ABSTRACT
We present ∼kiloparsec spatial resolution maps of the CO-to-H2 conversion factor (αCO) and dust-to-gas ratio (DGR) in 26 nearby, star-forming galaxies. We have simultaneously solved for αCO and the DGR by assuming that the DGR is approximately constant on kiloparsec scales. With this assumption, we can combine maps of dust mass surface density, CO-integrated intensity, and H i column density to solve for both αCO and the DGR with no assumptions about their value or dependence on metallicity or other parameters. Such a study has just become possible with the availability of high-resolution far-IR maps from the Herschel key program KINGFISH, 12CO J = (2–1) maps from the IRAM 30 m large program HERACLES, and H i 21 cm line maps from THINGS. We use a fixed ratio between the (2–1) and (1–0) lines to present our αCO results on the more typically used 12CO J = (1–0) scale and show using literature measurements that variations in the line ratio do not affect our results. In total, we derive 782 individual solutions for αCO and the DGR. On average, αCO = 3.1 M☉ pc−2 (K km s−1)−1 for our sample with a standard deviation of 0.3 dex. Within galaxies, we observe a generally flat profile of αCO as a function of galactocentric radius. However, most galaxies exhibit a lower αCO value in the central kiloparsec—a factor of ∼2 below the galaxy mean, on average. In some cases, the central αCO value can be factors of 5–10 below the standard Milky Way (MW) value of αCO, MW = 4.4 M☉ pc−2 (K km s−1)−1. While for αCO we find only weak correlations with metallicity, the DGR is well-correlated with metallicity, with an approximately linear slope. Finally, we present several recommendations for choosing an appropriate αCO for studies of nearby galaxies.
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1. INTRODUCTION
The H2 molecule is difficult to observe in the prevalent interstellar medium (ISM) conditions of a normal star-forming galaxy. Since H2 is the primary constituent of molecular gas, inferring its mass is crucial for studying this phase of the ISM and the star formation that occurs within it. A widespread practice is to use the second most abundant molecule, carbon monoxide (12CO), as a tracer and convert the measured CO integrated intensities into H2 column densities using a "CO-to-H2" conversion factor XCO33:
In mass surface density units, this equation can be rewritten as:
where is the total mass surface density of molecular gas (including a correction for the second most abundant element, He). A variety of observations have shown that αCO ≈ 4.4 M☉ pc−2 (K km s−1)−1 is characteristic of the local area of the Milky Way (MW; Solomon et al. 1987; Strong & Mattox 1996; Abdo et al. 2010). Despite uncertainties in the physics behind the conversion factor, the observability of CO ensures that it will remain a widely used molecular gas tracer, particularly at high redshift.
αCO is used in a variety of contexts in Galactic and extragalactic studies. In the following, we define and measure αCO on ∼kiloparsec scales in nearby galaxies. At these resolutions, the small-scale structure of the ISM is averaged out and the variation in αCO is driven by large-scale changes in the galactic environment (e.g., metallicity, galactic dynamics, ISM pressure). In general, extragalactic studies have adopted a single value of αCO for entire galaxies. The new ability to perform systematic studies of αCO on sub-galactic scales in nearby galaxies facilitated by high angular resolution maps of gas and dust will let us move beyond this simplistic assumption.
In addition, studying αCO on ∼kiloparsec scales has several advantages: (1) because we do not resolve molecular clouds, we avoid issues with sampling the cloud structure (e.g., envelopes of CO-free H2); (2) because our resolution element contains many clouds, we average over cloud evolutionary effects; and (3) we cover large enough fractions of the total molecular gas mass in a galaxy that it becomes reasonable to generalize our results to determine αCO values appropriate for integrated galaxy measurements. It is important to note that our definition of αCO is distinct from the line-of-sight /ICO one can measure in small regions of Galactic molecular clouds—in such cases the conversion factor is not well defined since it does not sample the full structure of the cloud.
In order to measure the conversion factor, one must measure (or equivalently, ) independently of CO and then compare it to observed CO integrated intensities. This measurement has been accomplished using a variety of techniques, including: measuring total gas masses from γ-ray emission plus a model for the cosmic ray distribution (Strong & Mattox 1996; Abdo et al. 2010), using the observed velocity dispersion and size of the molecular cloud to obtain virial masses (Solomon et al. 1987; Wilson 1995; Bolatto et al. 2008; Donovan Meyer et al. 2012; Wei et al. 2012; Gratier et al. 2012), and modeling multiple molecular gas lines with varying optical depths and critical densities (e.g., Weiß et al. 2001; Israel 2009a, 2009b). In general, few of these techniques are effective for constraining αCO in galaxies outside the Local Group due to the difficulty of obtaining the necessary observations (i.e., γ-ray maps or CO mapping at <100 pc resolution) or doubts about fundamental assumptions (e.g., that CO traces the full extent of molecular gas in the clouds; that the clouds lack contributions to virial balance from magnetic or pressure forces; that simple radiative transfer models can reproduce molecular gas excitation on kiloparsec scales).
Another possible technique to measure is to use dust as a tracer of the total gas column. Assuming that dust and gas are well mixed, the dust-to-gas ratio (DGR) is not a function of atomic/molecular phase, and the fraction of mass in ionized gas is negligible, the observed dust mass surface density can be converted to a gas mass surface density with information on the DGR, i.e., using the following equation:
Here, ΣD is the mass surface density of dust and and are the mass surface densities of atomic and molecular gas,34 respectively, and DGR is the dust-to-gas mass ratio. By measuring ΣD and and assuming the DGR (or simultaneously measuring it, as we will discuss shortly), the molecular gas mass can be determined. While still subject to its own systematic uncertainties (discussed in detail in Section 3.4), this technique relies on a different set of assumptions than those techniques mentioned previously.
Studies of the DGR or αCO have typically fixed one of the parameters in order to determine the other, so it is difficult to avoid circularity when using a fixed DGR to solve for αCO in Equation (3). Alternatively, with sufficiently high spatial resolution, the DGR can be determined along sight-lines free of molecular gas and extrapolated to regions where CO is detected. For very nearby galaxies like the Magellanic Clouds, such a technique has been used by Israel (1997) and Leroy et al. (2009a), who found that αCO determinations from virial masses can be strongly biased by envelopes of "CO-dark" molecular gas in low-metallicity systems. In more distant galaxies, we generally cannot isolate purely atomic lines of sight at the resolution of typical H i and CO observations. Instead, it is possible to use a technique developed by Leroy et al. (2011) to simultaneously measure αCO and the DGR using the assumption that the DGR should be constant over a region of a galaxy. Since we can now achieve ∼kiloparsec spatial resolution in the far-infrared (far-IR) with Herschel and have sensitive, high-resolution CO and H i maps, it is possible to extend this technique, which has thus far only been applied to the Local Group, to more distant galaxies.
The idea behind this technique (explained in detail in Section 3) is that spatially resolved measurements of ΣD, , and ICO allow one to solve for αCO and the DGR over regions smaller than the typical scale over which the DGR varies (i.e., one region is well represented by a single DGR value) and it covers a range of CO/H i ratios. Having chosen an appropriately sized region, we can determine these two constants, defining the best fit as that which produces the most uniform DGR for the multiple lines-of-sight included in the region. This technique assumes no prior value of the DGR or αCO—it makes use of the linear (by definition) dependence of on αCO to identify the solution. The technique is therefore only applicable in regions where CO is detected. Constraining αCO in more extreme conditions would require different techniques (see Schruba et al. 2012 for a more thorough discussion).
One useful aspect of solving simultaneously for αCO and the DGR is that the absolute normalization of the dust tracer is irrelevant for the determination of αCO as long as it is linear with the "true" ΣD. Since the DGR is calibrated from the map itself, any constant term will show up in both the DGR and ΣD and therefore has no impact on the assessment of . For example, Leroy et al. (2011) showed that the dust optical depth at 160 μm, determined using an assumed power-law dependence on frequency and an estimate of the dust temperature from the 70 μm/160 μm ratio, works comparably well as the dust mass surface density. Dobashi et al. (2008) performed a similar study in the Large Magellanic Cloud using AV mapping to trace dust mass surface density. Since we are also interested in the value of the DGR itself, we use ΣD as our tracer throughout this paper. We note that uncertainties in the absolute value of ΣD, as long as they do not introduce a nonlinearity within the region in question, will not affect the determination of αCO.
For this study, we make use of CO J = (2–1) observations from the large program HERA CO Line Emission Survey (HERACLES) on the IRAM 30 m telescope (Leroy et al. 2009b). It is important to note that we are therefore determining αCO appropriate for that CO line. Since most studies quote αCO for the CO J = (1–0) line, throughout the paper we use a line ratio (R21) to convert our measurements to the (1–0) scale. Systematic variations in R21 will result in errors in the (1–0) conversion factor, but the (2–1) conversion factor will not be affected since it is what we are directly deriving. Although it is convenient to discuss αCO in its typical (1–0) incarnation, we note that the (2–1) conversion factor itself will be important for future studies with the Atacama Large Millimeter Array (ALMA). For nearby galaxies, at a given angular resolution, mapping in the (2–1) line is more efficient than in the (1–0) line. For high-redshift galaxies, the (1–0) line may be shifted out of ALMA's frequency coverage. Thus, αCO for the (2–1) line will be useful regardless of its relationship to the (1–0) line.
This paper is laid out as follows. Section 2 presents the details of the resolved dust and gas observations we use. In Section 3, we describe the technique to simultaneously measure the DGR and αCO and discuss how the procedure is optimized to deal with more distant galaxies than those in the Local Group (more details on the technique can be found in Appendix A). We present the results of performing the solution on 26 nearby galaxies in Section 4 and discuss their implications for our understanding of how the DGR and αCO vary with metallicity and other ISM properties in Section 6.
2. OBSERVATIONS
We make use of observations of dust and gas from a series of surveys of nearby galaxies built upon the "Spitzer Infrared Nearby Galaxies Survey" (SINGS; Kennicutt et al. 2003). These observations include H i from "The H i Nearby Galaxies Survey" (THINGS; Walter et al. 2008), 12CO J = (2–1) from HERACLES (Leroy et al. 2009b, 2013), and far-IR dust emission from "Key Insights into Nearby Galaxies: A Far-Infrared Survey with Herschel" (KINGFISH; Kennicutt et al. 2011). In addition, several galaxies that were not included in THINGS have H i observations from either archival or new observations. The sample of galaxies in common among these surveys and for which we have detections of CO emission (see Schruba et al. 2012 for details on the HERACLES non-detections) consists of the 26 targets listed in Table 1.
