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Ignasi Pérez-Ràfols, Jordi Miralda-Escudé, Britt Lundgren, Jian Ge, Patrick Petitjean, Donald P. Schneider, Donald G. York, Benjamin A. Weaver, The cross-correlation of Mg ii absorption and galaxies in BOSS, Monthly Notices of the Royal Astronomical Society, Volume 447, Issue 3, 1 March 2015, Pages 2784–2802, https://doi.org/10.1093/mnras/stu2645
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Abstract
We present a measurement of the cross-correlation of Mg ii absorption and massive galaxies, using the Data Release (DR)11 main galaxy sample of the Baryon Oscillation Spectroscopic Survey (BOSS) of Sloan Digital Sky Survey III (SDSS-III; CMASS galaxies), and the DR7 quasar spectra of SDSS-II. The cross-correlation is measured by stacking quasar absorption spectra shifted to the redshift of galaxies that are within a certain impact parameter bin of the quasar, after dividing by a quasar continuum model. This results in an average Mg ii equivalent width as a function of impact parameter from a galaxy, ranging from 50 kpc to more than 10 Mpc in proper units, which includes all Mg ii absorbers. We show that special care needs to be taken to use an unbiased quasar continuum estimator, to avoid systematic errors in the measurement of the mean stacked Mg ii equivalent width. The measured cross-correlation follows the expected shape of the galaxy correlation function, although measurement errors are large. We use the cross-correlation amplitude to derive the bias factor of Mg ii absorbers, finding |$b_{\mathrm{Mg\,\small {II}}}=2.33\pm 0.19$|, where the error accounts only for the statistical uncertainty in measuring the mean equivalent width. This bias factor is larger than that obtained in previous studies and may be affected by modelling uncertainties that we discuss, but if correct it suggests that Mg ii absorbers at redshift z ≃ 0.5 are spatially distributed on large scales similarly to the CMASS galaxies in BOSS.
1 INTRODUCTION
The Mg ii doublet absorption line, at rest-frame wavelengths λ = 2796.3543 and 2803.5315 Å, is an extremely useful tracer of photoionized gas clouds in galactic haloes. Several reasons account for this trait: magnesium is among the most abundant of the heavy elements, the oscillator strength of this Mg ii doublet is particularly large, its rest-frame wavelength makes it easily observable from ground-based telescopes at redshifts z > 0.3, and magnesium is mostly in the form of Mg ii in photoionized, self-shielded clouds at the typical pressures of galactic haloes. Gas clouds with atomic hydrogen column densities |$N_{\rm H\,\small {I}} \lesssim 2\times 10^{17}\, {\rm cm}^{-2}$| are optically thin to photons above the hydrogen ionization potential of 13.6 eV, as well as to the harder photons that ionize Mg ii. Most of the magnesium is therefore ionized more than once in thin clouds, greatly reducing the Mg ii column density. On the other hand, in optically thick clouds, the shielded magnesium ions are mostly recombined to Mg ii, but Mg i has an ionization potential of 7.65 eV (below that of hydrogen) and is ionized by photons that penetrate the region of self-shielded hydrogen. Hence, self-shielded clouds in galactic haloes should have most of their magnesium as Mg ii (e.g. Bergeron & Stasińska 1986). In fact, most strong Mg ii systems are also Lyman limit systems, i.e. their H i column densities are high enough to be self-shielding (Rao, Turnshek & Nestor 2006).
The rest-frame equivalent width distribution of Mg ii absorption systems is approximated by an exponential form, dN/dz ∝ exp (−W/W*), with a value W* ≃ 0.6 Å at z = 0.5 that increases gradually with redshift, and an excess of systems over this form at W < 0.3 Å (Nestor, Turnshek & Rao 2005; Narayanan et al. 2007, and references therein). Most of the strong systems have a complex velocity structure, with a velocity dispersion of multiple absorbing components that is characteristic of galaxy velocity dispersions, favouring models of a collection of photoionized clouds randomly moving through a galactic halo (Bahcall 1975; Sargent et al. 1979; Churchill et al. 2000), as had already been proposed by Bahcall & Spitzer (1969).
The association of Mg ii absorption systems with galactic haloes was firmly established with the work of Lanzetta & Bowen (1990), Bergeron & Boissé (1991) and Steidel, Dickinson & Persson (1994). The observations of the frequency of occurrence of Mg ii absorbers at different impact parameters from luminous galaxies led to a simple model of haloes that are close to spherical, in which absorption with rest-frame equivalent width W > 0.3 Å is nearly always observed within an impact parameter |$r_{\rm p} \lesssim 50 (L_{\rm K}/L_{\rm K}^{*})^{0.15}\, {\rm kpc}$| of a galaxy of K-band luminosity LK, and becomes rapidly weaker at larger radii, independently of the type of galaxy being considered (Steidel 1995). Actually, the natural expectation is that there is a smooth profile of declining mean Mg ii absorption strength with impact parameter around a galaxy, caused by a decreasing density of clouds with radius in a galactic halo. This is consistent with more recent work, where the mean Mg ii equivalent width (which is indicative of the number of intersected individual clumps with saturated absorption) has been shown to steeply decline with the impact parameter rp roughly as |$\overline{W} \propto r_{\rm p}^{-1.5}$| (Chen et al. 2010a), with a characteristic radius at a fixed |$\overline{W}$| that scales proportionally to |$R_{\rm Mg\,\small {II}}\propto {M_{*}}^{0.3} (\mathrm{sSFR})^{0.1}$| (Chen et al. 2010b), where M* is the stellar mass in the galaxy and sSFR is the star formation rate per unit of stellar mass. We also note that this describes the mean profile of Mg ii absorption around galaxies, and that there are rare cases where Mg ii absorption is absent even at very small impact parameter from luminous galaxies (Johnson et al. 2014).
The large extent of the gaseous haloes traced by metal absorbers and their nearly ubiquitous presence around all massive galaxies, with only a weak dependence on the specific star formation rate, are observational facts providing support to a scenario in which the Mg ii absorbers are a signature of the accretion process of new material on to galaxies. Accreting gas at the temperatures of virialization in galactic haloes is thermally unstable and should naturally form photoionized clouds whenever the cooling time of hot halo gas is short compared to the age of the galaxy. This behaviour naturally leads to a two-phase model of gaseous galactic haloes, where cool clouds can form in approximate pressure equilibrium with a hot medium and are produced in abundance within the cooling radius (Spitzer 1956; Mo & Miralda-Escudé 1996; Maller & Bullock 2004). On the other hand, there is evidence at small radii pointing to the impact of galactic winds on Mg ii absorbers: the absorbers are more numerous near the minor axis of their associated galaxies (Bordoloi et al. 2011, 2012; Kacprzak et al. 2011; Kacprzak, Churchill & Nielsen 2012; Lundgren et al. 2012). The distribution of Mg ii absorption systems around galaxies is therefore likely to be sensitive to processes involving both inflow and outflow of material into and from the regions containing the bulk of the stellar mass in galaxies.
