by von Neumann and Shannon, and then a genuine probe into the phases of the CMB radiation. The conclusion of our study is that the observed CMB is not as random as the cosmological principle predicts. It would be interesting if these phenomena could be confronted by alternative cosmological models, and more importantly are seen in CMB polarization observations with comparable signal-to-noise ratio in the future.

ACKNOWLEDGEMENTS

Some of the results in this work were derived using the publicly available healpix/healpy package (Górski et al. 2005; Zonca et al. 2020). This work made use of camb7 (Lewis, Challinor & Lasenby 2000; Howlett et al. 2012), a freely available Boltzmann solver for CMB anisotropies. We acknowledge the use of NASA’s WMAP data from the LAMBDA, part of the High Energy Astrophysics Science Archive Center (HEASARC). HEASARC/LAMBDA is a service of the Astrophysics Science Division at the NASA Goddard Space Flight Center. Part of the results presented here are based on observations obtained with Planck, an ESA science mission with instruments and contributions directly funded by ESA Member States, NASA, and Canada. We also acknowledge the use of isap software (Starck, Fadili & Rassat 2013). This research used resources of the National Energy Research Scientific Computing Center (NERSC), a U.S. Department of Energy Office of Science User Facility operated under Contract No. DE-AC02-05CH11231. Further, this work also made use of scipy8 (Virtanen et al. 2020), numpy9 (Harris et al. 2020), astropy10 (Astropy Collaboration 2013, 2018, 2022), and matplotlib11 (Hunter 2007).

DATA AVAILABILITY

This work made use of the publicly available CMB data from WMAP and Planck missions, and other details provided in the accompanying supplementary notes. As such, no new data are generated as part of this work.

Footnotes

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record ascl:2008.022

APPENDIX A: DATA AND SIMULATIONS

A1 Data

WMAP is a space-based NASA mission, which made observations of the microwave sky in five frequency channels, 23, 33, 41, 61, and 94 GHz. These five frequency channels are also referred to as |$K,Ka,Q,V,$| and W bands, respectively. Cleaned CMB maps from these five raw satellite data were obtained using the ILC method where suitable weights were used to remove foregrounds. The observed signal in a frequency channel, |$\nu _i$| (or simply i), is supposed to be a linear combination given by

(A1)

where |$\Delta T_c(\hat{n})$| is CMB, the cosmic signal, that is independent of frequency (in thermodynamic units), |$F_i(\hat{n})$| represents sum of all foregrounds (galactic/extragalactic astrophysical emission) at frequency ‘i’ that are frequency dependent, and |$N_i(\hat{n})$| is the detector noise in channel ‘i’. When the observed sky is digitized using healpix, the sky positions, |$\hat{n}$|⁠, are equivalently described by pixel indices ‘p’ whose pixel centres represent the direction of photons reaching us.

Taking linear combination of raw maps from different frequencies, we get an estimate of the CMB sky to be

(A2)

where |$\Delta T_{\rm res}(p) = \sum _{i=1}^{n_f} w_i [F_i (p) + N_i (p)]$| and |$n_f$| are the total number of frequency channels. Thus, the ILC weights are obtained by minimizing the variance of the cleaned map, |$\Delta \hat{T}_c (\hat{n})$|⁠, subject to the constraint that |$\sum _i w_i=1$| so that the cosmic CMB signal remains untouched while residual term is minimum or effectively zero. The variance of cleaned CMB map is then given by

(A3)

where |${\boldsymbol w} = (w_1, w_2,\ldots , w_{n_f})^T$| is the |$n_f \times 1$| column vector of weights, |$\langle ... \rangle$| represents expectation value of a quantity inside the angular brackets, and

(A4)

is the covariance matrix between different frequency maps and |$\overline{\Delta T}_i$| is the average of all pixels of frequency map ‘i’.

Since the foreground strength varies across the sky, the ILC procedure is applied by dividing the observed sky into different regions as shown in Fig. A1. In WMAP’s 1 yr data release, a cleaned CMB map using ILC method was obtained by a non-linear minimization procedure (Bennett et al. 2003b). However, Eriksen et al. (2004) showed that the ILC weights can be obtained analytically using the Lagrange multiplier method as

(A5)

where |${\boldsymbol e} = (1,1,\ldots ,1)^T$| is an |$n_f \times 1$| column vector, and |${\hat{\boldsymbol w}}$| are the estimated weights for taking linear combination of raw satellite maps. Cleaned CMB maps thus obtained using the ILC procedure as provided by the WMAP team were used in this study.