Table 1. Galaxy Sample
Galaxy | R.A. | Decl. | Distance | i | P.A. | Morphology | R25 | Solution Pixela |
---|---|---|---|---|---|---|---|---|
(J2000) | (J2000) | (Mpc) | (°) | (°) | (') | Radius (kpc) | ||
NGC 0337 | −07°34'410 | 19.3 | 51 | 90 | SBd | 1.5 | 3.5 | |
NGC 0628 | +15°47'000 | 7.2 | 7 | 20 | SAc | 4.9 | 1.3 | |
NGC 0925 | +33°34'435 | 9.1 | 66 | 287 | SABd | 5.4 | 1.7 | |
NGC 2841 | +50°58'352 | 14.1 | 74 | 153 | SAb | 3.5 | 2.6 | |
NGC 2976 | +67°55'000 | 3.6 | 65 | 335 | SAc | 3.6 | 0.6 | |
NGC 3077 | +68°44'020 | 3.8 | 46 | 45 | I0pec | 2.7 | 0.7 | |
NGC 3184* | +41°25'280 | 11.7 | 16 | 179 | SABcd | 3.7 | 2.1 | |
NGC 3198 | +45°32'589 | 14.1 | 72 | 215 | SBc | 3.2 | 2.6 | |
NGC 3351* | +11°42'140 | 9.3 | 41 | 192 | SBb | 3.6 | 1.7 | |
NGC 3521* | −00°02'092 | 11.2 | 73 | 340 | SABbc | 4.2 | 2.0 | |
NGC 3627* | +12°59'296 | 9.4 | 62 | 173 | SABb | 5.1 | 1.7 | |
NGC 3938 | +44°07'149 | 17.9 | 14 | 195 | SAc | 1.8 | 3.3 | |
NGC 4236 | +69°27'450 | 4.5 | 75 | 162 | SBdm | 12.0 | 0.8 | |
NGC 4254* | +14°24'590 | 14.4 | 32 | 55 | SAc | 2.5 | 2.6 | |
NGC 4321* | +15°49'210 | 14.3 | 30 | 153 | SABbc | 3.0 | 2.6 | |
NGC 4536* | +02°11'160 | 14.5 | 59 | 299 | SABbc | 3.5 | 2.6 | |
NGC 4569* | +13°09'460 | 9.9 | 66 | 23 | SABab | 4.6 | 1.8 | |
NGC 4625 | +41°16'260 | 9.3 | 47 | 330 | SABmp | 0.7 | 1.7 | |
NGC 4631 | +32°32'290 | 7.6 | 85 | 86 | SBd | 7.3 | 1.4 | |
NGC 4725 | +25°30'030 | 11.9 | 54 | 36 | SABab | 4.9 | 2.2 | |
NGC 4736* | +41°07'132 | 4.7 | 41 | 296 | SAab | 3.9 | 0.8 | |
NGC 5055* | +42°01'453 | 7.9 | 59 | 102 | SAbc | 5.9 | 1.4 | |
NGC 5457b* | +54°20'570 | 6.7 | 18 | 39 | SABcd | 12.0 | 1.2 | |
NGC 5713 | −00°17'210 | 21.4 | 48 | 11 | SABbcp | 1.2 | 3.9 | |
NGC 6946* | +60°09'144 | 6.8 | 33 | 243 | SABcd | 5.7 | 1.2 | |
NGC 7331 | +34°24'565 | 14.5 | 76 | 168 | SAb | 4.6 | 2.6 |
Notes. Distances and morphologies from the compilation of Kennicutt et al. (2011). Orientation parameters are from Walter et al. (2008) where possible, and are otherwise from the LEDA and NED databases. aSolution pixels are defined in Section 3. They are the regions in which we solve for αCO and the DGR. bM101. *CO J = (1–0) maps available from the Nobeyama survey of nearby galaxies (Kuno et al. 2007).
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The SINGS and KINGFISH surveys targeted galaxies with a variety of morphologies, located within 30 Mpc of the Milky Way. Due to the requirement of a CO detection for our work, all but one of the viable targets are spiral galaxies, the exception being NGC 3077, which is a starbursting dwarf. In Table 1, we list the positions, distances, orientation parameters, and the B-band isophotal radii at 25 mag arcsec−2 (R25) for our targets. Throughout the text, we define r25 = r/R25, where r is the galactocentric radius in units of arcminutes.
2.1. Dust Mass Surface Density
We use dust mass surface density maps derived from pixel-by-pixel modeling of the infrared (IR) spectral energy distribution (SED) observed by Spitzer and Herschel with models developed by Draine & Li (2007). A detailed description of the modeling for NGC 0628 and NGC 6946 is presented in Aniano et al. (2012) and the full-sample results are presented in G. Aniano et al. (in preparation). The dust models include a description of the dust properties (size distribution, composition, and optical properties of the grains) with a variable fraction of dust in the form of polycyclic aromatic hydrocarbons (PAHs). The dust is illuminated by a radiation field distribution wherein a fraction of the dust is heated by a minimum radiation field Umin while the rest is heated by a power-law distribution of radiation fields extending up to U = 107 UMMP, where UMMP is the solar neighborhood radiation field from Mathis et al. (1983). The fraction of the dust mass heated by radiation fields where U > 102 UMMP is typically very small, so the dust mass surface density is not very sensitive to the exact value of the upper limit on U.
The resolution of the dust mass surface density map is equivalent to that of the lowest resolution IR map included in the modeling. In order to preserve spatial resolution while still covering the peak of the dust SED, we use the dust modeling at a resolution matched to the SPIRE 350 μm map (FWHM ∼ 25''). This limiting resolution allows us to include the following maps in the dust modeling: IRAC 3.6, 4.5, 5.8, and 8.0 μm; MIPS 24 and 70 μm; PACS 70, 100, and 160 μm; and SPIRE 250 and 350 μm. In theory, we could perform this analysis at even higher resolution using the SPIRE 250 resolution maps, which include all IRAC bands; MIPS 24 μm; all PACS bands; and SPIRE 250 μm. However, Aniano et al. (2012) found that maps where the limiting resolution exceeds MIPS 70 μm are less reliable due to the comparatively low surface brightness sensitivity of the PACS observations. At SPIRE 250 μm resolution, they find systematic errors of up to ∼30%–40% in the dust mass (compared to their best estimate, which includes all IRAC, MIPS, PACS, and SPIRE bands). However, when both SPIRE 250 μm and 350 μm observations are included, the systematic errors in the dust mass are ∼10% or less. We proceed by using the SPIRE 350 μm resolution dust modeling results.
Aside from the dust mass surface density, the Aniano et al. (2012) modeling also constrains a number of other quantities that we make use of later in interpreting the results. These quantities include , the average radiation field heating the dust; Umin, the minimum radiation field; fPDR, the fraction of the dust luminosity that comes from dust heated by U > 100 UMMP; and qPAH, the fraction of the dust mass accounted for by PAHs with fewer than 103 carbon atoms.
Statistical uncertainties on ΣD and the other derived parameters were measured by Aniano et al. (2012) with a Monte Carlo approach. In most of the regions we consider, the statistical uncertainties on the dust mass surface densities are small, but the signal-to-noise ratio (S/N) of the dust mass maps is generally a function of radius and the outskirts can have S/N ∼ 5 in some cases. Our error estimates take these uncertainties into account and are described in Section 3.3. Possible systematic effects are discussed in Section 3.5.
2.2. H i Surface Density
To trace the atomic gas surface density in our targets, we use a combination of NRAO35 Very Large Array (VLA) H i observations from THINGS (Walter et al. 2008) and supplementary H i, observations both new and archival, described in Leroy et al. (2013). The source and angular resolution of the H i maps for our targets are listed in Table 2.
Table 2. H i Observation Summary
Galaxy | Source | FWHM Beam Properties | ||
---|---|---|---|---|
Major ('') | Minor ('') | P.A. (°) | ||
NGC 0337 | Archival | 20.2 | 13.0 | 160.3 |
NGC 0628 | THINGS | 11.9 | 9.3 | −70.3 |
NGC 0925 | THINGS | 5.9 | 5.7 | 30.6 |
NGC 2841 | THINGS | 11.1 | 9.4 | −12.3 |
NGC 2976 | THINGS | 7.4 | 6.4 | 71.8 |
NGC 3077 | THINGS | 14.3 | 13.2 | 60.5 |
NGC 3184 | THINGS | 7.5 | 6.9 | 85.4 |
NGC 3198 | THINGS | 11.4 | 9.4 | −80.4 |
NGC 3351 | THINGS | 9.9 | 7.1 | 24.1 |
NGC 3521 | THINGS | 14.1 | 11.2 | −61.7 |
NGC 3938 | Archival | 18.5 | 18.2 | 48.6 |
NGC 3627 | THINGS | 10.0 | 8.9 | −60.9 |
NGC 4236 | New | 16.7 | 13.9 | 69.6 |
NGC 4254 | Archival | 16.9 | 16.2 | 54.4 |
NGC 4321 | Archival | 14.7 | 14.1 | 163.4 |
NGC 4536 | Archival, New | 14.7 | 13.8 | −11.4 |
NGC 4569 | Archival | 14.2 | 13.9 | 32.9 |
NGC 4625 | Archival | 13.0 | 12.5 | −29.2 |
NGC 4631 | Archival | 14.9 | 13.3 | 178.1 |
NGC 4725 | Archival, New | 18.6 | 17.0 | −20.9 |
NGC 4736 | THINGS | 10.2 | 9.1 | −23.0 |
NGC 5055 | THINGS | 10.1 | 8.7 | −40.0 |
NGC 5457 | THINGS | 10.8 | 10.2 | −67.1 |
NGC 5713 | Archival | 15.5 | 14.9 | 121.9 |
NGC 6946 | THINGS | 6.0 | 5.6 | 6.6 |
NGC 7331 | THINGS | 6.1 | 5.6 | 34.3 |
Note. Galaxies with new H i data were observed in VLA project AL735 (PI: A. Leroy).