The association of Mg ii absorbers with galaxies implies a large-scale cross-correlation of these objects. The cross-correlation is in general a result of two effects. First, if every galaxy is surrounded by a gas halo, a Mg ii absorber located at an impact parameter rp from a galaxy may actually be associated with this galaxy, and be part of the gas halo around it. Secondly, the Mg ii absorber may be associated with a different galaxy that may be a satellite of the first, or with an unrelated galaxy that is spatially correlated with the first, following the usual galaxy autocorrelation. These are usually described as the 1-halo and 2-halo terms, although Mg ii systems are considered to be associated with galaxies, rather than dark matter haloes. In the limit of impact parameters much smaller than the typical size of a galaxy halo, the first term, determined by the gas halo profile around each galaxy (e.g. Tinker & Chen 2008), dominates, whereas in the limit of large impact parameters, the second term is the important one. The total cross-correlation is in general a combination of the two terms over a wide range of intermediate impact parameters, and it is impossible to cleanly separate the two contributions. But in the large-scale limit, the cross-correlation of Mg ii absorbers and galaxies should follow the form of the galaxy correlation function, with an amplitude that is proportional to the product of the two bias factors of the two populations. Hence, measuring the large-scale clustering amplitude helps determine the bias factor, and therefore the halo population that the Mg ii absorbing clouds are associated with.
The large-scale Mg ii–galaxy cross-correlation was first measured using the photometric catalogue of luminous red galaxies in the Sloan Digital Sky Survey (SDSS; see York et al. 2000) and the set of individually detected Mg ii absorbers in the spectra of SDSS quasars by Bouché, Murphy & Péroux (2004), Bouché et al. (2006), Lundgren et al. (2009), Gauthier, Chen & Tinker (2009) and Lundgren et al. (2011). In the absence of precise galaxy redshifts, only the projected cross-correlation function can be measured. The work by Lundgren et al. (2009), based on a set of 2705 Mg ii absorbers with rest-frame equivalent width W > 0.8 Å over the redshift interval 0.36 < z < 0.8, found that the form of the projected cross-correlation is well matched by the luminous red galaxy autocorrelation in the impact parameter range 0.3 h−1Mpc < rp < 30 h−1Mpc, and measured the bias factor of these Mg ii systems to be bMg = 1.10 ± 0.24. Gauthier et al. (2009) performed a similar analysis for a sample of 1158 Mg ii absorbers with W < 1 Å over the redshift interval 0.4 < z < 0.7 and found the bias factor of these Mg ii systems to be bMg = 1.36 ± 0.38. Both works found an indication that weak absorbers, with W < 1.5 Å, cluster more strongly (i.e. they have a larger bias factor) than strong absorbers, and are therefore located in more massive haloes on average, although this result was not of high statistical significance. The method used by Bouché et al. (2006), Lundgren et al. (2009) and Gauthier et al. (2009), based on a catalogue of identified Mg ii systems, requires careful attention to the selection function of both galaxies and Mg ii systems through an extensive use of simulations, because the number of absorbers will obviously be enhanced in regions of the survey containing more galaxies and more quasar spectra, or where the spectra are of higher signal-to-noise ratio (S/N), owing to variable observing conditions and also intrinsic clustering of the quasar sources.
We present a different approach in this paper to measure the cross-correlation of massive galaxies and Mg ii absorbers, based on the galaxies with spectroscopically measured redshifts of the new Baryon Oscillation Spectroscopic Survey (BOSS) of the SDSS-III Collaboration (Eisenstein et al. 2011; Dawson et al. 2013). Instead of identifying individual Mg ii absorbers, we use a stacking method to measure the average Mg ii absorption around a galaxy as a function of the impact parameter and redshift separation. In other words, we measure the redshift-space cross-correlation function of galaxies and Mg ii absorption. Our approach is similar to that of Zhu & Ménard (2013b), who have measured the mean Ca i absorption around galaxies, and to Zhu et al. (2013), who have obtained a similar measurement of the large-scale Mg ii absorption; we compare their results with ours and discuss the differences near the end of this paper. The data set we use is described in Section 2, and the method is presented in detail in Sections 3 and 4. We present the results in Section 5, which are applied to infer the mean bias factor of Mg ii systems in Section 6. Finally, we summarize our conclusions in Section 7. Throughout this paper, we use the Λ cold dark matter model with H0 = 68 km s−1 Mpc−1 and Ωm = 0.3.
2 DATA SAMPLE
The first step in the analysis is to identify quasar–galaxy pairs in which the quasar sightline passes within a specified bin of projected proper radius, or impact parameter rp, from the foreground galaxy. For the background quasar sample, we use the quasar catalogue of Schneider et al. (2010) from the 7th Data Release (DR7; Abazajian et al. 2009) of the SDSS-II Collaboration (Gunn et al. 1998, 2006; York et al. 2000; Eisenstein et al. 2011; Bolton et al. 2012; Smee et al. 2013), with 105 783 spectroscopically confirmed quasars. For the galaxies, the CMASS catalogue (Dawson et al. 2013) of the SDSS-III Collaboration that is prepared for the DR11 [extension of the SDSS DR9 (Ahn et al. 2012) and the SDSS DR10 (Ahn et al. 2013)] is used, which contains a total of 938 280 galaxies. The DR11 galaxies represent the majority of the final BOSS sample, also covering most of the sky area included in DR7. We note that this galaxy catalogue is the same that was used by Zhu et al. (2013), even though they refer to it as the luminous red galaxy catalogue. We exclude any galaxies at redshift lower than 0.35, corresponding to |$1+z=\lambda _{\rm min}/\lambda _{\mathrm{Mg\,\small {II}}}$|, where we set λmin = 3800 Å as the shortest wavelength with sufficient S/N to provide a useful Mg ii absorption signal. This requirement reduces the galaxy sample to 895 472 galaxies. The quasar sample could be increased by including the DR11 sample from BOSS, but most of the new quasars in DR11 are fainter than those in DR7 (having therefore lower S/N) and are at a high redshift, at which the Mg ii lines associated with the CMASS galaxies appear superposed with the Lyα forest.
The luminosity and redshift distributions of all the DR11 CMASS galaxies meeting these two conditions for at least one quasar that is within an impact parameter bmax = 12.8 Mpc, as computed from the angular separation at the redshift of the galaxy, are shown in Fig. 1. Note that the density of quasars in DR7 implies that each galaxy has on average ∼3 quasars within this impact parameter, therefore the majority of galaxies have at least one quasar pair and these distributions are nearly the same as those of the whole DR11 CMASS sample. These distributions represent the characteristics of the galaxies for which we measure the mean Mg ii absorption equivalent width as a function of impact parameter in this paper.
3 STACKING PROCEDURE
A crucial step to measure the Mg ii–galaxy cross-correlation, in the form of δτe, is to estimate the quasar continuum with a method that is, to the best possible degree, free of systematic errors when averaging over a large number of lines of sight. In particular, it is important to ensure that the presence of a Mg ii line itself, which in most cases may be too weak to be individually detected in the relatively low S/N SDSS quasar spectra, does not bias the estimate of the continuum. Obviously, if the spectral region where we expect to find the Mg ii line associated with a galaxy is used for the continuum determination, the continuum estimate may be systematically biased too low because of the presence of an undetected Mg ii line. This systematic bias may be important when stacking large numbers of spectra, even though the Mg ii lines causing the bias are not individually detected in any single spectrum.