Mask from WMAP 9 yr data release depicting the 11 regions used to obtain the composite ILC map. Regions are selected depending on the strength of the foreground signal that varies across the sky (from grey to blue to green to dark red).
Figure A1.

Mask from WMAP 9 yr data release depicting the 11 regions used to obtain the composite ILC map. Regions are selected depending on the strength of the foreground signal that varies across the sky (from grey to blue to green to dark red).

To employ real/pixel-space ILC method, all the input raw maps should have the same beam and pixel resolution. So, the raw maps having different beam and pixel resolution were repixelized so that they have a common beam resolution given by a Gaussian beam of |$\mathrm{ FWHM}=1^\circ$| at |$N_{\rm side}$| = 512 following

(A6)

in harmonic space, where |$b_l$| is the circularized beam transfer function and |$p_l$| being the pixel window function corresponding to the  |$N_{\rm side}$| of a healpix digitized map. Here, |$b_l^{\rm in}=b_l^i$| where |$i=K,Ka,Q,V,W$| bands of WMAP and |$b_l^{\rm out}=b_l^{1^\circ }$|⁠, i.e. a 1° FWHM Gaussian beam transfer function. These |$a_{lm}^{\rm out}$| are then converted into a map using healpix.

We also made use of ESA’s Planck satellite data as provided by Planck collaboration through their 2015 and 2018 data releases (for which complementary simulations are available). Particularly, we made use of the smica-cleaned CMB maps in this work. They are available at a much higher resolution of healpix  |$N_{\rm side}$| = 2048. So, these are downgraded to get smica CMB maps at |$N_{\rm side}$| = 512 smoothed to have a Gaussian beam of |$\mathrm{ FWHM}=1^\circ$|⁠, just like WILC CMB maps following equation (A6). We note that smica foreground cleaning procedure is also an ILC method, but performed in harmonic space using |$a_{lm}^i$|⁠, i.e. spherical harmonic coefficients of raw satellite maps from different frequencies in which Planck made microwave sky observations, viz. 30, 44, 70, 100, 143, 217, 353, 545, and 857 GHz. The weights are computed using the formula

(A7)

similar to equation (A5), where |$C_{ij}(l) = \sum _{m=-l}^l a_{lm}^i a^{j*}_{lm}$|⁠. Specifically, weights for the smica procedure are obtained by using fitted elements of the cross frequency channel covariance matrix |$C_{ij}(l)$| as a function of ‘l’ via a minimization procedure. For more details, the reader may consult Cardoso et al. (2008).

Now, in order to use Planck 2013 PR1 data, the complementary simulations are no longer available with the release of Planck PR2 and PR3 data sets. However, we can still make use of this data set by employing a cleaning procedure, and then processing the simulations in the same way. Here, we adopt the pixel-space ILC method, described above, to clean the Planck 2013 raw maps. However, we use only the observed raw satellite maps in 30, 44, 70, 100, 143, 217, and 353 GHz frequency bands to produce cleaned CMB sky, which is referred to as PR1 ILC. To clean the satellite maps, we used the WMAP 9 yr region masks (shown in Fig. A1) for iterative cleaning of microwave sky. All these frequency maps are first downgraded to |$N_{\rm side}$| = 512 and smoothed to have a Gaussian beam of |$\mathrm{ FWHM}=1^\circ$|⁠, following equation (A6). The ILC weights thus obtained are given in Table A1.

Table A1.

ILC weights corresponding to the 12 regions (indexed 0 to 11) defined by the WMAP 9 yr regions’ mask shown in Fig. A1 to derive a cleaned CMB map from Planck PR1 data. All the frequency bands labelled 30, 44, |$\ldots$|⁠, 353 are in units of ‘GHz’.