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The H i maps were converted from integrated intensities to column densities using Equation (5) of Walter et al. (2008). We convolved each map with an elliptical Gaussian kernel determined by its individual beam properties to produce a circular Gaussian point spread function (PSF). We then use kernels created following the procedures in Aniano et al. (2011) to convolve the circular Gaussian to match the SPIRE PSF at 350 μm. For the H i, we assume the uncertainties to be the larger of either 0.5 M☉ pc−2 or 10% of the measured column density. Systematic uncertainties from H i opacity effects are discussed in Section 3.4.
2.3. CO Integrated Intensity
To trace the molecular gas distribution in our targets, we use CO J = (2–1) mapping from the HERACLES survey (Leroy et al. 2009b). Integrated intensity maps were generated from the CO spectral cubes by integrating the spectra over a range in velocity around either (1) the detected CO line in that spectrum or (2) the expected CO velocity predicted from the H i velocity (since H i is detected at high S/N in almost all relevant pixels). We propagate uncertainties through these masking steps, creating in the end an integrated CO line map and an uncertainty map. The HERACLES maps have PSFs well approximated by a circular Gaussian with a FWHM of 134. We convolve the maps with kernels constructed using the techniques described by Aniano et al. (2011) to match the resolution of the SPIRE 350 μm maps. We have tested the effect of error beams (i.e., the extended wings of the PSF or stray light pick-up of the IRAM 30 m telescope) on the HERACLES maps and find that the effect is less than ∼5% for all galaxies and closer to 1% for most.
Our measurements of αCO directly determine the conversion factor appropriate for CO J = (2–1). However, to compare with the standard CO J = (1–0) factor, which is more frequently used, we convert to (1–0) using a fixed value of the line ratio R21 = (2–1)/(1–0) = 0.7. Due to revised telescope efficiencies, the R21 we use differs slightly from that used in Leroy et al. (2009b). The R21 we assume was found to be an appropriate average for the HERACLES sample (E. W. Rosolowsky et al., in preparation; note that we find good agreement with this R21 by comparing the HERACLES measurements with published CO J = (1–0) measurements as described in the Appendix). We discuss the effects of assuming a fixed R21 on our results for the (1–0) conversion factor in Section 3.4. In order to use the αCO values with CO J = (2–1) observations, they should be divided by a factor of 0.7.
2.4. Ancillary Datasets
2.4.1. Metallicity
In the analysis presented in Section 4, we study the variations of αCO and the DGR as a function of metallicity. Wherever possible, we make use of the metallicity measurements from Moustakas et al. (2010, hereafter M10), who derived characteristic metallicities as well as radial gradients in oxygen abundance for the SINGS sample. M10 present results using two different calibrations for the strong-line abundances—from Kobulnicky & Kewley (2004, KK04) and Pilyugin & Thuan (2005, PT05). Both calibrations are considered in the following analysis.
Our preferred metallicity measurement is a radial gradient from H ii region metallicities (M10, Table 8). For several galaxies, no radial gradient measurement is available, so we use a fixed metallicity for the entire galaxy equal to the "characteristic metallicity" (M10, Table 9). In the case of NGC 4236 and 4569, the only metallicity measurements available are from the B-band luminosity–metallicity (L–Z) relationship and we use those values from M10 with no gradient. Finally, two of our galaxies are not in the M10 sample. For NGC 3077, we use the metallicity 12 + log (O/H) = 8.9 given in KK04 with no gradient, from Calzetti et al. (1994). To obtain a PT05 measurement for NGC 3077, we subtract 0.6 dex, the average offset between the two calibrations found by M10. For NGC 5457 (a.k.a. M 101), a galaxy with a well-known radial metallicity gradient, we use the measurements from Bresolin (2007). These metallicities are from direct methods, so are not on the same scale as the measurements from either PT05 or KK04. The metallicities and gradients we use are listed in Table 3. These values are converted to match the r25 values we adopt in this work, which can be slightly different from those adopted by M10. In order to compare with the MW, we use the metallicity of the Orion Nebula H ii region in the PT05 and KK04 calibrations, i.e., 12+log(O/H) = 8.5 for PT05 and 8.8 for KK04, which were obtained by applying the strong-line metallicity calibrations to the integrated spectrum of Orion from integral field spectroscopy36 (Sánchez et al. 2007).
Table 3. Adopted Metallicities and Gradients
PT05 | PT05 | KK04 | KK04 | ||
---|---|---|---|---|---|
Galaxy | Central Metallicity | Metallicity Gradient | Central Metallicity | Metallicity Gradient | Source |
(12 + log(O/H)) | (dex ) | (12 + log(O/H)) | (dex ) | ||
NGC 0337 | 8.18 ± 0.07 | ⋅⋅⋅ | 8.84 ± 0.05 | ⋅⋅⋅ | M10 Table 9 |
NGC 0628 | 8.43 ± 0.02 | −0.25 ± 0.05 | 9.19 ± 0.02 | −0.54 ± 0.04 | M10 Table 8 |
NGC 0925 | 8.32 ± 0.01 | −0.21 ± 0.03 | 8.91 ± 0.01 | −0.43 ± 0.02 | M10 Table 8 |
NGC 2841 | 8.72 ± 0.12 | −0.54 ± 0.39 | 9.34 ± 0.07 | −0.36 ± 0.24 | M10 Table 8 |
NGC 2976 | 8.36 ± 0.06 | ⋅⋅⋅ | 8.98 ± 0.03 | ⋅⋅⋅ | M10 Table 9 |
NGC 3077 | 8.30 ± 0.20 | ⋅⋅⋅ | 8.90 ± 0.20 | ⋅⋅⋅ | K11 |
NGC 3184 | 8.65 ± 0.02 | −0.46 ± 0.06 | 9.30 ± 0.02 | −0.52 ± 0.05 | M10 Table 8 |
NGC 3198 | 8.49 ± 0.04 | −0.38 ± 0.11 | 9.10 ± 0.03 | −0.50 ± 0.08 | M10 Table 8 |
NGC 3351 | 8.69 ± 0.01 | −0.27 ± 0.04 | 9.24 ± 0.01 | −0.15 ± 0.03 | M10 Table 8 |
NGC 3521 | 8.44 ± 0.05 | −0.12 ± 0.25 | 9.20 ± 0.03 | −0.52 ± 0.15 | M10 Table 8 |
NGC 3627 | 8.34 ± 0.24 | ⋅⋅⋅ | 8.99 ± 0.10 | ⋅⋅⋅ | M10 Table 9 |
NGC 3938 | 8.42 ± 0.20 | ⋅⋅⋅ | 9.06 ± 0.20 | ⋅⋅⋅ | M10 L–Z |
NGC 4236 | 8.17 ± 0.20 | ⋅⋅⋅ | 8.74 ± 0.20 | ⋅⋅⋅ | M10 L–Z |
NGC 4254 | 8.56 ± 0.02 | −0.35 ± 0.08 | 9.26 ± 0.02 | −0.39 ± 0.06 | M10 Table 8 |
NGC 4321 | 8.61 ± 0.07 | −0.31 ± 0.17 | 9.29 ± 0.04 | −0.28 ± 0.11 | M10 Table 8 |
NGC 4536 | 8.21 ± 0.08 | ⋅⋅⋅ | 9.00 ± 0.04 | ⋅⋅⋅ | M10 Table 9 |
NGC 4569 | 8.58 ± 0.20 | ⋅⋅⋅ | 9.26 ± 0.20 | ⋅⋅⋅ | M10 L–Z |
NGC 4625 | 8.35 ± 0.17 | ⋅⋅⋅ | 9.05 ± 0.07 | ⋅⋅⋅ | M10 Table 9 |
NGC 4631 | 8.12 ± 0.11 | ⋅⋅⋅ | 8.75 ± 0.09 | ⋅⋅⋅ | M10 Table 9 |
NGC 4725 | 8.35 ± 0.13 | ⋅⋅⋅ | 9.10 ± 0.08 | ⋅⋅⋅ | M10 Table 9 |
NGC 4736 | 8.40 ± 0.01 | −0.23 ± 0.12 | 9.04 ± 0.01 | −0.08 ± 0.10 | M10 Table 8 |
NGC 5055 | 8.59 ± 0.07 | −0.59 ± 0.27 | 9.30 ± 0.04 | −0.51 ± 0.17 | M10 Table 8 |
NGC 5457 | 8.75 ± 0.05 | −0.75 ± 0.06 | 8.75 ± 0.05 | −0.75 ± 0.07 | B07 |
NGC 5713 | 8.48 ± 0.10 | ⋅⋅⋅ | 9.08 ± 0.03 | ⋅⋅⋅ | M10 Table 9 |
NGC 6946 | 8.45 ± 0.06 | −0.17 ± 0.15 | 9.13 ± 0.04 | −0.28 ± 0.10 | M10 Table 8 |
NGC 7331 | 8.41 ± 0.06 | −0.21 ± 0.31 | 9.18 ± 0.05 | −0.49 ± 0.25 | M10 Table 8 |
References. Moustakas et al. (2010, M10), Kennicutt et al. (2011, K11), Bresolin (2007, B07).
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2.4.2. Star Formation Rate and Stellar Mass Surface Density Maps
The star formation rate (SFR) surface densities (ΣSFR) are calculated from Hα and 24 μm maps using the Hα maps and the procedure described in Leroy et al. (2012). The Hα maps have been convolved to match the SPIRE 350 μm PSF assuming an initial ∼1''–2'' FWHM Gaussian PSF, although the large difference between the initial and final PSF makes this choice mostly irrelevant. We use 24 μm maps from SINGS, processed (background subtracted, convolved, and aligned) as described in Aniano et al. (2012). The Aniano et al. (2012) modeling results described in Section 2.1 are also used to remove a cirrus component unrelated to star formation from the 24 μm map, as described in Leroy et al. (2012).
We calculate the stellar mass surface density (Σ*) from the IRAC 3.6 μm observations from SINGS, as described in Leroy et al. (2008). These calculations provide only a rough tracer of stellar mass surface density, since we do not take into account corrections for various contaminants in the 3.6 μm band (Zibetti & Groves 2011; Meidt et al. 2012).
2.5. Processing
After all maps have been convolved to the SPIRE 350 μm resolution, we sample them with a hexagonal grid with approximately half-beam spacings (i.e., 125). Uncertainties in the dust mass surface density, CO integrated intensity, and H i column density are propagated through the necessary convolutions and samplings. Surface densities and other quantities have been deprojected using the orientation parameters listed in Table 1.