To illustrate the importance of the quasar continuum determination for the problem of measuring the average Mg ii absorption around galaxies at large impact parameters, we explore two different methods and we perform a number of tests for the presence of systematic errors. The first method, designated as mean subtraction, is specifically designed for our problem, while the second method, designated as variable smoothing, fits a continuum by iteratively smoothing the spectrum with a variable smoothing length to flexibly fit both emission lines and featureless continuum regions. The latter method uses the entire spectrum to determine the continuum, including the region where the associated Mg ii line is expected, and is therefore subject to the systematic error described above. We now describe each method in detail. Tests of the methods that show that the mean subtraction method correctly recovers the mean equivalent width and the variable smoothing method is subject to various systematic errors, including the continuum fitting bias mentioned above, are presented in Appendix A.
3.1 Method 1: mean subtraction
The first approach uses the mean spectrum of all quasars as a continuum fit model. Each quasar spectrum is divided by the mean quasar spectrum, and then a linear fit to this ratio is obtained around the spectral region of the expected Mg ii line for each galaxy–quasar pair, but without using the narrower central interval where the Mg ii line should be located. This linear fit is used to further improve the continuum estimate, allowing for intrinsic variations of the quasar continua. The results are then stacked for all quasar–galaxy pairs at each interval of impact parameter, after shifting to the redshift of the galaxy in each pair, to obtain the final composite Mg ii absorption spectrum. We now explain each of these steps in detail.
3.1.1 Generating the mean spectrum
The mean quasar spectrum is generated using the DR7 quasar spectra following a similar approach as the one undertaken by Vanden Berk et al. (2001). The mean spectrum in Vanden Berk et al. (2001) was generated using 1800 quasars (fig. 3 of Vanden Berk et al. 2001), so our mean spectrum is more accurate because of the much larger number of quasars available in DR7. In addition, we normalize the spectra using a spectral window that is particularly suited to obtaining the most accurate continuum model in the region where Mg ii absorption lines are found. There is therefore a small difference between our mean spectrum and that of Vanden Berk et al. (2001).
3.1.2 Generating the composite Mg ii absorption spectra
The whole procedure is illustrated in Fig. 4 with a couple of examples, one with an individually detected Mg ii absorption system and one without any individually detected Mg ii absorption but with a random metal absorption line. Note that the contribution of these random metal absorption lines is later corrected for (Section 3.3).
3.2 Method 2: variable smoothing
3.3 Unbiasing the composite spectra
After the stacking of all the normalized spectra of quasar–galaxy pairs as a function of the velocity variable v has been completed by using either continuum fitting method, the mean value of the transmission |$\bar{F}_i$| that is obtained far from the expected Mg ii line (i.e. at large values of ‖v‖) is close to unity but not exactly so. The main reason for this is the presence of random metal absorption lines (unrelated to the galaxy of the pair) that are detected above a 3σ fluctuation and therefore excluded when fitting the continuum. Other reasons may be affecting this mean background of |$\overline{F}_i$| related to systematic effects in the noise distribution and the continuum fitting method. We eliminate this bias by performing the same linear fit to the stacked spectrum as in Section 3.1.2, using again the velocity intervals (−5000, −2000) and (2000, 5000) km s−1 to measure two average values of |$\overline{F}_i$|, and obtaining a linear fit based on two points at the centre of these intervals. The final normalized stacked flux is found by dividing by this linear fit.
Our results will actually be shown, for convenience, in terms of the effective excess optical depth, defined according to |$\delta \tau _{{\rm e},i} = - \log \bar{F}_i$|, in Figs 5 to 7.
3.4 Bootstrap errors
The errors computed from the known observational noise in the observed quasar spectra that are stacked are actually a lower limit to the true errors. In reality, the intrinsic variability of real quasar continua and of the associated Mg ii and other random metal absorption lines imply the presence of additional errors that are not taken into account and which are correlated among the pixels of the final stacks. We therefore compute bootstrap errors, which are generally used in our analysis and model fits in this paper.
To calculate these bootstrap errors, we use the BOSS plates as the regions of the sky in which the sample is divided. Each quasar is tagged with the plate number at which its best spectrum was observed. For DR7 there are Nplates = 1822 plates. Pairs are counted as belonging to the plate that contains the quasar, irrespective of the galaxy position.
Bootstrap errors are computed in the standard way, generating N = 1000 samples by randomly selecting Nplates among all the plates with repetition, and then recalculating the composite spectra using both methods. Bootstrap errors are assigned to the final effective optical depth τe, at each velocity bin and each impact parameter interval from the dispersion found among the 1000 random samples. These bootstrap errors are computed for both continuum fitting methods.
We note that, specially at large impact parameter, some galaxies will be paired to quasars in different plates. This implies the presence of residual correlations among the bootstrap samples because of the common galaxies in pairs belonging to different plates, but we believe this effect is negligibly small because the most important error correlations should arise from the quasar spectra.
4 MODEL FOR THE ABSORPTION PROFILE
The usual analysis in the astronomical literature of individual Mg ii absorption lines is done by fitting with Voigt profiles, with the equivalent width and the velocity dispersion as free parameters. Whenever the observed absorption profile is not adequately fitted in terms of the two Voigt profiles of the Mg ii doublet, one can include the presence of multiple cloud components with blended absorption lines in order to improve the fit. Here, we are analysing a stack of a large number of Mg ii absorption systems that may be mostly undetected individually, but for which we can accurately predict the expected mean position from the redshift of the galaxy near the quasar line of sight. The effective optical depth in the stack, |$\tau _{\rm e} = -\log (\bar{F})$|, should in this case have a single symmetric component for each line in the doublet, with a profile reflecting the velocity dispersion of Mg ii absorbing clouds and galaxies in haloes, as well as the large-scale halo correlation in redshift space for large impact parameters. This cross-correlation function can be modelled in terms of the halo occupation distribution formalism (e.g. Gauthier, Tinker & Chen 2008; Zhu & Ménard 2013a), but the density profile of Mg ii clouds in haloes does not have to follow that of galaxies, and it will generally depend on complex physics of galaxy winds and gas accretion in the circumgalactic medium. For simplicity, we shall assume in this section a model with a Gaussian velocity distribution and a power-law form for the projected correlation function, as an approximation to the generally complex form of the galaxy-absorber cross-correlation function. In the next section, we shall use a more accurate form of the correlation function obtained from halo simulations to determine the amplitude of our measured cross-correlation.
The fitting is performed by χ2 minimization, computed including all the pixels of the stacked spectra in the central interval |v| < 2000 km s−1. Each pixel is weighted according to the bootstrap error measured in that pixel as described in Section 3.4, but without considering the cross-correlations of the errors between pixels. In practice, the bootstrap error bars in different pixels of the stacked spectra are nearly equal. The spectrum outside the interval |v| < 2000 km s−1, which is used for deriving the continuum fit in Method 1, is not considered here for the fit. We note also that for a real Gaussian profile for each component of the Mg ii doublet, the continuum fitting of Method 1 implies that we formally need to subtract a small constant from the double Gaussian in equation (16), equal to the integrated value of the model absorption over the interval v ∈ (2000, 5000) km s−1 used for determining the continuum, but we neglect this effect here.