Region304470100143217353
00.050 3858–0.077 6323–1.181 15171.560 16081.575 2080–0.976 37560.049 4050
10.045 4710–0.128 2175–0.639 20351.357 55881.214 3440–0.902 03800.052 0853
20.001 3979–0.232 57340.050 68730.828 20150.960 1726–0.643 89500.036 0092
30.031 9588–0.234 5117–0.062 60220.741 93770.927 8901–0.411 49670.006 8239
40.020 9488–0.199 2118–0.242 91890.685 50181.161 7237–0.433 49800.007 4544
5–0.018 0088–0.346 13481.019 2336–0.201 80880.396 99760.184 3588–0.034 6377
60.066 8860–0.087 3926–0.981 56140.927 61511.608 2933–0.534 96760.001 1272
70.064 4619–0.008 3785–1.258 85801.075 46681.783 5900–0.666 59630.010 3141
80.238 8520–0.799 9371–0.349 76201.174 91541.465 5975–0.755 95600.026 2902
9–0.031 1495–0.176 96420.687 0286–0.690 50720.580 31130.742 9941–0.111 7130
10–0.000 01400.037 7577–1.080 44962.091 41971.330 2067–1.494 77170.115 8512
110.033 5069–0.106 5167–0.829 97051.144 62481.544 6750–0.824 97510.038 6556
Region304470100143217353
00.050 3858–0.077 6323–1.181 15171.560 16081.575 2080–0.976 37560.049 4050
10.045 4710–0.128 2175–0.639 20351.357 55881.214 3440–0.902 03800.052 0853
20.001 3979–0.232 57340.050 68730.828 20150.960 1726–0.643 89500.036 0092
30.031 9588–0.234 5117–0.062 60220.741 93770.927 8901–0.411 49670.006 8239
40.020 9488–0.199 2118–0.242 91890.685 50181.161 7237–0.433 49800.007 4544
5–0.018 0088–0.346 13481.019 2336–0.201 80880.396 99760.184 3588–0.034 6377
60.066 8860–0.087 3926–0.981 56140.927 61511.608 2933–0.534 96760.001 1272
70.064 4619–0.008 3785–1.258 85801.075 46681.783 5900–0.666 59630.010 3141
80.238 8520–0.799 9371–0.349 76201.174 91541.465 5975–0.755 95600.026 2902
9–0.031 1495–0.176 96420.687 0286–0.690 50720.580 31130.742 9941–0.111 7130
10–0.000 01400.037 7577–1.080 44962.091 41971.330 2067–1.494 77170.115 8512
110.033 5069–0.106 5167–0.829 97051.144 62481.544 6750–0.824 97510.038 6556
Table A1.

ILC weights corresponding to the 12 regions (indexed 0 to 11) defined by the WMAP 9 yr regions’ mask shown in Fig. A1 to derive a cleaned CMB map from Planck PR1 data. All the frequency bands labelled 30, 44, |$\ldots$|⁠, 353 are in units of ‘GHz’.

Region304470100143217353
00.050 3858–0.077 6323–1.181 15171.560 16081.575 2080–0.976 37560.049 4050
10.045 4710–0.128 2175–0.639 20351.357 55881.214 3440–0.902 03800.052 0853
20.001 3979–0.232 57340.050 68730.828 20150.960 1726–0.643 89500.036 0092
30.031 9588–0.234 5117–0.062 60220.741 93770.927 8901–0.411 49670.006 8239
40.020 9488–0.199 2118–0.242 91890.685 50181.161 7237–0.433 49800.007 4544
5–0.018 0088–0.346 13481.019 2336–0.201 80880.396 99760.184 3588–0.034 6377
60.066 8860–0.087 3926–0.981 56140.927 61511.608 2933–0.534 96760.001 1272
70.064 4619–0.008 3785–1.258 85801.075 46681.783 5900–0.666 59630.010 3141
80.238 8520–0.799 9371–0.349 76201.174 91541.465 5975–0.755 95600.026 2902
9–0.031 1495–0.176 96420.687 0286–0.690 50720.580 31130.742 9941–0.111 7130
10–0.000 01400.037 7577–1.080 44962.091 41971.330 2067–1.494 77170.115 8512
110.033 5069–0.106 5167–0.829 97051.144 62481.544 6750–0.824 97510.038 6556
Region304470100143217353
00.050 3858–0.077 6323–1.181 15171.560 16081.575 2080–0.976 37560.049 4050
10.045 4710–0.128 2175–0.639 20351.357 55881.214 3440–0.902 03800.052 0853
20.001 3979–0.232 57340.050 68730.828 20150.960 1726–0.643 89500.036 0092
30.031 9588–0.234 5117–0.062 60220.741 93770.927 8901–0.411 49670.006 8239
40.020 9488–0.199 2118–0.242 91890.685 50181.161 7237–0.433 49800.007 4544
5–0.018 0088–0.346 13481.019 2336–0.201 80880.396 99760.184 3588–0.034 6377
60.066 8860–0.087 3926–0.981 56140.927 61511.608 2933–0.534 96760.001 1272
70.064 4619–0.008 3785–1.258 85801.075 46681.783 5900–0.666 59630.010 3141
80.238 8520–0.799 9371–0.349 76201.174 91541.465 5975–0.755 95600.026 2902
9–0.031 1495–0.176 96420.687 0286–0.690 50720.580 31130.742 9941–0.111 7130
10–0.000 01400.037 7577–1.080 44962.091 41971.330 2067–1.494 77170.115 8512
110.033 5069–0.106 5167–0.829 97051.144 62481.544 6750–0.824 97510.038 6556