3. SOLVING SIMULTANEOUSLY FOR αCO AND THE DGR
In order to use the dust mass surface density to trace the total gas mass surface density, we assume (1) that dust and gas are well mixed (i.e., that Equation (3) holds), (2) that the DGR is constant on ∼kiloparsec scales in our target galaxies, and (3) within a given ∼kiloparsec region, the DGR does not change between the atomic and molecular phases. Then, given multiple measurements of ΣD, , and ICO that span a range of CO/H i values in a kiloparsec-scale region of a galaxy, we can adjust αCO until we find the value that returns the most uniform DGR for the region. This procedure makes no assumption about the value of the DGR, only that it is constant in that region. In addition, this procedure makes no presumptions about the value of αCO or the scales over which it varies. If αCO varies on small scales, our measured αCO value will represent the dust (or gas) mass surface density weighted average αCO for the region. We discuss this process in detail in the following sections.
A simultaneous solution for αCO and the DGR can only be performed if a range of CO/H i ratios are present in the measurements. The linear dependence of on αCO provides leverage to adjust αCO in order to best describe all of the points with the same DGR over a range of CO/H i ratios. An "incorrect" αCO value will result in a dependence of the measured DGR on the CO/H i ratio, increasing the spread in the DGR values in the region. An illustration of this effect is shown in panel (c) of Figure 1. Finding a solution or best-fit αCO is equivalent to locating a minimum in the DGR scatter at a given value of αCO.
The basic procedure we use minimizing the scatter in the DGR values in the region was suggested by Leroy et al. (2011). There are, however, a variety of other techniques to solve for αCO and the DGR given multiple measurements, including directly fitting a plane to ICO, ΣD, and . It is not clear a priori which scatter minimization technique is optimal, so we performed a set of simulations, described in the Appendix, to test various techniques and optimize the procedure for our dataset and objectives. We describe the resulting scatter minimization procedure in more detail below.
3.1. Defining the "Solution Pixel"
To perform the solution, we require multiple measurements of dust and gas tracers in the region. We also aim, however, to select the smallest possible regions, in order to ensure an approximately constant DGR. We proceed by dividing each target galaxy into hexagonal regions encompassing 37 of the half-beam spaced sampling points. We call these regions "solution pixels" (see panel (a) of Figure 1 for an example). The 37-point solution pixels are a compromise between small region sizes and a sufficient number of independent measurements needed to minimize statistical noise. The solution pixels tile the galaxy with center-to-center spacing of 375. Thus, neighboring solution pixels are not independent and share ∼40% of their sampling points. The overlap between solution pixels is illustrated in Figure 1. Such a tiling is optimal because it fully samples the data. To ensure that the final results are not dependent on the placement of the solution pixels, we performed a test where we distributed the solution pixels randomly throughout the galaxies and compared the resulting radial trends in αCO to what we measured using the fixed grid described above. The radial trends were in agreement, demonstrating that our results are insensitive to the exact placement of the solution pixel grid. The solution pixels correspond to physical scales ranging from ∼0.6 kpc to 3.9 kpc. We have tiled each galaxy with solution pixels out to the maximum value of r25 contained in the HERACLES maps.
3.2. Minimizing the DGR Scatter
For each sampling point i in the solution pixel, the measurements of ΣD, i, , i, and ICO, i, along with an assumed αCO, determine the DGRi. We step through a grid of αCO values to find the αCO that results in the most uniform DGR for all the DGRi values in the solution pixel. In all solutions presented here, we use an αCO grid with 0.05 dex spacing, spanning the range αCO = 0.1–100 M☉ pc−2 (K km s−1)−1.
We determine the most "uniform" DGR in a solution pixel by minimizing the scatter in the DGRi values as a function of αCO. The scatter is measured with a robust estimator of the standard deviation37 of the logarithm of the DGRi values—this technique appears to work best because outliers have little effect on the measured scatter because of both the logarithmic units and the outlier suppression. After measuring the scatter in the DGR at every αCO value, we find the αCO at which the scatter (Δlog(DGR)) is minimized. This value is taken to be our best-fit αCO value for the region. We consider a solution to be found when a minimum has been located in the DGR scatter within the range of our αCO grid. This outcome does not occur in every solution pixel—some pixels do not have sufficient CO/H i contrast, others have too low S/N, and, for some, the minimum is at the edge of the allowable range and the solution is not well constrained. The failed solutions are not included in our further analysis.
An illustration of the technique is shown in Figure 1 for a region in NGC 6946. In panel (a), we show the HERACLES CO J = (2–1) map of the galaxy with our half-beam sampling grid; the hexagonal region shows the "solution pixel" in question, which includes 37 individual samples from the maps. Panels (b) and (c) show how varying αCO affects the mean DGR and the scatter for the points in the region, illustrating how the scatter increases away from the best αCO value. Panel (d) shows the scatter as a function of αCO for the whole αCO grid. A clear minimum exists for this solution pixel at αCO ∼ 1.4 M☉ pc−2 (K km s−1)−1.
3.3. Statistical Uncertainties on αCO and the DGR
We judge the uncertainties on the "best-fit" αCO and the DGR in several ways. First, to take into account statistical errors, we perform a Monte Carlo test on the solutions by adding random noise to our measured ΣD, , and ICO values according to each point's measurement errors. We repeat the solution with the randomly perturbed data values 100 times and find the standard deviation of the results. We also perform a "bootstrapping" trial, which tests the sensitivity of each solution to individual measurements. In each bootstrap iteration for a given solution pixel, we randomly select 37 sampling points, with replacement, and derive the solution. The bootstrap procedure is repeated 100 times for each solution pixel and we measure the resulting standard deviation of the αCO values. The standard deviations from the Monte Carlo and bootstrapping iterations are added in quadrature to produce the final quoted error for the αCO values we determine. In addition, to check these uncertainties, we also estimate the scatter and bias in αCO for the given technique from our simulated data trials described in the Appendix, based on the median CO S/N in the solution pixel and the measured minimum of Δlog(DGR). The uncertainties from Monte Carlo plus bootstrapping are comparable to what we expect given the simulated data trials.
3.4. Systematic Uncertainties on αCO
3.4.1. Uncertainties on αCO from R21 Variations
In the following, we report αCO appropriate for the (1–0) line, since it is the canonical CO-to-H2 conversion factor that most observational and theoretical studies utilize. To do so, we have converted between (2–1) (which we have directly measured) and (1–0) using a fixed line ratio R21 = 0.7. Deviations from this R21 value will result in systematic offsets in the (1–0) conversion factor, while the (2–1) conversion factor will be unaffected since it is what we have directly measured. To quantify any (1–0) αCO offsets, we have investigated the variability of R21 in those galaxies with publicly available CO J = (1–0) maps from the Nobeyama survey of nearby spiral galaxies (Kuno et al. 2007). Galaxies that have Nobeyama maps are marked with an asterisk in Table 1. The details of this comparison can be found in the Appendix. We find that deviations from R21 = 0.7 can cause small systematic shifts in αCO appropriate for the (1–0) line, but the magnitude of the shifts are generally within the uncertainties on the αCO solutions (i.e., typically less than 0.2 dex). We note that variations of R21 within a pixel would introduce additional systematic uncertainties on αCO.
3.4.2. Variations of ΣD Linearity within Solution Pixels
We assume that the dust tracer we employ (ΣD) linearly tracks the true dust mass surface density in a solution pixel. Because we calibrate the DGR based on the values of ΣD within each pixel, any multiplicative constant term cancels out in Equation (3) and does not affect the measurement of αCO. Nonlinearities in ΣD that are uncorrelated with the atomic/molecular phase add scatter to our measurements of αCO but do not introduce systematic errors. In the following, we discuss several sources of nonlinearity in ΣD that are correlated with the ISM phase and estimate their systematic error contribution.
- 1.Variation of dust emissivity. A variety of observations have suggested that dust emissivity increases in molecular gas relative to atomic gas (note, however, that most of the studies use CO to trace molecular gas and may interpret variations in αCO as changes in emissivity). Recent work has suggested that the dust emissivity increases by a factor of ∼2 between the atomic and molecular ISM (Planck Collaboration et al. 2011a; Martin et al. 2012). If the dust in molecular regions has a higher emissivity, ΣD will overestimate the amount of dust there, causing us to overestimate the amount of gas. In that case, we would recover a higher αCO than actually exists. As a first approximation, our measured αCO would be too high by the change in emissivity between atomic and molecular phases, a factor of ∼2 based on the previously discussed results.
- 2.Variation of the DGR. Evidence from the depletion of gas phase metals in the MW suggests that the DGR increases as a function of the H2 fraction. To estimate the magnitude of such effects, we use the results of Jenkins (2009). From the minimum level of depletion measured in the MW to complete depletion of all heavy elements, the DGR varies by a factor of four. A large fraction of this change in the DGR comes from the depletion of oxygen, however, which may not predominantly be incorporated into dust as it is depleted (see the discussion in Section 10.1.4 of Jenkins 2009). Excluding oxygen, the possible change in the DGR is a factor of two. Using the correlation between the depletion and the H2 fraction from Figure 16 of Jenkins (2009), we find that for 10%–100% H2 fractions (as are appropriate for our regions), the possible variation in the DGR is a factor of two (or less, depending on the contribution of oxygen). As in the case of dust emissivity variations, the effect of the DGR increasing in molecular gas would be to artificially increase our measured αCO by the same factor as the increase in the DGR.
- 3.Systematic biases in measuring ΣD from SED modeling. Because warm dust will radiate more strongly per unit mass than cold dust at all wavelengths, the SED will not clearly reflect the presence of cold dust unless it dominates the mass. This fact means that the SED fitting technique is not sensitive to cold dust contained in giant molecular cloud (GMC) interiors (AV ≳ 1) at our spatial resolution. The fraction of the dust mass in these interiors, assuming a spherical cloud with uniform density and total AV ≈ 8 mag, is ∼40%; this estimate agrees well with the recent extinction mapping measurements of MW GMCs of Kainulainen et al. (2011) and Lombardi et al. (2011). If we underestimate the mass of dust by missing cold dust in GMC interiors, we would underestimate the amount of molecular gas and adjust αCO downward. The magnitude of this effect is at a factor of ∼2 level and is opposite in direction to what we expect for dust emissivity or the DGR increase in molecular clouds.