5 RESULTS
The results of the stacked absorption profiles are obtained for a total of 17 impact parameter intervals, measured in proper units at the redshift of the galaxy. The first interval is for rp < 50 kpc, and the other 16 intervals are 2(i−1)/2 < (rp/50 kpc) < 2i/2, for i = 1 to 16, up to a maximum impact parameter of 12.8 Mpc. The stacked profiles are shown as the effective optical depth, |$\tau _{\rm e}=-\log (\bar{F})$|, in Figs 5–7. Results are presented for our two continuum fitting methods, the mean subtraction method (thick, solid blue line) and the variable smoothing method (thin, solid red line). The error bars plotted on the left-hand side are the rms values of the bootstrap error of τe in one pixel, which has little variation among different pixels in each stacked spectrum. The results of the fitted model parameters and their bootstrap errors computed by repeating the fit for bootstrap realizations of the stacked profiles, are given in Table 1 (the cross-correlations of the parameter errors are omitted).
. | Mean subtraction . | Variable smoothing . |
---|---|---|
τ0 | 0.0060 ± 0.0001 | 0.0034 ± 0.0001 |
α | 0.70 ± 0.01 | 0.88 ± 0.01 |
σ0 ( km s−1) | 250 | 250 |
x | 1.35 ± 0.06 | 0.46 ± 0.08 |
q | 0.65 ± 0.03 | 0.66 ± 0.03 |
We0( km s−1) | 6.27 ± 0.10 | 3.58 ± 0.08 |
. | Mean subtraction . | Variable smoothing . |
---|---|---|
τ0 | 0.0060 ± 0.0001 | 0.0034 ± 0.0001 |
α | 0.70 ± 0.01 | 0.88 ± 0.01 |
σ0 ( km s−1) | 250 | 250 |
x | 1.35 ± 0.06 | 0.46 ± 0.08 |
q | 0.65 ± 0.03 | 0.66 ± 0.03 |
We0( km s−1) | 6.27 ± 0.10 | 3.58 ± 0.08 |
. | Mean subtraction . | Variable smoothing . |
---|---|---|
τ0 | 0.0060 ± 0.0001 | 0.0034 ± 0.0001 |
α | 0.70 ± 0.01 | 0.88 ± 0.01 |
σ0 ( km s−1) | 250 | 250 |
x | 1.35 ± 0.06 | 0.46 ± 0.08 |
q | 0.65 ± 0.03 | 0.66 ± 0.03 |
We0( km s−1) | 6.27 ± 0.10 | 3.58 ± 0.08 |
. | Mean subtraction . | Variable smoothing . |
---|---|---|
τ0 | 0.0060 ± 0.0001 | 0.0034 ± 0.0001 |
α | 0.70 ± 0.01 | 0.88 ± 0.01 |
σ0 ( km s−1) | 250 | 250 |
x | 1.35 ± 0.06 | 0.46 ± 0.08 |
q | 0.65 ± 0.03 | 0.66 ± 0.03 |
We0( km s−1) | 6.27 ± 0.10 | 3.58 ± 0.08 |
The stacks in Figs 5–7 show the mean absorption profile of the Mg ii doublet line, clearly seen at the expected positions at small impact parameters. The amplitude of the random pixel-to-pixel variations outside of the central absorption feature is generally consistent with the computed bootstrap error bars. The expected doublet feature of the Mg ii line is generally resolved at rp ≲ 200 kpc, and is smoothed out at larger impact parameter by the velocity dispersion of the absorbers, which should increase linearly with rp in the limit of large radius because of Hubble expansion. The fact that our parameter x is close to unity supports this interpretation, although we note that the precise expected theoretical value of x in the linear regime is not one because of redshift distortions. We do not analyse this issue further in this paper because the maximum impact parameter that we analyse is not yet in the linear regime, and a more detailed model would be necessary for the velocity distribution of absorbers as a function of impact parameter. We mention here that we initially considered a simpler model with x = 0 and σ0 as free parameter, but this choice gave a substantially worse fit and resulted in a high value of the velocity dispersion because of its increase with radius. As mentioned previously, fits leaving both σ0 and x0 as free parameters lead to a substantial degeneracy and to solutions with very large values of σ0, driven by the excess of absorption that is seen in the last rp bin for the mean subtraction method. We have not found an explanation for this excess in the last bin, which is only marginally consistent (at the ∼3σ level, as shown in Fig. 8) with our fit.
A value q ≃ 0.65 is obtained for the line ratio of the Mg ii doublet, consistent with a mixture of saturated and unsaturated lines. It has been previously reported that the mean equivalent width of the Mg ii lines decreases with impact parameter (Gauthier et al. 2009, and references therein). This result may imply that absorbers are less saturated at larger impact parameters, and should therefore have a decreasing value of q, although this interpretation depends on whether the internal velocity dispersion of the absorbing clouds varies with impact parameter (note that this internal velocity dispersion is much smaller than the velocity dispersion of absorbing components around their host galaxies). Our model assumes a constant value of q for simplicity.
The mean equivalent widths obtained with our two methods, by directly integrating the effective optical depth in the stacked spectra as in equation (18), are shown in Fig. 8 as blue triangles for the mean subtraction method, and red squares for the variable smoothing method. These values and their bootstrap errors are also given in Table 2, together with the number of galaxy–quasar pairs that contribute to the stacked spectrum at each impact parameter bin. Note that this mean equivalent width is for the sum of the two lines in the Mg ii doublet. There is a systematic difference in the mean equivalent width obtained with the two methods; the variable smoothing method yields a systematically smaller equivalent width compared to the mean subtraction method, and the discrepancy increases with impact parameter, reaching more than a factor of 2 at rp = 10 Mpc. As mentioned previously in Section 3, the reason for this difference is that the spectral region where Mg ii absorption is expected is used to determine the continuum in the variable smoothing method. The presence of weak lines that remain undetected in individual spectra causes the continuum to be underestimated in a way that depends on the S/N and the equivalent width of the undetected line in a complex manner. This systematic underestimate of the continuum causes the underestimate of the mean equivalent width. Appendix A presents quantitative tests demonstrating the presence of this systematic error of the variable smoothing method, and shows also that the result obtained with the mean subtraction method, which does not use the stacked spectrum in the region of the Mg ii absorption to determine the continuum, is free of any similar systematic effect to the extent that we are able to discern.