The cleaned CMB map obtained using ILC method on Planck PR1 data, specifically using 30–353 GHz channel raw maps, and the corresponding inpainted map thus obtained are shown in Fig. A2.

Top: Cleaned CMB map obtained from Planck PR1 data using 30–353 GHz raw frequency maps, cleaned using ILC method. Bottom: Same map inpainted using isap with the mask depicted in Fig. 1.
Figure A2.

Top: Cleaned CMB map obtained from Planck PR1 data using 30–353 GHz raw frequency maps, cleaned using ILC method. Bottom: Same map inpainted using isap with the mask depicted in Fig. 1.

A2 Simulations

Frequency-specific mock maps for WMAP data are generated as follows. A random realization of the CMB sky is created at |$N_{\rm side}$| = 512 using the fiducial theoretical power spectrum (⁠|$C_l^{\mathrm{ th}}$|⁠) from that release. It is then smoothed with the frequency-specific beam transfer function, |$b_l^i$|⁠, and is then added with frequency-specific noise. The WMAP frequency-specific noise maps are generated as Gaussian noise in each pixel ‘p’ using the noise rms of each channel (⁠|$\sigma _0^i$|⁠), and the |$N_{\rm obs}^i (p)$| map that gives the effective number of observations per pixel in a frequency band ‘i’. Zero mean, unit variance Gaussian random number arrays of the same dimension as the number of pixels in frequency-specific maps (⁠|$N_{\rm pix} = 12\times N_{\rm side}^2$|⁠) are generated and then multiplied by the noise rms map per pixel given by |$\sigma _i(p)=\sigma _0^i/\sqrt{N^i_{\rm obs}(p)}$| to create a band-specific noise simulation. It is then added to the channel-specific beam-smoothed CMB realization. Now, all these noisy CMB maps are repixelized following equation (A6) so that they have a common |$N_{\rm side}$| = 512 and beam resolution due to a Gaussian beam of |$\mathrm{ FWHM}=1^\circ$|⁠. The noise rms, |$\sigma^i_0$|⁠, maps of effective number of observations per pixel, |$N_{\rm obs}^i (p)$|⁠, and the WMAP frequency-specific beam transfer functions, |$b_l^i$|⁠, are provided as part of each WMAP data release at NASA’s LAMBDA webpage.

Once the smoothed noisy frequency-specific CMB maps are obtained, they are combined using the same region-specific ILC weights obtained from data. Thus, we generate 1000 mock WILC maps corresponding to each data release from WMAP.