To summarize, variations of the DGR and dust emissivity between atomic/molecular gas could both bias our αCO results toward higher values by factors of ∼2. Systematic biases in accounting for cold dust in the SED modeling act in the opposite direction (i.e., biasing αCO toward lower values), also by a factor of ∼2.
3.4.3. Opaque H I
The H i maps we use have not been corrected for any optical depth effects (Walter et al. 2008). H i observations of M31 at high spatial and spectral resolution have suggested there may be large local opacity corrections on 50 pc scales (Braun et al. 2009). To estimate the importance of any opaque H i, we have used the corrected and uncorrected maps of M31, provided to us by R. Braun. Convolving to 500 pc spatial resolution, the average resolution element in M31 has a 20% correction to the H i column density. Choosing only regions with NH > 1021 cm−2, the average correction is ∼30%. Essentially all resolution elements have opacity corrections less than a factor of two.
If opaque H i exists at the level Braun et al. (2009) found in M31, it would have two main effects on our solutions for αCO. First, on average, the optically thin estimate for the atomic gas mass would be too low, resulting in our procedure determining a DGR that is too high (excess dust compared to the amount of gas). In the molecular regions, then, we will expect too much gas based on that same DGR, and consequently artificially increase αCO. Second, since the opaque H i features do not appear to be spatially associated with molecular gas (see Braun et al. 2009, Section 4.1, for a further discussion), these features will act as a source of intrinsic scatter in the DGR. In the Appendix, we explore the effect of intrinsic scatter on our solution technique. At the level of opaque H i in M31, we do not find an appreciable bias in the recovered αCO due to scatter. We expect the magnitude of the systematic effects due to opaque H i, if it exists, to be well within the statistical uncertainties we achieve on the αCO measurements.
3.5. Systematic Uncertainties on the DGR
3.5.1. Absolute Calibration of ΣD
As we have discussed above, as long as ΣD is a linear tracer of the true dust mass surface density within a given solution pixel, its absolute calibration has no effect on the αCO value we measure. The same is not true for the DGR value. Any uncertainties on the calibration of ΣD will be directly reflected in the DGR measurement. The ΣD values we used are from fits of the Draine & Li (2007) models to the IR SED using the MW RV = 3.1 grain model. The extent to which the appropriate dust emissivity κν deviates from the value used by this model represents a systematic uncertainty on the DGR values we derive. Our knowledge of κν in different environments is limited, but there are constraints from observations of dust extinction curves and depletions in the Large Magellanic Cloud (LMC) and Small Magellanic Cloud (SMC; cf. Weingartner & Draine 2001), where measured RV values can deviate significantly from the canonical value of 3.1. Draine et al. (2007) demonstrated that the ΣD values decreased by a factor of ∼1.2 when the LMC or SMC dust model was used instead of the MW RV = 3.1 model. Given that our sample is largely dominated by spiral galaxies and hence does not probe environments with metallicities comparable to those of the SMC (due to the faintness of CO in such regions and our S/N limitations), we expect that the systematic uncertainties on our DGR when comparing with other results from Draine & Li (2007) model fits is small. It is important to note, however, that different dust models, even fit to the same RV = 3.1 extinction curve, have systematic offsets in their dust mass predictions due to different grain size distributions, grain composition, etc. Therefore, the comparison of our DGR values to results from studies not using the Draine & Li (2007) models will show systematic offsets.
4. RESULTS
4.1. NGC 0628 Results Example
We divided each of the 26 galaxies in our sample into solution pixels and performed the simultaneous solution for the DGR and αCO in each pixel. As an example, we present the results for NGC 0628 in the following section. The results for all solution pixels in all galaxies can be found in the Appendix.
Figure 2 shows, from left to right, the H i, CO, and ΣD maps used in our analysis. The circles overlaid on the maps represent the centers of the solution pixels we have defined. Figure 3 shows the same circles representing the solution pixel centers. The left panel shows the pixel centers now filled in with a color representing the best αCO solution for that pixel. In the middle panel, a gray scale shows the uncertainty on that αCO solution. The DGR values are shown in the panel on the right. Finally, in Figure 4, we show these measured αCO values as a function of galactocentric radius (r25). For comparison, Figure 4 also shows the local MW αCO = 4.4 M☉ pc−2 (K km s−1)−1 value with a solid horizontal line (dotted lines show a factor of two above and below; see Section 5.1 for details on the measurement of the MW value). We note that the MW may show a gradient of αCO with radius (also discussed in Section 5.1), but for purposes of comparison with the most widely used conversion factor, we use a constant αCO on all plots.
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Standard image High-resolution imageIn general, NGC 0628 shows a αCO value consistent with the MW value within a factor of two at all galactocentric radii. Outside a radius of r25 ∼ 0.6, we find few good solutions. There is a weak trend for lower αCO at smaller radii, with the central solution pixel having a conversion factor αCO = 2.2 M☉ pc−2 (K km s−1)−1. Recent work by Blanc et al. (2013) found consistent results for αCO by inverting the SFR surface density map using a fixed molecular gas depletion time.
4.2. Completeness of Solutions
The technique we have used to solve for the DGR and αCO simultaneously only works if there is sufficient S/N in the CO map and a range of CO/H i ratios in each solution pixel. These two constraints impose limits on where in the galaxies we can recover solutions. In order to perform statistical tests on our sample of αCO and DGR values, we need to understand what biases these limits introduce into our results. For example, the failure of the technique in regions with low CO S/N generally limits our good solutions to the inner parts of galaxies, where metallicities tend to be higher. In order to judge the existence of trends in αCO versus metallicity, we therefore need to understand where we have achieved good solutions.
To investigate these effects, we have examined the fraction of solution pixels that have solutions and the uncertainty on the derived αCO values as a function of the range of CO/H i ratios and mean ICO in a pixel. In general, the H i in our target galaxies has a quite flat radial profile, while the CO drops off approximately exponentially (Schruba et al. 2011). Because of these trends, wherever there is sufficient signal in CO to achieve a good solution, the CO/H i range is adequate as well. Thus, we find that the mean ICO of a solution pixel is the best predictor for the existence and quality of a solution. Figure 5 shows the fraction of pixels with solutions and the average uncertainty on the solutions as a function of mean ICO. We identify a cut-off at ICO > 1 K km s−1 above which we obtain solutions >90% of the time and those solutions have an average uncertainty of <0.5 dex. For any statistical analysis that follows, we use only pixels above this cut-off.
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Standard image High-resolution image4.3. Properties of Full-sample αCO Solutions
In Tables 4 and 5, we list the average αCO derived galaxy by galaxy and for the full sample. These averages only include solution pixels where ICO > 1 K km s−1. The first two columns of Table 5 list the mean and standard deviation of the individual solution pixel measurements. This approach treats each solution pixel equally, regardless of how strongly it contributes to the total molecular gas mass. The third column instead lists the mean αCO derived from the total and the total ICO for the galaxy (above ICO = 1 K km s−1), which is equivalent to a mean where the pixels are weighted by their ICO, values. If a single αCO value were to be applied to the data, this value would be the optimal quantity to use. For most galaxies, the CO-weighted mean is higher than the straight mean of the solution pixels. This result is due to the fact that the molecular gas is not evenly distributed across the galaxy and the area-weighted average is different then the molecular gas-weighted average.
Table 4. Galaxy Average αCO
Galaxy | Mean αCO | Std. Dev. | CO Weighted | Number of |
---|---|---|---|---|
(dex) | Mean αCO | Measurements | ||
NGC 0337 | 22.4 | 16.2−31.0 (0.14) | 21.8 | 2 |
NGC 0628 | 3.9 | 2.1−7.4 (0.28) | 5.1 | 67 |
NGC 0925 | 10.0 | 6.8−14.7 (0.17) | 10.0 | 1 |
NGC 2841 | 5.0 | 2.5−10.3 (0.31) | 5.7 | 19 |
NGC 2976 | 3.3 | 0.9−12.5 (0.58) | 4.7 | 18 |
NGC 3077 | 4.6 | 2.3−9.4 (0.31) | 5.4 | 7 |
NGC 3184 | 5.3 | 2.9−9.5 (0.26) | 6.3 | 43 |
NGC 3198 | 11.0 | 6.4−18.9 (0.24) | 11.9 | 11 |
NGC 3351 | 2.7 | 1.0−6.9 (0.41) | 2.9 | 28 |
NGC 3521 | 7.6 | 4.9−11.8 (0.19) | 7.3 | 42 |
NGC 3627 | 1.2 | 0.4−3.3 (0.44) | 1.8 | 43 |
NGC 3938 | 5.5 | 4.1−7.5 (0.13) | 5.8 | 19 |
NGC 4236 | ... | ... | ... | 0 |
NGC 4254 | 3.4 | 2.1−5.7 (0.22) | 4.7 | 46 |
NGC 4321 | 2.2 | 1.1−4.6 (0.32) | 2.2 | 57 |
NGC 4536 | 2.6 | 1.0−6.7 (0.41) | 2.6 | 13 |
NGC 4569 | 1.1 | 0.3−4.1 (0.57) | 1.2 | 14 |
NGC 4625 | ... | ... | ... | 0 |
NGC 4631 | 10.8 | 5.6−19.5 (0.26) | 9.8 | 40 |
NGC 4725 | 1.2 | 0.4−3.2 (0.44) | 1.8 | 7 |
NGC 4736 | 1.0 | 0.5−2.0 (0.29) | 1.1 | 33 |
NGC 5055 | 3.7 | 1.9−7.4 (0.30) | 4.0 | 86 |
NGC 5457 | 2.3 | 1.1−4.8 (0.32) | 2.9 | 142 |
NGC 5713 | 4.6 | 1.7−12.6 (0.44) | 5.4 | 13 |
NGC 6946 | 2.0 | 0.9−4.4 (0.35) | 1.8 | 158 |
NGC 7331 | 9.8 | 6.2−15.3 (0.20) | 10.7 | 32 |
Notes. Averages include only solution pixels with ICO > 1 K km s−1. The number of measurements meeting this criterion are shown in the last column of the table.
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Table 5. Sample Average αCO
Sample | Mean αCO | Std. Dev. | CO Weighted | Gal. Weighted | Gal and CO Weighted |
---|---|---|---|---|---|
All Lines of Sight | (dex) | Mean αCO | Mean αCO | Mean αCO | |
Incl < 65° | 2.6 | 1.0−6.6 (0.41) | 2.9 | 3.1 | 3.5 |
Incl > 65° | 7.2 | 3.0−17.6 (0.39) | 8.2 | 6.5 | 6.7 |
Note. Averages include only solution pixels with ICO > 1 K km s−1.