rp . | Mean subtraction . | Variable smoothing . | Npairs . | ||
---|---|---|---|---|---|
. | 〈W〉 . | σ(〈W〉) . | 〈W〉 . | σ(〈W〉) . | . |
(kpc) . | (Å) . | (Å) . | (Å) . | (Å) . | . |
(0, 50] | 1.10 | 0.35 | 0.84 | 0.25 | 76 |
(50, 70.71] | 0.22 | 0.40 | 0.54 | 0.25 | 94 |
(70.71, 100] | 0.49 | 0.15 | 0.33 | 0.10 | 204 |
(100, 141.42] | 0.48 | 0.12 | 0.230 | 0.074 | 423 |
(141.42, 200] | 0.229 | 0.080 | 0.084 | 0.049 | 758 |
(200, 282.84] | 0.317 | 0.058 | 0.168 | 0.041 | 1396 |
(282.84, 400] | 0.181 | 0.076 | 0.102 | 0.042 | 2621 |
(400, 565.69] | 0.042 | 0.049 | 0.069 | 0.028 | 4904 |
(565.69, 800] | 0.081 | 0.029 | 0.069 | 0.019 | 9576 |
(800, 1131.37] | 0.040 | 0.018 | 0.006 | 0.012 | 19 166 |
(1131.37, 1600] | 0.032 | 0.015 | 0.015 | 0.010 | 38 922 |
(1600, 2262.74] | 0.0506 | 0.0093 | 0.0354 | 0.0068 | 75 567 |
(2262.74, 3200] | 0.0360 | 0.0072 | 0.0211 | 0.0051 | 148 769 |
(3200, 4525.48] | 0.0258 | 0.0062 | 0.0152 | 0.0038 | 290 340 |
(4525.48, 6400] | 0.0119 | 0.0044 | 0.0073 | 0.0028 | 559 840 |
(6400, 9050.97] | 0.0180 | 0.0036 | 0.0053 | 0.0022 | 1062 482 |
(9050.97, 12800] | 0.0169 | 0.0028 | 0.0041 | 0.0020 | 1961 450 |
rp . | Mean subtraction . | Variable smoothing . | Npairs . | ||
---|---|---|---|---|---|
. | 〈W〉 . | σ(〈W〉) . | 〈W〉 . | σ(〈W〉) . | . |
(kpc) . | (Å) . | (Å) . | (Å) . | (Å) . | . |
(0, 50] | 1.10 | 0.35 | 0.84 | 0.25 | 76 |
(50, 70.71] | 0.22 | 0.40 | 0.54 | 0.25 | 94 |
(70.71, 100] | 0.49 | 0.15 | 0.33 | 0.10 | 204 |
(100, 141.42] | 0.48 | 0.12 | 0.230 | 0.074 | 423 |
(141.42, 200] | 0.229 | 0.080 | 0.084 | 0.049 | 758 |
(200, 282.84] | 0.317 | 0.058 | 0.168 | 0.041 | 1396 |
(282.84, 400] | 0.181 | 0.076 | 0.102 | 0.042 | 2621 |
(400, 565.69] | 0.042 | 0.049 | 0.069 | 0.028 | 4904 |
(565.69, 800] | 0.081 | 0.029 | 0.069 | 0.019 | 9576 |
(800, 1131.37] | 0.040 | 0.018 | 0.006 | 0.012 | 19 166 |
(1131.37, 1600] | 0.032 | 0.015 | 0.015 | 0.010 | 38 922 |
(1600, 2262.74] | 0.0506 | 0.0093 | 0.0354 | 0.0068 | 75 567 |
(2262.74, 3200] | 0.0360 | 0.0072 | 0.0211 | 0.0051 | 148 769 |
(3200, 4525.48] | 0.0258 | 0.0062 | 0.0152 | 0.0038 | 290 340 |
(4525.48, 6400] | 0.0119 | 0.0044 | 0.0073 | 0.0028 | 559 840 |
(6400, 9050.97] | 0.0180 | 0.0036 | 0.0053 | 0.0022 | 1062 482 |
(9050.97, 12800] | 0.0169 | 0.0028 | 0.0041 | 0.0020 | 1961 450 |
rp . | Mean subtraction . | Variable smoothing . | Npairs . | ||
---|---|---|---|---|---|
. | 〈W〉 . | σ(〈W〉) . | 〈W〉 . | σ(〈W〉) . | . |
(kpc) . | (Å) . | (Å) . | (Å) . | (Å) . | . |
(0, 50] | 1.10 | 0.35 | 0.84 | 0.25 | 76 |
(50, 70.71] | 0.22 | 0.40 | 0.54 | 0.25 | 94 |
(70.71, 100] | 0.49 | 0.15 | 0.33 | 0.10 | 204 |
(100, 141.42] | 0.48 | 0.12 | 0.230 | 0.074 | 423 |
(141.42, 200] | 0.229 | 0.080 | 0.084 | 0.049 | 758 |
(200, 282.84] | 0.317 | 0.058 | 0.168 | 0.041 | 1396 |
(282.84, 400] | 0.181 | 0.076 | 0.102 | 0.042 | 2621 |
(400, 565.69] | 0.042 | 0.049 | 0.069 | 0.028 | 4904 |
(565.69, 800] | 0.081 | 0.029 | 0.069 | 0.019 | 9576 |
(800, 1131.37] | 0.040 | 0.018 | 0.006 | 0.012 | 19 166 |
(1131.37, 1600] | 0.032 | 0.015 | 0.015 | 0.010 | 38 922 |
(1600, 2262.74] | 0.0506 | 0.0093 | 0.0354 | 0.0068 | 75 567 |
(2262.74, 3200] | 0.0360 | 0.0072 | 0.0211 | 0.0051 | 148 769 |
(3200, 4525.48] | 0.0258 | 0.0062 | 0.0152 | 0.0038 | 290 340 |
(4525.48, 6400] | 0.0119 | 0.0044 | 0.0073 | 0.0028 | 559 840 |
(6400, 9050.97] | 0.0180 | 0.0036 | 0.0053 | 0.0022 | 1062 482 |
(9050.97, 12800] | 0.0169 | 0.0028 | 0.0041 | 0.0020 | 1961 450 |
rp . | Mean subtraction . | Variable smoothing . | Npairs . | ||
---|---|---|---|---|---|
. | 〈W〉 . | σ(〈W〉) . | 〈W〉 . | σ(〈W〉) . | . |
(kpc) . | (Å) . | (Å) . | (Å) . | (Å) . | . |
(0, 50] | 1.10 | 0.35 | 0.84 | 0.25 | 76 |
(50, 70.71] | 0.22 | 0.40 | 0.54 | 0.25 | 94 |
(70.71, 100] | 0.49 | 0.15 | 0.33 | 0.10 | 204 |
(100, 141.42] | 0.48 | 0.12 | 0.230 | 0.074 | 423 |
(141.42, 200] | 0.229 | 0.080 | 0.084 | 0.049 | 758 |
(200, 282.84] | 0.317 | 0.058 | 0.168 | 0.041 | 1396 |
(282.84, 400] | 0.181 | 0.076 | 0.102 | 0.042 | 2621 |
(400, 565.69] | 0.042 | 0.049 | 0.069 | 0.028 | 4904 |
(565.69, 800] | 0.081 | 0.029 | 0.069 | 0.019 | 9576 |
(800, 1131.37] | 0.040 | 0.018 | 0.006 | 0.012 | 19 166 |
(1131.37, 1600] | 0.032 | 0.015 | 0.015 | 0.010 | 38 922 |
(1600, 2262.74] | 0.0506 | 0.0093 | 0.0354 | 0.0068 | 75 567 |
(2262.74, 3200] | 0.0360 | 0.0072 | 0.0211 | 0.0051 | 148 769 |
(3200, 4525.48] | 0.0258 | 0.0062 | 0.0152 | 0.0038 | 290 340 |
(4525.48, 6400] | 0.0119 | 0.0044 | 0.0073 | 0.0028 | 559 840 |
(6400, 9050.97] | 0.0180 | 0.0036 | 0.0053 | 0.0022 | 1062 482 |
(9050.97, 12800] | 0.0169 | 0.0028 | 0.0041 | 0.0020 | 1961 450 |
The green circles with error bars in Fig. 8 show the results of Zhu et al. (2013), who have used a sample of galaxies and quasar spectra similar to ours to infer the same mean equivalent width as a function of impact parameter. Their result is systematically below ours, roughly by a factor of ∼2 at all impact parameters, and is lower even compared to our variable smoothing method. We believe the reason is again due to the systematic underestimate of the continuum. The continuum fitting method used by Zhu et al. (2013) also uses the observed spectra in the region where Mg ii absorption is expected in a rather complex way that is described in Zhu & Ménard (2013b), and the systematic error that this induces is difficult to predict but may in principle explain why it produces a systematically low estimate of the equivalent width. Note that in principle this underestimation will only affect the individually undetected systems. Individually undetected systems cannot be distinguished from the noise and will thus be fitted away by the continuum fitter. Individually detected systems will, in principle, not suffer from this effect. The error bars of Zhu et al. (2013) are also smaller than ours, since their continuum fitting can better remove any features of the quasar spectrum that are superposed with the Mg ii absorption lines, at the cost of introducing a systematic bias in the continuum estimate.