Simulated smica CMB maps from Planck satellite are provided as part of each data release by the Planck collaboration by processing the FFP simulations in the same way as smica CMB map is obtained from observational data. smica map is provided at a higher resolution of |$N_{\rm side}$| = 2048 with a Gaussian beam smoothing of |$\mathrm{ FWHM}=5 \ \mathrm{ arcmin}$|⁠. Hence, these maps are also repixelized to |$N_{\rm side}$| = 512 and whose beam window function is given by a Gaussian with |$\mathrm{ FWHM}=1^\circ$| following equation (A6) (by taking |$b_l^{\rm in}=b_l^{5^{\prime }}$|⁠, |$b_l^{\rm out}=b_l^{1^\circ }$|⁠, |$p_l^{\rm in}=p_l^{2048}$|⁠, and |$p_l^{\rm out}=p_l^{512}$|⁠) similar to WILC maps.

Now, to generate mock CMB maps for Planck’s PR1 data, the ILC weights used to clean the raw satellite maps from Planck PR1 are applied to the simulated FFP frequency realizations, iteratively, after processing them similar to data. We recall that Planck-provided raw maps are available at |$N_{\rm side}$| = 1024 for 30, 44, and 70 GHz bands (LFI bands) and at |$N_{\rm side}$| = 2048 for 100, 143, 217, 353, 545, and 857 GHz bands (HFI bands).So, they are processed to bring all of them to a common beam and pixel resolution of |$1^\circ$| FWHM Gaussian beam and |$N_{\rm side}$| = 512, respectively. Thus, we generated 1000 mock PR1 ILC maps from the corresponding frequency-specific FFP realizations. Note that we did not use the last two high-frequency bands in obtaining Planck PR1 ILC CMB map.

We further note that WILC maps had a residual foreground bias correction applied based on simulated foreground cleaned CMB maps (Hinshaw et al. 2007). However, such a bias correction procedure was not employed on the CMB maps recovered using any of the four component separation methods (in real or harmonic space) employed by the Planck collaboration. So, we also did not apply any such corrections to PR1 ILC CMB map.

APPENDIX B: MASKS USED

The presence of residual foregrounds in the cleaned CMB maps can bias our inferences. Thus, such regions of the sky are masked and inpainted using the isap package. However, there will also be a bias introduced in the inpainted CMB maps if large fractions of the sky have to be inpainted. Since we are interested in CMB multipoles |$l \le 61$|⁠, we use a single mask that has largely contiguous sky regions, but also masks extended regions with potential foreground residuals. It is obtained by combining WMAP’s 9 yr Kp8 temperature cleaning mask and Planck’s 2018 common inpainting mask for temperature analysis as described below. WMAP’s 9 yr Kp8 mask that is available at healpix  |$N_{\rm side}$| = 512 is upgraded to |$N_{\rm side}$| = 2048 after removing small point sources from it. Then, it is combined (multiplied) with Planck 2018 common inpainting mask provided for intensity data. The combined mask thus obtained is then convolved with a Gaussian beam of |$\mathrm{ FWHM}=1^\circ$| while deconvolving with a Gaussian beam of |$\mathrm{ FWHM}=5 \ \mathrm{ arcmin}$|⁠, and repixelized at |$N_{\rm side}$| = 512. This combined smoothed mask is then thresholded such that those pixels that have a value |$\ge \!\! 0.8$| are set to ‘1’ and rest are set to ‘0’. Mask thus obtained has a sky fraction of  |$f_{\rm sky}$|  |$\approx 0.929$|⁠, which was shown in Fig. 1.

The data as well as simulated CMB maps corresponding to various data releases from WMAP and Planck missions are all inpainted using this mask.

APPENDIX C: SMOOTHED K- AND Ka-BAND MAPS FROM WMAP 1 AND 3 yr DATA RELEASE

There are few details to be noted in the generation of mock WILC CMB maps described in the previous section, and our observations while carrying out this analysis.

Since WMAP’s K and |$Ka$| frequency channel detectors are of low resolution, the effective circularized beam transfer functions (⁠|$b_l^i$|⁠) of these two bands were determined up to |$l_{\rm max}=750$| and 850, respectively, by the WMAP team. However, beam transfer functions that are provided cannot be used as such, since K-band |$b_l$| from first year data are positive only up to |$l=603$|⁠, and in 3 yr data release K- and |$Ka$|-band |$b_l$| are positive up to only |$l=718$| and 845, respectively. (Here, we also note that WMAP’s first year Q-band |$b_l$| are provided only up to |$l_{\rm max}=1000$|⁠. Since the maps are being synthesized at |$N_{\rm side}$| = 512, in general one uses mode information up to |$l_{\rm max}=2\times N_{\mathrm{ side}}$| when employing healpix, i.e. |$l_{\rm max}=1024$| in our case.)