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Figure 6 shows several histograms illustrating the distribution of our measured αCO values. The mean, derived with several different weighting schemes, is listed in Table 5. The top panels of Figure 6 show histograms of all solution pixels while the bottom panels show histograms of the galaxy averages from Table 4. On these histograms, we highlight galaxies with high inclinations (i > 65°) in green. It is clear that the high inclination galaxies tend to have higher αCO values on average than the more face-on galaxies. In the highest inclination galaxies, the pixel will include contributions from gas at larger radii, this gas tends to have a lower DGR and be less molecular-gas-rich. This result is equivalent to the challenge faced by Leroy et al. (2011) in the SMC, where some of the H i along the line of sight originates in an essentially dust-free envelope, and in M31, where regions along the minor axis of the galaxy have contributions from gas and dust at a variety of radii. In addition, optical depth effects for H i may be accentuated for highly inclined galaxies. All galaxies with i > 65° show average αCO values above the mean (except for NGC 0925, which has a somewhat uncertain inclination; de Blok et al. 2008). We thus eliminate all galaxies with i > 65°, leaving 782 total αCO measurements.
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Standard image High-resolution imageIn Table 5, we list the average values of αCO for the full galaxy sample. Excluding the high inclination galaxies, we find an average αCO = 2.6 M☉ pc−2 (K km s−1)−1 for the individual solution pixel results. Weighted by ICO, the average value is slightly higher, αCO = 2.9 M☉ pc−2 (K km s−1)−1. To avoid highly resolved galaxies like NGC 5457 and 6946 contributing more points to the average, we also calculate averages where each galaxy contributes uniformly. These averages are listed in the last two columns of Table 5. The average value for our sample, αCO = 3.1 M☉ pc−2 (K km s−1)−1, is only slightly lower than what is found in the MW disk.
The standard deviation in αCO is 0.38 dex, when all lines of sight are treated equally (with our ICO and inclination cut-offs). A key question we would like to answer is to what degree this scatter represents (1) the true scatter within each galaxy, (2) the galaxy-to-galaxy offsets, or (3) the variation of αCO as a function of local parameters. If the scatter comes from variations with local environmental parameters, we may be able to generate a prescription for αCO as a function of other observables. In the following sections, we explore the variations of αCO within and among our galaxies to understand if and why αCO varies.
4.4. Radial Variations in αCO
In Figure 7, we present a summary of the αCO values we find as a function of galactocentric radius. Plots of αCO from each individual galaxy as a function of r25 are presented in the Appendix. Each individual solution that makes our ICO and inclination cut is shown in Figure 7 as a gray circle. We also display the mean and standard deviation of the αCO values in 0.1 r25 bins for each galaxy (this mean treats all solution pixels equally). The top panel of Figure 7 shows the measured αCO values and the bottom panel shows those same values normalized by each galaxy's average αCO from Table 4.
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Standard image High-resolution imageThe average radial profile of our galaxies is mostly flat as a function of r25, but almost all galaxies show a decrease in αCO in the inner ∼0.2 r25 compared to their average value. The mean central decrease is ∼0.3–0.4 dex, but it can be as much as 0.8 dex. For several galaxies, this decrease leads to a central αCO value that is an order to magnitude lower than the MW αCO (e.g., NGC 4736, 5457, and 6946). The central depression persists even after correcting for differences in R21 (see the following section for further discussion).
Normalizing each galaxy by its average αCO and making each galaxy contribute equally to the average leads to a much smaller scatter at r25 > 0.3; this result can be seen in the bottom panel of Figure 7 where the radial profiles show much less scatter than the individual measurements, which is not the case in the top, unnormalized, panel. Inside that radius, the scatter in the normalized αCO profiles is reduced, but not by as much as outside that radius, indicating that individual galaxies show different central profiles of αCO. The overall conclusions to be drawn from Figure 7 are: (1) outside r25 ∼ 0.3, most of the scatter in our αCO measurements can be explained by galaxy-to-galaxy differences, (2) inside that galactocentric radius, galaxy-specific trends in αCO dominate the scatter, and (3) in general, the inner region of galaxies shows a lower αCO value than the rest of the disk.
4.5. αCO in Galaxy Centers
In Table 6, we list the central αCO values and compare them to the MW value and the mean for the galaxy. Almost all of the central solution pixels have αCO lower than the galaxy mean. The galaxies NGC 3351, 3627, 4321, 4736, 5457, and 6946 show αCO values a factor of five or more lower than the MW value, at the 3σ confidence level. For NGC 4736, 5457, and 6946, in particular, the central solution pixel has a αCO value an order of magnitude below the MW value. Only one galaxy, NGC 0337, shows a central αCO higher than the MW value at a 3σ confidence level. In Table 6, we also list the CO (2–1)/(1–0) ratio measured as described in Section 3.4.1. While the central solution pixels do tend to have higher R21 values than the value we adopted, the difference is less than a factor of two in all cases and does not alter our main conclusions about the low (1–0) conversion factor in these regions. In particular, for the 10 galaxies with measured R21 and i < 65°, the central αCO corrected for R21 is still on average 0.3 dex lower (i.e., a factor of two) than the galaxy average.
Table 6. Central αCO Measurements
Galaxy | log (αCO, Cen) | ΔMW = | ΔMW/σ | Δmean = | Δmean/σ | R21 | log (R21/0.7) |
---|---|---|---|---|---|---|---|
±σ | log (αCO/αCO, MW) | log (αCO/〈αCO〉) | |||||
NGC 0337 | +1.25 ± 0.17 | +0.61 | 3.6 | −0.10 | 0.6 | ... | ... |
NGC 0628 | +0.35 ± 0.24 | −0.29 | 1.2 | −0.24 | 1.0 | ... | ... |
NGC 2976 | +0.00 ± 0.49 | −0.64 | 1.3 | −0.51 | 1.0 | ... | ... |
NGC 3077 | +0.60 ± 0.17 | −0.04 | 0.2 | −0.06 | 0.4 | ... | ... |
NGC 3184 | +0.25 ± 0.16 | −0.39 | 2.5 | −0.47 | 3.0 | 0.77 ± 0.05 | +0.04 |
NGC 3351 | −0.15 ± 0.14 | −0.79 | 5.6 | −0.58 | 4.1 | 1.10 ± 0.24 | +0.19 |
NGC 3627 | −0.25 ± 0.14 | −0.89 | 6.3 | −0.34 | 2.4 | 0.54 ± 0.05 | −0.12 |
NGC 3938 | +0.70 ± 0.19 | +0.06 | 0.3 | −0.04 | 0.2 | ... | ... |
NGC 4254 | +0.95 ± 0.82 | +0.31 | 0.4 | +0.41 | 0.5 | 1.03 ± 0.06 | +0.17 |
NGC 4321 | −0.20 ± 0.17 | −0.84 | 4.8 | −0.55 | 3.1 | 1.25 ± 0.16 | +0.25 |
NGC 4536 | +0.35 ± 0.13 | −0.29 | 2.2 | −0.07 | 0.5 | 1.26 ± 0.28 | +0.26 |
NGC 4625 | +1.05 ± 0.41 | +0.41 | 1.0 | ... | ... | ... | ... |
NGC 4725 | −0.15 ± 0.71 | −0.79 | 1.1 | −0.22 | 0.3 | ... | ... |
NGC 4736 | −0.55 ± 0.17 | −1.19 | 6.9 | −0.56 | 3.2 | 1.35 ± 0.09 | +0.29 |
NGC 5055 | +0.00 ± 0.25 | −0.64 | 2.6 | −0.57 | 2.3 | 1.10 ± 0.08 | +0.20 |
NGC 5457 | −0.45 ± 0.20 | −1.09 | 5.5 | −0.80 | 4.1 | 0.90 ± 0.08 | +0.11 |
NGC 5713 | +0.50 ± 0.25 | −0.14 | 0.6 | −0.16 | 0.6 | ... | ... |
NGC 6946 | −0.40 ± 0.31 | −1.04 | 3.4 | −0.70 | 2.3 | 1.07 ± 0.14 | +0.19 |
Note. Galaxies with i > 65° have been omitted from the table.
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The central solution pixels can be outliers from the rest of the pixels in our sample in the sense of having high CO/H i ratios. Since there are relatively few solution pixels with these conditions, they may not have been well represented in the simulated data we used to test the accuracy of the solution technique. High CO/H i ratios could bias the results: if the S/N of the H i maps is almost always higher than the S/N of the CO maps, the DGR scatter could be reduced in these conditions purely by decreasing the importance of CO in assessing the gas mass surface density. Since this bias would move the αCO results toward lower values in the centers, we performed a test to judge whether our low central αCO measurements could be due to this effect. The details of the test are described in the Appendix. In brief, we generated simulated datasets with known αCO values where the , ICO, and ΣD S/N is matched to the observations in each central solution pixel. We performed Monte Carlo trials to see how well the known input αCO was recovered. In all cases, we found no evidence for a bias in the central solution pixel.
Taking into account the offset from R21 variations, our results show that the central αCO in NGC 3351, 3627, 4321, 4736, 5457, and 6946 is lower than the MW value by a factor of 4–10. Many of these galaxies show αCO values closer to the MW value at larger radii, in line with the general trend seen in Figure 7. For NGC 3627, the mean αCO for the galaxy is low as well, suggesting that the central region is not distinct from the rest of the disk (this galaxy is an interacting member of the Leo Triplet, so it is unique in our sample). Conversely, examination of the individual galaxy αCO measurements as a function of radius (shown in the Appendix) for NGC 3351, 4321, 4736, 5457, and 6946 demonstrates that these galaxies show an unresolved region of lower-than-average αCO values in their centers (note that our solution pixel grid oversamples the data, so an unresolved central depression affects the r25 = 0 point and the six adjacent solution pixels). The closest galaxy that shows a central depression is NGC 4736 at D = 4.66 Mpc. At this distance, our solution pixel covers a region of radius 0.8 kpc. Even for this nearby example, we do not resolve the central depression. We tested whether the depressions were resolved using a grid of independent solution pixels (i.e., not overlapping) and found that the depression only affected the central pixel, consistent with it being unresolved. We note that our ability to detect any central depression may be a function of the galaxy's distance due to the increased size of the central solution pixel. Even at D = 14.3 Mpc, however, we detect a clear central depression in NGC 4321.