6 DISCUSSION
6.1 Relation of the mean equivalent width to the bias factor of Mg ii absorption systems
Our measurement of the cross-correlation of Mg ii absorption systems and galaxies in the CMASS catalogue of BOSS clearly reflects properties of the spatial distribution of these two objects. In the limit of large scales, when the fluctuations are in the linear regime, any population of objects that traces the large-scale mass perturbations is characterized by its bias factor and the autocorrelation in real space is equal to the correlation function of the mass times the square of the bias factor, with redshift distortions added in redshift space (Kaiser 1987; Cole & Kaiser 1989). The cross-correlation of two classes of objects is, in the same large-scale limit, equal to the mass correlation function times the product of the two bias factors. On small, non-linear scales, the correlations are more complex and they depend on other physics that determine the distribution of galaxies and Mg ii absorbers in relation to dark matter haloes.
Here, we shall make two approximations to physically interpret our measurement of We(rp): first, we neglect the effect of the finite integrating range ±2000 km s−1 that we have used, ignoring the difference from the true projected correlation that is obtained by integrating to infinity. This approximation is likely not very good for the largest impact parameters we use; we discuss this further below. Secondly, we assume that the cross-correlation of Mg ii systems and CMASS galaxies is the same as the autocorrelation of CMASS galaxies times the ratio of bias factors bMg/bg of the two types of objects. In other words, we assume the linear relation can be extended into the non-linear regime as far as the ratio of the cross-correlation to the autocorrelation is concerned.
This second assumption can be justified from observations of the correlations of galaxies of different luminosity. Zehavi et al. (2011) measured the projected correlation of galaxies in the DR7 catalogue in different luminosity ranges, and, to a good approximation, in the impact parameter range of our interest, the result is a fixed shape times the variable bias factor, as seen for example in their fig. 6. The shape of the galaxy correlation can be interpreted as arising from the correlation among virialized haloes and the distribution of galaxies within each halo (e.g. Zheng et al. 2005). This shape does vary slightly with luminosity, but the most important variation is the normalization determined by the bias factor. There is a greater variation of the shape of the projected correlation with galaxy colour (see fig. 21 in Zehavi et al. 2011). In addition, the projected cross-correlation of galaxies of different colour is not exactly equal to the geometric mean of the projected autocorrelations of the two types of galaxies (see their fig. 15). Our assumption can only be considered as a first approximation that will need to be tested in the future, but it allows us to obtain a bias factor for Mg ii absorption systems assuming that they behave in a similar way as galaxies in the CMASS catalogue.
6.2 Mean absorption from Mg ii systems
The value of τe0, representing the average absorption from the population of Mg ii absorbers, must be independently known before we can use the measured mean excess of Mg ii absorption around galaxies to infer the bias factor of Mg ii systems with equation (21). This parameter can be estimated from equation (4) using models of the equivalent width distribution that fit the observational data.
Unfortunately, the sample of absorbers of Nestor et al. (2005) is somewhat heterogeneous, and the main uncertainty we encounter in using it to compute τe0 is due to the redshift evolution. A fit to this evolution was determined by Nestor et al. (2005), where the parameters of the exponential model vary as W* ∝ (1 + z)0.634±0.097 and N* ∝ (1 + z)0.226 ± 0.170, both for the weak and strong populations. We infer from their model fits and the mean value of N* that the mean redshift of their sample is z ≃ 1.1 and we use these relations to convert the product N*W* to the mean redshift of the CMASS galaxy catalogue, z ≃ 0.55. We find |$N_{\rm str}^{*} W_{\rm str}^{*} = 0.55$| Å and |$N_{\rm wk}^{*} W_{\rm wk}^{*} = 0.095$| Å, with an error that is close to 10 per cent, although it is poorly defined because the errors in the redshift evolution of |$N_{\rm str,wk}^{*}$| and |$W_{\rm str,wk}^{*}$| should be correlated, and this information (and the exact redshift distribution of the absorbers) was not provided in Nestor et al. (2005).
6.3 Derivation of the bias factor of Mg ii systems
The galaxy bias factor in the model of Nuza et al. (2013) shown as the dashed black line is bg = 2.00 ± 0.07. Note that this value is lower than that obtained by Guo et al. (2013), bg = 2.16 ± 0.01, for the average CMASS galaxy. Using the value given by Guo et al. (2013) would lead to a larger measured value of the bias factor of the Mg ii systems. As explained in Guo et al. (2013), the value of the galaxy bias increases with luminosity and redshift, and it can also depend on the range of scales used to fit its value. Here, we use the galaxy bias value and the projected galaxy autocorrelation function of Nuza et al. (2013), but the discrepancy with the higher value obtained by Guo et al. (2013) needs to be resolved to remove this source of uncertainty on the derived bias value of the Mg ii absorption systems.
We find a huge difference for bMg for the different methods. Thus, we stress once again the importance of the quasar continuum estimate. Getting the estimate right is crucial for the measurement of the bias and failing to do so may lead to really different results.
Our measurement for the mean subtraction method is discrepant from the previously reported values by Gauthier et al. (2009) of bMg = 1.36 ± 0.38 and by Lundgren et al. (2009) of bMg = 1.10 ± 0.24. Our result is closer to the bias factor measured for the galaxies, implying that most of the Mg ii systems are associated with massive galaxies like the CMASS ones or even more massive. On the other hand, the measurement for the variable smoothing method is compatible with the previous ones. Finally, the measurement using Zhu et al. (2013) data points is also not compatible with the reported values but for the opposite reason. It is too low.
However, as we discussed in Section 5 and in Appendix A, both the variable smoothing method and the method used in Zhu et al. (2013) underestimate the observed mean equivalent width. We have presented proof that it is indeed true for the variable smoothing case. We also argued that this is also likely to be true for the method used in Zhu et al. (2013). This means that the ‘correct’ value should be the 2.33 ± 0.19 obtained for the mean subtraction method even though it is not compatible with the values reported in Gauthier et al. (2009) and Lundgren et al. (2009).
Note that our measurement of the bias factor remains subject to systematic uncertainties that will need to be improved: the determination of τe0, the use of a wider velocity interval for determining the quasar continuum and the mean Mg ii absorption compared to the ones used in this paper, and the use of a better modelling of the cross-correlation that includes redshift distortions in the regime of large impact parameters, and a more general density profile of Mg ii absorbers in haloes of different mass.