In order to perform ILC cleaning on raw satellite data, the individual frequency-specific maps from WMAP are synthesized at the same pixel resolution of |$N_{\rm side}$| = 512 and a common beam smoothing given by a Gaussian kernel of |$\mathrm{ FWHM}=1^\circ$| (which is slightly greater than the resolution of WMAP’s K-band detector’s effective Gaussian width). Since the input and output maps are at |$N_{\rm side}$| = 512 in this case, |$p_l^{\rm in}=p_l^{\rm out}$|⁠. The effective beam smoothing applied to each frequency map is then |$b_l^{i,{\rm eff}}=b_l^{1^\circ }/b_l^i$|⁠. Thus, in obtaining |$1^\circ$| Gaussian beam smoothed raw maps, only the positive circularized |$b_l^i$| of K and |$Ka$| bands were used in computing |$b_l^{i,{\rm eff}}$|⁠, and the rest were set to zero.

However, this procedure seems to have been used from WMAP 5 yr data analysis onwards uniformly for processing all frequency maps, but not in 1 and 3 yr WMAP data analysis, especially K- and |$Ka$|-band maps. Our observations are presented in Fig. C1. In the top panel, power spectrum plots of WMAP’s first year |$1^\circ$| Gaussian beam smoothed K- and |$Ka$|-band maps as available from NASA’s LAMBDA site and their power spectrum as obtained by us following equation (A6) are shown. Also shown are the power spectra of K- and |$Ka$|-band maps that are obtained using respective |$b_l^i$| as given, but only up to some low multipole (i.e. not all positive |$b_l^i$| were used), beyond which extrapolated |$b_l^i$| are employed. These extrapolated |$b_l^i$| were obtained by us, through trial and error, such that we are able to match the power spectra of smoothed K- and |$Ka$|-band maps thus obtained following equation (A6), with the power spectra of smoothed K- and |$Ka$|-band maps as provided by WMAP team.

Power spectra of raw satellite maps from WMAP’s K and $Ka$ bands provided by WMAP team as part of WMAP’s 1 and 3 yr data products, and as obtained by us following equation (A6).
Figure C1.

Power spectra of raw satellite maps from WMAP’s K and |$Ka$| bands provided by WMAP team as part of WMAP’s 1 and 3 yr data products, and as obtained by us following equation (A6).

One readily notices that there is an artificial rise in the power at high multipoles when one uses equation (A6) utilizing all positive |$b_l^i$| of K- and |$Ka$|-band maps as given. This could be the reason for using extrapolated |$b_l^i$| by WMAP team for these two band maps in deriving |$1^\circ$| Gaussian beam smoothed raw maps that are eventually used in obtaining a cleaned CMB map employing ILC method. However, these |$b_l^{i,{\rm eff}}$| to get smoothed raw maps are not made publicly available to be able to appropriately simulate ILC-like maps from WMAP.

The bottom panel of Fig. C1 is same as the top panel but corresponds to WMAP 3 yr K- and |$Ka$|-band maps. We note that the rise in smoothed raw maps’ power is seen in K-band only in first year, and in both K- and |$Ka$|-band map powers in 3 yr data owing to difference in fitted circularized beam transfer functions of corresponding detectors. These combination |$b_l^i$| containing partly the circularized |$b_l^i$| of K- and |$Ka$|-bands as provided and the extrapolated beam transfer function found by us (through trial and error) were used to simulate smoothed noisy frequency-specific CMB maps to which ILC weights were applied in generating mock ILC-cleaned CMB maps.