The type of nuclear activity in each galaxy is not a good predictor for whether or not it displays a central αCO depression. Of the galaxies that show the clearest central depression, NGC 3351, 5457, and 6946 are classified as star-formation or H ii region dominated, while NGC 4321 and 4736 have signatures of active galactic nucleus (AGN) or low-ionization nuclear emission-line region activity (for details on the nuclear classifications; see Kennicutt et al. 2011). Several galaxies with flat radial αCO profiles do show evidence for AGN activity: NGC 3627, 4254, and 4725, for example. Enhanced AGN activity could affect molecular gas properties in the nuclei (e.g., Krips et al. 2008), but the relatively weak AGNs present in the KINGFISH galaxies may not dominate on the kiloparsec scales we study here.
To summarize, we find that several galaxies in our sample show central αCO values that are substantially lower than the MW value and also well below the galaxy average. This phenomenon appears to take the form of a depression in the central region that is unresolved by our solution pixel grid. We discuss these central regions and the physical conditions that may lead to low αCO values further in Section 6.3.
4.6. Correlations of αCO with Environmental Parameters
Variations in αCO may be related to variations in the local environmental conditions including metallicity, ISM pressure, interstellar radiation field strength, gas temperature, dust properties, or other variables. Correlations between αCO and quantities that trace these environmental conditions may allow us to identify the drivers of αCO variations. These correlations may also provide tools to predict the appropriate αCO in a given environment. In the following, we examine the correlations of our measured αCO with several observables that trace ISM conditions. For each tracer, we use the average value in each solution pixel. The physical interpretation of these correlations or lack thereof is discussed in Section 6.1.
In Figure 8, we plot our measured αCO values as a function of the average radiation field intensity (), the PAH fraction (qPAH), metallicity (12+log(O/H)), stellar mass surface density (Σ*), SFR surface density (ΣSFR), and the dust mass surface density (ΣD). Each panel shows the individual measurements as gray symbols and the average for the galaxies as red symbols. The MW αCO is highlighted with a horizontal gray line and the mean αCO treating all solution pixels equally (αCO = 2.6 M☉ pc−2 (K km s−1)−1) is shown as a dashed horizontal line. Overlaid on each panel is the binned mean and standard deviation and a linear fit to the gray points. In Table 7, we list the linear fit results as well as the rank correlation (RC) coefficient for each panel and its significance in standard deviations away from the null hypothesis. The RC coefficients suggest there are significant correlations between αCO and all of the variables except metallicity. Due to possible inconsistencies between various metallicity measurements and incomplete knowledge of metallicity gradients in some galaxies, we examine the trends with metallicity separately in Section 4.6.1.
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Standard image High-resolution imageTable 7. αCO Correlation Properties
log(αCO) vs. | Correlationa | σ from | Linear Fitb | |
---|---|---|---|---|
Variable | Coeff. | Null | Offset | Slope |
r25 | +0.19 | 5.2 | 0.29 | +0.29 |
log() | −0.18 | 5.0 | 0.50 | −0.31 |
qPAH (%) | +0.14 | 3.9 | 0.11 | +0.10 |
12+log(O/H) | −0.05 | 1.4 | 2.39 | −0.24 |
log(Σ*) | −0.26 | 7.1 | 1.05 | −0.33 |
log(ΣD) | −0.15 | 4.1 | 0.26 | −0.22 |
log(ΣSFR) | −0.18 | 5.1 | 0.00 | −0.16 |
Notes. These correlations are shown in Figure 8. aSpearman rank correlation coefficient. bCorrelation with metallicity using a homogeneous sample of metallicity measurements is discussed in Section 4.6.1.
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Several other radiation field properties are measured from the dust SED modeling. These include Umin, the minimum radiation field heating the dust, and fPDR, the fraction of the dust luminosity that arises in "photodissociation region (PDR) like" regions where U > 100 UMMP. We have investigated the dependence of αCO on these quantities and find weak trends with low significance.
The existence of a correlation between αCO and environmental parameters does not directly identify the cause of the variations in αCO, particularly since all of the parameters change radially to first order. In Figure 9, we illustrate the radial variations of the same variables by plotting them normalized by their average value as a function of r25. All of the variables show significant correlations with radius. Table 8 lists the correlation coefficients and linear fits to the normalized radial profiles of the parameters. In all cases, the correlation of the variables with r25 is more significant than the correlation of αCO with those variables.
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Standard image High-resolution imageTable 8. Correlation Properties versus r25
Variable vs. | Correlationa | σ from | Linear Fit | |
---|---|---|---|---|
r25 | Coeff. | Null | Offset | Slope |
log(αCO/〈αCO〉gal) | +0.18 | 5.0 | −0.10 | +0.23 |
log() | −0.57 | 15.9 | 0.17 | −0.39 |
qPAH/〈qPAH〉gal | +0.19 | 5.3 | −0.17 | +0.40 |
log((O/H)/〈O/H〉gal) | −0.65 | 18.2 | 0.07 | −0.17 |
log(Σ*/〈Σ*〉gal) | −0.73 | 20.5 | 0.43 | −0.97 |
log(ΣD/〈ΣD〉gal) | −0.68 | 19.1 | 0.25 | −0.56 |
log(ΣSFR/〈ΣSFR〉gal) | −0.31 | 8.8 | 0.37 | −0.86 |
Notes. These correlations are shown in Figure 9. aSpearman rank correlation coefficient.
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If all of the variations of these parameters were primarily related to radius, we would not expect to find stronger correlations between αCO and any parameter than between αCO and radius. Our results suggest, however, that the correlation between αCO and Σ* is stronger (rs = −0.25) and more significant (7.1σ) than the correlation with radius r25 (rs = +0.19, 5.2σ). One possible explanation is that our Σ* measurement may trace the stellar profile better than r25 itself. Other explanations for the correlation of αCO with Σ* will be discussed in Section 6.1.
Figure 7 illustrates that the normalized radial profile of αCO shows a factor of ∼2 standard deviation in a typical radial bin. This uncertainty can be explained primarily by the uncertainty on our αCO solutions themselves, which is typically close to a factor of ∼2. It is therefore unlikely that we could predict αCO as a function of other variables to better precision than a factor of ∼2 unless the galaxy average αCO is highly correlated with that variable. In general, the galaxy averages shown in Figure 8 do not appear to be more tightly correlated with the environmental parameters. Figure 8 thus illustrates that aside from outliers at the extremes of these plots, the minimum standard deviation of αCO in these bins is a factor of two or more and correlations with environmental parameters do not allow us to predict the behavior of αCO within the galaxies better than our normalized radial profile.
As previously discussed, the average profile of αCO versus radius is mostly flat with a central depression in some galaxies. Many of the environmental parameters we plot in Figures 8 and 9 show radial trends extending over the entire range we cover, although the normalized trends generally span less than an order of magnitude. This range does not provide the leverage necessary to separate the dominantly radial correlations of multiple variables. Future studies attempting to associate changes in αCO with environmental parameters will need either higher precision measurements of αCO or observations spanning a greater range of environments.
One possible way to overcome the limitations of separating various radial trends is to normalize all of the variables by their mean in radial bins and then search for residual trends between them. We have investigated such non-radial variations in 0.1 r25 bins and, in general, find only very weak trends. NGC 4254 is one of few galaxies that shows a marginally significant correlation—the normalized αCO measurements correlate with normalized and Σ* at the level of 4σ–5σ from the Spearman RC coefficient. In both cases, the correlation is positive, such that αCO increases in regions with higher and Σ* compared to the average in that radial bin. NGC 6946 also shows a correlation at the 5σ level between normalized αCO and fPDR. In this case, the correlation is negative, meaning that αCO decreases in regions with high fPDR.
NGC 6946 is unique in that the non-radial structure is clearly visible in the maps of αCO shown in the Appendix. The low αCO values in that galaxy appear to track the spiral arm structure seen in the ICO and ΣD maps. To quantify this observation, we have investigated the correlation between the radially normalized αCO, ICO, ΣD, and values. These correlations are weak (all are <5σ significance in the Spearman RC) but more widespread. NGC 3627, 4254, 4321, 5457, and 6946 all show some degree of correlation at >3σ with radially normalized ICO, , or ΣD values. For all galaxies aside from NGC 6946, the correlations are positive, in the sense that the conversion factor is higher where there is more H i and dust or more CO emission. NGC 6946 shows negative correlations with all of these parameters.
4.6.1. αCO versus Metallicity
Metallicity has been suggested by several theoretical and observational studies to be an important driver for αCO variations. Unfortunately, metallicity measurements in nearby galaxies are often very uncertain and subject to systematic errors from different calibrations and techniques. In Figure 8, we show our αCO measurements as a function of metallicity from the PT05 calibration (middle left panel). Our measurements span ∼0.5 dex in metallicity with no statistically significant trend in αCO. One possible reason for the lack of a clear trend in this figure is that we have combined metallicity measurements obtained with different techniques. In addition, many of the galaxies in our sample lack constraints on possible gradients.
To explore any metallicity trends that may be washed out due to systematic effects when combining metallicities from different sources, we isolate a sample of galaxies with uniformly determined metallicities from M10 and plot those separately in Figure 10. We have eliminated galaxies whose metallicities have been determined from integrated spectrophotometry (those listed as "M10 Table 9" in Table 3) because the drift scan observations were not always along angles that allow a robust gradient measurement. We also isolate our highest confidence αCO measurements by showing only those with uncertainties less than 0.3 dex (a factor of ∼2). We show metallicities with both the PT05 and KK04 calibrations for comparison.
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Standard image High-resolution imageIn general, there is a slight negative correlation of αCO with metallicity for this subsample. With the PT05 calibration, we find a RC coefficient of r = −0.2, which is 3.8σ from the null result given the number of measurements. Using the KK04 metallicities, we find r = −0.1 at 2.0σ from the null result. If we remove the S/N cut on the αCO measurements, the correlations in both PT05 and KK04 essentially disappear, yielding results that are less than 1σ from the null result.