One possible reason for our high value of the Mg ii bias is the degeneracy between τe0 and the Mg ii bias. What we are actually fitting is the product of both. We can only recover the Mg ii bias once we fix the value of τe0. This means that an underestimation of τe0 will result in an overestimation of the Mg ii bias. Thus, a more robust measurement of τe0 is required. Another possible reason for our high value of the Mg ii bias is that the bias may decrease with the equivalent width of the Mg ii absorbers, as found both by Lundgren et al. (2009) and Gauthier et al. (2009). Our method includes all the Mg ii absorbers and measures their average bias, weighting each absorber by its equivalent width. This average bias would be larger than the one for strong, individually detected Mg ii lines if the weak absorbers are associated with massive halo environments, whereas absorbers of high equivalent width occur in galaxies hosted by low-mass haloes. Yet another possible explanation is our use of a limited velocity range for evaluating the projected cross-correlation of Mg ii absorption and galaxies. We note that the high value of the bias we obtain is driven by the last point (at largest impact parameter) in Fig. 10. This point might be too high because linear redshift distortions have increased the density of Mg ii absorbers in the interval used for integration, and decreased them in the interval used for continuum fitting. The projected cross-correlation should not be affected by these redshift distortions when it is computed by integrating over the whole line of sight, but at the largest impact parameters our integrating intervals are probably not large enough. This systematic effect can only be addressed by improving the continuum fitting method and the model of the cross-correlation in future work.
We now compare our results for the Mg ii–galaxy cross-correlation with those of Zhu et al. (2013). The modelling of Zhu et al. (2013) involves a free parameter, which they designate as |$f_{\mathrm{Mg\,\small {II}}}$|, that reflects the gas-to-mass ratio in haloes (ignoring the degree of saturation of the absorption lines), and they assume a fixed density profile for the absorbers in haloes. Zhu et al. (2013) do not relate this parameter to the mean absorption of the field population of Mg ii absorbers, so they fit the amplitude of the cross-correlation with this unconstrained, free parameter. They determine a characteristic host halo mass for the Mg ii absorbers of Mh ≃ 1013.5 M⊙ based on the presence of a feature in the shape of the cross-correlation at rp ∼ 1 Mpc that reflects a transition from the 1-halo term to the 2-halo term in their modelling. The weakness of this feature implies a poor determination of this characteristic halo mass (see the contours in their fig. 6, showing the large degeneracy with the |$f_{\mathrm{Mg\,\small {II}}}$| parameter). Their determination of this halo mass is therefore highly dependent on their model of the halo density profile, and does not generally match the total observed abundance of Mg ii absorbers. Moreover, the Mg ii absorbers are likely hosted in haloes with a very broad mass range, which should cause a smoothing of any feature due to the transition from the 1-halo to the 2-halo term. The specific density profile of absorbers they assume has not been tested and is not theoretically well motivated. Mg ii absorbers can be distributed in haloes differently from galaxies, depending on the physics of gas cooling and galactic winds in haloes. Autocorrelations and cross-correlations of galaxies of different types have been found to have widely different shapes (see e.g. figs 15 and 16 in Zehavi et al. 2011) which do not always possess the clear feature that is predicted for a tracer that follows the dark matter profile in haloes of a specific mass. Therefore, we think there is insufficient evidence for the presence of any feature in the Mg ii–galaxy cross-correlation that may be used to determine a characteristic host halo mass.
Instead, we propose that the amplitude of this cross-correlation should be related to the field population of Mg ii absorbers (e.g. through the effective optical depth τe0 that we have introduced), and can then be used to determine the mean bias factor |$b_{\mathrm{Mg\,\small {II}}}$|, which should be equal to the mean bias factor of the host haloes of the absorbers (weighted by their rest-frame equivalent width), and is robustly defined even if the range of host halo masses is very broad.
6.4 The ratio of Mg ii-absorbing gas to the total mass
Measurements of the average Mg ii absorption around galaxies can be compared with mass measurements averaged in the same way obtained from weak gravitational lensing. This comparison was done in Zhu et al. (2013) to obtain an estimate for the ratio of gas mass to total mass in the haloes around the CMASS galaxies of the BOSS survey. We now examine this question to point out a number of uncertainties in this derivation.
Therefore, the fraction of baryons in the Mg ii clouds can be a small one even if the mean metallicity is relatively low. However, the mean saturation parameter |$\bar{S}$| is likely much larger than unity, so it is possible that the Mg ii absorbers account for an important fraction of the baryons in galactic haloes, and for the accreting material that fuels the star formation rate. We note that any further comparison of the detailed radial profiles of We(rp) and wgg(rp) cannot be reliably used to infer a profile of the gas-to-mass ratio, because ZMg is likely to vary with rp, since the heavy elements must have originated from galactic winds, and the values of |$\bar{S}$|, |$x_{\mathrm{Mg\,\small {II}}}$| and gMg may also vary substantially with rp. The mean value of the gas-to-mass ratio is still highly uncertain because of the unknown value of |$\bar{S}/(x_{\mathrm{Mg\,\small {II}}}\, g_{\mathrm{Mg}}\, Z_{\mathrm{Mg}})$|.
7 SUMMARY AND CONCLUSIONS
In this paper, we have used the Mg ii line to measure the cross-correlation of Mg ii absorption and galaxies in BOSS. The large size of the samples we use (SDSS DR7 quasar catalogue as background sample and DR11 CMASS galaxy catalogue as foreground sample) enables a statistical approach to detect Mg ii absorption that is too weak to be detected individually and would otherwise be missed. We present a method to estimate the quasar continuum designed for this type of measurements and compare our results with those obtained by a more typical continuum estimate. Our main results can be summarized as follows.
The method to fit the quasar continuum is crucial to measure the mean Mg ii equivalent width as a function of impact parameter. Methods that use the observed flux in the spectral region near the Mg ii line wavelength at the galaxy redshift to determine the continuum suffer from a systematic bias, because the absorption from individually undetected systems inevitably lowers the continuum estimate and causes an underestimate of the mean absorption. The tests presented in Appendix A show that our mean subtraction method does not suffer from any systematic effect to the extent that we are able to discern.
We find that the cross-correlation of Mg ii absorption and CMASS galaxies follows the shape of the CMASS galaxies autocorrelation at large scales. We use the CMASS autocorrelation model from Nuza et al. (2013) and the measured galaxy bias factor to derive a bias factor of Mg ii absorbers of bMg = 2.33 ± 0.19. This value is substantially larger than the previous measurements by Gauthier et al. (2009) and Lundgren et al. (2009). This discrepancy may be due to a real difference, because our measurement includes a contribution from weak Mg ii absorption systems which may be more strongly clustered than strong absorbers, and may also be affected by our imperfect determination of the projected cross-correlation at large impact parameters owing to our limited integrating range. More accurate measurements and better modelling will be necessary to clarify this question.
Funding for SDSS-III has been provided by the Alfred P. Sloan Foundation, the Participating Institutions, the National Science Foundation, and the US Department of Energy Office of Science. The SDSS-III website is http://www.sdss3.org/. IP-R and JM-E have been supported in part by Spanish grants AYA2009-09745 and AYA2012-33938.