We were able to match the power spectrum of WMAP’s first year |$1^\circ$| beam smoothed K-band raw map, as provided, with the WMAP 1 yr K-band map’s power spectrum by using |$b_l^{K}$| up to |$l=551$| as given, and fitting them using UnivariateSpline method of scipy (a python software library) choosing the degree of spline to be |$k=2$| (i.e. using a quadratic spline) to obtain extrapolated |$b_l^K$| up to |$l=1024$|⁠. Then, the extrapolated and given beam transfer functions of K band are combined at |$l=508$|⁠. Similarly, for WMAP’s 3 yr K band, we found (by trial and error) that interp1d method of scipy with the parameter choice kind = ‘slinear’ (first order/linear spline) gives extrapolated |$b_l$| from |$l=570$| onwards such that the combined |$b_l$| result in a raw map power spectrum, following equation (A6), that matches with the smoothed raw maps’ |$C_l$| from WMAP 3 yr data. Thus, combined |$b_l$| up to a maximum multipole of |$l=750$| were used for obtaining smoothed K-band map, and up to |$l=830$| were used to get |$Ka$|-band smoothed map.

APPENDIX D: SMOOTHED LFI MAPS FROM PLANCK PR1 DATA

We discussed the problem of appropriately simulating |$1^\circ$| Gaussian beam smoothed maps corresponding to K and |$Ka$| bands that match with WMAP’s 1 and 3 yr smoothed K- and |$Ka$|-band data maps as provided by WMAP team in the previous section.

We are faced with a similar problem in trying to employ real space ILC method with Planck PR1 low-frequency maps, specifically with the 30 GHz channel. Since we also chose to repixelize all the maps being used in this study to |$N_{\rm side}$| = 512 having a beam smoothing given by a Gaussian kernel with |$\mathrm{ FWHM}=1^\circ$|⁠, Planck 30 GHz channel poses a similar problem. The circular beam transfer functions of all frequency maps from Planck 2013 data release are shown in Fig. D1.

Circular beam transfer functions ($b_l$) of all frequency maps that we used from Planck PR1 data. One can easily notice the unphysical upward trend of the 30 GHz channel’s effective circular $b_l$ as provided by Planck collaboration. Similar trend for 44 GHz is not a concern for this study.
Figure D1.

Circular beam transfer functions (⁠|$b_l$|⁠) of all frequency maps that we used from Planck PR1 data. One can easily notice the unphysical upward trend of the 30 GHz channel’s effective circular |$b_l$| as provided by Planck collaboration. Similar trend for 44 GHz is not a concern for this study.

It is clear from the figure that beam transfer functions of Planck’s 30 GHz frequency map from PR1 as provided are not usable beyond |$l \sim 850$| or so after which it shows an unphysical upward trend. Hence, we adopt the same strategy as used for WMAP’s K- and |$Ka$|-band maps from the 1 and 3 yr data releases described in the preceding section.

We fit the Planck PR1 30 GHz channel’s |$b_l$| as given for multipoles up to |$l=860$| using a spline. Then, the beam transfer functions as provided up to |$l=773$| are appended with the extrapolated |$b_l$| obtained from the fit, where the two cross each other. The extrapolated |$b_l$| were obtained by a fit to the given |$b_l$| for 30 GHz detector using UnivariateSpline functionality of scipy, a python software library, with the parameter |$k=2$|⁠, i.e. a quadratic spline. The effective (extrapolated) |$b_l$| are generated up to |$l=1100$|⁠. Then following equation (A6) Planck PR1 30 GHz map was synthesized at |$N_{\rm side}$| = 512 having |$1^\circ$| Gaussian beam smoothing with mode information up to |$l_{\rm max}=1024$|⁠.

One can also see from Fig. D1 that the 44 GHz detector beam transfer function also shows a similar unphysical upward trend, but at a much higher multipole value. So, there was no need for such a procedure to repixelize frequency maps other than 30 GHz channel map at |$N_{\rm side}$| = 512. The beam transfer functions are well behaved up to |$l=1024$| for rest of the frequency maps.

We also note that this can be addressed in two other ways. As in WMAP 5 yr and later data releases, |$a_{lm}^i$| of frequency maps in generating the smoothed maps can be set to zero for modes beyond that multipole for which |$b_l$| are not provided or are not physically acceptable. A better way to address this is to use harmonic space ILC using only those modes (⁠|$a_{lm}^i$|⁠) from frequency channels where |$b_l$| are available/acceptable to deconvolve the observed map for detector beam smoothing effects (see, for example, Tegmark et al. 2003).

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