SDSS-III is managed by the Astrophysical Research Consortium for the Participating Institutions of the SDSS-III Collaboration including the University of Arizona, the Brazilian Participation Group, Brookhaven National Laboratory, University of Cambridge, Carnegie Mellon University, University of Florida, the French Participation Group, the German Participation Group, Harvard University, the Instituto de Astrofisica de Canarias, the Michigan State/Notre Dame/JINA Participation Group, Johns Hopkins University, Lawrence Berkeley National Laboratory, Max Planck Institute for Astrophysics, Max Planck Institute for Extraterrestrial Physics, New Mexico State University, New York University, Ohio State University, Pennsylvania State University, University of Portsmouth, Princeton University, the Spanish Participation Group, University of Tokyo, University of Utah, Vanderbilt University, University of Virginia, University of Washington, and Yale University.
REFERENCES
APPENDIX A: TESTS OF THE CONTINUUM FITTING METHODS
The method to fit the quasar continuum is a crucial part of the measurement of the mean Mg ii absorption equivalent width as a function of impact parameter from a galaxy, Wτ(b), presented in this paper. The two methods we have used produce a different result, which is also different from the result reported by Zhu et al. (2013). It is therefore important to perform tests on these methods that can reveal the presence of systematic errors in the Wτ(b) estimates. This appendix presents the results of three tests. The first one (Section A1) checks for any systematic mean absorption that might be artificially introduced by the continuum fitting method when there is no correlation between Mg ii absorbers and galaxies. The second one (Section A2) verifies that the correct equivalent width of an individually detected Mg ii absorption system in a spectrum is correctly recovered. Finally, Appendix A3 reveals the effect on the fitted continuum of the presence of weak absorbers that are individually undetected, and the way these absorbers can bias the estimate of the mean equivalent width.
A1 Systematic errors in the absence of correlations
One might suspect that a small average absorption (either positive or negative) is artificially introduced by the method to fit the continuum, even when the regions selected to search for absorbers are completely random and should therefore have no average absorption. This might happen if the quasar continuum is systematically overestimated or underestimated, depending in a complex manner on the varying noise properties and the shape of the true quasar continuum. To test for this possibility, we have remeasured the mean Mg ii equivalent widths after rotating the right ascension coordinate of all the quasars by 5°and 10°, in the two possible directions, and after increasing and decreasing the redshift of the galaxies by 0.05. These separations are large enough to make any residual cross-correlation of galaxies and Mg ii absorbers completely negligible, so the measured correlation should be consistent with zero. Note that this procedure ensures that the autocorrelations that are present among the Mg ii absorbers, quasars and galaxies are preserved, so that their contribution to the measurement errors of the cross-correlation is the same.
The result of this test is shown in Fig. A1, in the left-hand panel for the mean subtraction method and the right-hand panel for the variable smoothing method. The real data set is shown as big red circles with error bars, after dividing by the best-fitting power-law model that is described in Section 4 and plotted in Fig. 8. The average of six mock data sets are shown also after dividing by the same model as blue stars. In the absence of any systematics, the mean absorption in the mock data sets is expected to be zero, whereas the real data should produce a ratio to the best-fitting model that is consistent with 1. The results do not show any systematic errors for the mean subtraction method. There appears to be a small negative systematic absorption that is introduced by the variable smoothing method, as indicated by the negative values of the mock sample in the right-hand panel, at large impact parameters (where the mean equivalent width can be measured with the smallest error bar). This average negative absorption is approximately equal to the best-fitting model prediction at ∼10 Mpc, or ∼0.3 km s−1 (see Fig. 8). This result may be due to some subtle effect in the variable smoothing method that introduces a small bias by systematically underestimating the continuum in the absence of real absorption lines, possibly due to occasional false identifications of noise spikes as real absorbers. As we shall see below, the variable smoothing method is actually affected by a more serious systematic error that partially eliminates the contribution of weak absorption systems to the mean equivalent width.
A2 Tests of the equivalent width measurement for individually detected systems
We now test that the mean equivalent width measured for absorbing systems that are individually clearly detected above the noise agrees with other well-established methods. For this purpose, we use the Mg ii absorber catalogue of Zhu & Ménard (2013b), which contains 35 752 absorption systems from the SDSS DR7 quasar spectra sample. The integrated equivalent widths we obtain for systems in this catalogue, using our two methods of mean subtraction and variable smoothing, are compared with the equivalent widths provided in the catalogue in Fig. A2. There is a large scatter in the equivalent widths obtained with different methods. This result is not surprising, because the noise can change the determination of the continuum in random ways in different methods. In particular, in the method of the mean subtraction, the equivalent width is obtained by integrating the absorbed fraction over a wide interval around the absorber, according to equation (18), adding noise to the estimate. However, the average of the equivalent width estimator in our mean subtraction method, shown by the black points in Fig. A2 (with an rms dispersion indicated by the error bars), agrees very well with the equivalent width provided by the Zhu & Ménard (2013b) catalogue. The variable smoothing method apparently suffers from a bias causing a 10 to 20 per cent increase of the average of the equivalent width (see the black points in middle panel of Fig. A2), which may be due to a tendency of this method to overestimate the continuum level around detected absorption lines.
A3 Impact of individually undetected systems on the mean equivalent width
We now test how the presence of weak absorption systems that cannot be individually detected in a single spectrum but contribute to the mean equivalent width as a function of impact parameter from a galaxy can bias the estimate of the quasar continuum in the different methods we use. For this purpose, artificial absorbers are introduced in a spectrum, and then we refit the continuum and measure the change in the measured equivalent width.
The change in equivalent width caused by the insertion of an absorber, ΔW = W ′ − W, is plotted in Fig. A3 as a function of the equivalent width Wi of the inserted absorber, obtained by integrating 1 − exp[−τ(v)] over the same velocity interval that is used for determining W and W ′ (Wi is nearly equal to W0 in equation (A1), except that the integrating interval does not extend to infinity). The different lines correspond to different values of the absorber velocity dispersion, σ. The solid blue lines represent the mean subtraction method, and they coincide precisely with ΔW = Wi for all values of σ. The result, as expected, is that the continuum determined by this method is unaffected by the presence of the absorbers that have narrow widths compared to the chosen integrating interval width of 4000 km s−1. The reason is that, in the mean subtraction method, the continuum c′(v) is determined using only the measured flux outside of this interval.
On the other hand, the variable smoothing method (dashed red lines in Fig. A3) is strongly biased to lowering the estimated continuum in response to the presence of a weak absorption system. The result is that the change caused by the absorber in the estimated equivalent width, ΔW, can be much less than the true value, and the difference is a complex function of the equivalent width W0, the velocity dispersion and the S/N of the spectrum. The underestimate of the continuum level is naturally smaller for narrower lines (lower σ), because the lines are detected and eliminated from the continuum estimation for lower values of W0.
To summarize, the three tests of our continuum fitting methods presented in this appendix demonstrate that the variable smoothing method suffers from several systematic errors. The first test shows that a small negative absorption, of equivalent width ∼− 0.3 km s−1, is induced where there is none. The second test indicates that the equivalent width of strong, detected systems is overestimated by 10–20 per cent. Finally, the third test shows that for weak systems, the continuum is systematically underestimated, thereby strongly reducing the contribution of these systems to the measured equivalent width. However, the mean subtraction method successfully passes all these tests and should therefore provide a reliable estimate of the stacked equivalent width as a function of impact parameter.