The weakness of the correlation between αCO and metallicity suggests that in the regions of the galaxies we are studying, metallicity may not be the primary driver of αCO variations. Along these lines, it is interesting to note the contrast between a galaxy like NGC 6946, which has a relatively shallow metallicity gradient, and galaxies like NGC 0628 and 3184, which are thought to have much steeper gradients. NGC 6946 has αCO values spanning a range of an order of magnitude, while NGC 0628 and 3184 have much smaller ranges—the opposite of what we would expect if their metallicity gradients were the dominant factor controlling αCO.
4.7. Properties of the Full-sample DGR Solutions
In the Appendix, we show the measured DGR for all galaxies and solution pixels in figures similar to Figure 3. The DGR we report is the mean value for all of the individual sampling points in a solution pixel. Generally, the scatter in the DGRi values within a solution pixel is small (<0.1 dex). This result means that the uncertainty on the αCO value generally dominates the uncertainty on the DGR as well. Therefore, it is important to note that the errors in the DGR and αCO values are highly correlated. We assign a representative uncertainty on the DGR using the ±1σ bounds on αCO. In general, when good solutions are obtained, the DGR measurements vary smoothly across the galaxy. This result supports our key assumption that the DGR varies on scales larger than our solution pixels. The smoothness of the DGR maps can be seen by inspecting the figures in the Appendix and the results for NGC 0628 shown in Figure 3.
In Figure 11, we show a histogram of all of the measured DGR values for our galaxies that comply with our cuts in inclination and ICO. The average of our measurements treating all lines of sight equally is log(DGR) = −1.86 with a standard deviation of 0.22 dex. This finding is slightly higher than the value typically adopted for the solar neighborhood of log(DGRMW) = −2.0. Forcing all galaxies to contribute equally to the average despite differing numbers of solution pixels gives log(DGR) = −1.96. The lower scatter in the DGR measurements for all solution pixels compared to the αCO measurements, despite the uncertainty on αCO dominating the uncertainty on the DGR, is due to the contribution of H i to the total gas mass surface density. Because H i makes up some fraction of the gas mass, the DGR has a smaller possible range over which to vary compared with αCO.
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Standard image High-resolution image4.8. Correlations of the DGR with Environmental Parameters and Radius
The DGR may also vary as a function of environmental parameters. To explore any such trends, we show our measured DGR values as a function of the same tracers we have previously studied in Figure 12. We list the correlation coefficients and linear fit parameters in Table 9.
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Standard image High-resolution imageTable 9. DGR Correlation Properties
log(DGR) vs. | Correlationa | σ from | Linear Fitb | |
---|---|---|---|---|
Variable | Coeff. | Null | Offset | Slope |
r25 | −0.33 | 9.2 | −1.71 | −0.35 |
log() | +0.01 | 0.3 | −1.87 | +0.02 |
qPAH (%) | +0.00 | 0.1 | −1.85 | +0.00 |
12+log(O/H) | +0.26 | 7.3 | −6.50 | +0.55 |
log(Σ*) | +0.28 | 7.9 | −2.27 | +0.21 |
log(ΣSFR) | +0.03 | 0.8 | −1.79 | −0.03 |
Notes. These correlations are shown in Figure 8. aSpearman rank correlation coefficient. bCorrelation with metallicity using a homogeneous sample of metallicity measurements is discussed in Section 4.8.
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The DGR shows significant correlations with galactocentric radius, metallicity, and Σ*. Even with heterogeneously determined metallicities, it shows a much clearer trend with 12+log(O/H) than αCO does over the same range. A correlation of the DGR with metallicity is expected—given the high depletions of elements such as Mg, Si, Ca, and Ti in the local area of the MW, to first order the mass of dust should be proportional to the amount of heavy elements.
In Figure 13, we show the DGR as a function of metallicity for the same sample of galaxies in Figure 10. In addition to the best linear fit, shown with a dotted black line, we also plot a prediction for the linear scaling of the local MW DGR with metallicity (solid black line). The dashed lines above and below show a factor of two higher and lower DGRs. The scaling of the plot is such that it covers three orders of magnitude, the same range covered in Figure 10. It is clear that the DGR values have much less scatter than the αCO values over the same range of metallicity—a product of the limited allowable range of DGRs set by the fact that some dust is associated with H i.
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Standard image High-resolution imageThe DGR values show a stronger correlation with metallicity than the αCO values do. With the PT05 calibration, we find a RC coefficient of 0.35, which is significant at the 6.4σ level. For KK04, the correlation coefficient is 0.39 at 6.9σ. In a given metallicity bin, the standard deviation of the DGR values is ∼0.15 dex for PT05 and ∼0.18 for KK04. This result suggests that, on average, we should be able to predict DGRs to better than a factor of two given the metallicity in one of these calibrations. In addition, we do not see evidence for major galaxy-to-galaxy offsets in the DGR versus metallicity plots, which distinguishes the DGR and αCO behaviors; most galaxies appear to have similar slopes in the plots.
Neither the KK04 nor PT05 calibration values fall directly along the line of the scaled MW DGR. On the PT05 scale, almost all of our sample has higher DGRs for a given metallicity than the MW scaling, while the opposite is true on the KK04 scale. For purposes of scaling the MW metallicity, we have used strong-line abundance measurements calculated from the integrated spectrum of the Orion Nebula.
The best linear fit to the data is shown with a dotted line in both the PT05 and KK04 panels. This fit is parameterized by the following equation, where uncertainties have been determined using bootstrapping:
For the PT05 measurements, we find the following constants:
For the KK04 measurements, the constants are:
In these equations, the constant c is the mean metallicity of the sample of points. We use this parameterization in order to avoid covariance in the offset (a) and slope (b). In both cases, the slope is below unity. It can be seen in Figure 13 that the flatter-than-unity slope is mainly due to NGC 3184 (blue stars). Leaving this galaxy out of the fits produces slopes of 1.13 ± 0.10 and 1.01 ± 0.11 for the PT05 and KK04 calibrations, respectively. Omitting this galaxy also increases the significance of both correlations by 1σ–2σ.
We note that it is necessary to use the same strong-line metallicity calibration that we have (i.e., KK04 or PT05) in order to predict the DGR (or αCO) using our fits. To the extent that applying our DGR(Z) relation is merely an interpolation over a given metallicity range, there is relatively little uncertainty introduced in the process. Any systematic errors in the metallicity scale itself are minimized if the same scale is used in the calibration and the application.
5. COMPARISON TO THE LITERATURE
5.1. Measurements of αCO in the Milky Way and Nearby Galaxies
The local region of the MW is seen to have a conversion factor close to αCO = 4.4 M☉ pc−2 (K km s−1)−1. This standard value has been recovered to within a factor of two by various techniques: γ-ray measurements (Digel et al. 1996; Abdo et al. 2010); virial masses (Solomon et al. 1987); and dust (Dame et al. 2001; Pineda et al. 2008; Planck Collaboration et al. 2011b). A number of studies of the Galactic center, however, have found very different answers. Using γ-ray observations, Strong et al. (2004) found evidence that αCO in the Galactic center was a factor of 5–10 lower than in the disk. Similar results using dust as a tracer for total gas mass have been found by Sodroski et al. (1995), who suggest that αCO is lower by a factor of 3–10. Dahmen et al. (1998) modeled multiple 12CO, 13CO, and C18O lines and found that the standard conversion factor from the disk overestimated the molecular gas mass in the Galactic center by an order of magnitude. Thus, several independent measurements suggest that the MW has a αCO value near its center that is between 3 and 10 times lower than that in the solar neighborhood. The properties of the transition from the standard disk value to this lower number are not well constrained, although γ-rays provide some hint of a gradient (Strong et al. 2004).
The agreement among the various techniques in the Galactic center provides confidence in the resulting low αCO. On their own, each technique is subject to a number of important systematic uncertainties. For γ-ray modeling, a key limitation is our knowledge of the cosmic ray distribution. In the case of multi-line modeling approaches, it is not clear that the approximations involved adequately represent the variety of excitation conditions in the molecular gas (Mao et al. 2000; Bayet et al. 2006). Virial mass-based techniques rely on the assumption that the clouds are in virial equilibrium, with gravity opposed primarily by turbulent motions. If magnetic stresses and thermal pressures are significant, or if GMCs are actually not self-gravitating, the virial technique may fail to reflect the true conversion factor, particularly in regions like the Galactic center (e.g., Dahmen et al. 1998).
Measurements of αCO using various techniques in nearby galaxies have provided somewhat contradictory results. Virial mass studies of GMCs in nearby galaxies tend to find αCO values very similar to the MW disk (Wilson 1995; Bolatto et al. 2008), even in galaxy centers (Donovan Meyer et al. 2012) and in low-metallicity galaxies like the SMC (Bolatto et al. 2008). In contrast, a number of studies using dust-based techniques have found very high αCO values in low-metallicity galaxies, suggesting substantial amounts of "dark molecular gas" or "CO-free H2" around GMCs (Israel 1997; Dobashi et al. 2008; Leroy et al. 2009a, 2011). Leroy et al. (2011) used dust to trace the total amount of gas and determine αCO for the major galaxies of the Local Group. Their results suggested that (1) at low metallicity, αCO can be well above the standard MW value, (2) in the central few kiloparsecs of M31, the conversion factor was slightly lower than the standard value, and (3) the 10 kpc ring of M31, M33, and the LMC (which collectively span ∼0.5 dex in metallicity) all showed αCO values in agreement with the MW value. Studies of the centers of several nearby galaxies with "large velocity gradient" (LVG) or related modeling have found evidence for αCO up to an order of magnitude lower than the MW value (e.g., Weiß et al. 2001; Israel 2009a, 2009b).
The study presented here is the first to create maps of αCO in galaxies outside the Local Group. Therefore, we are able to study αCO across a range of environments and connect the various trends that have been found in previous works. We find that for ICO > 1 K km s−1, αCO is relatively constant for a range of radii and metallicities in galaxies. In the central ∼kiloparsec, we observe that galaxies often show a lower-than-average αCO value, sometimes by up to factors of 10. These low αCO values we find in several galaxy centers are not unprecedented, given the results from multi-line modeling studies and the evidence that the Galactic center shows a similar depression. Our lowest metallicities are still above the transition abundance seen by Leroy et al. (2011), where galaxies in the Local Group began to display much higher αCO (i.e., 12+log(O/H) ≲ 8.2). The picture that emerges from the synthesis of these literature results is one where αCO is generally around the standard MW value with a factor of ∼2 variability in the disks of galaxies, in the regime where CO is bright and metallicity is greater than ∼1/2 Z☉, with some galaxies showing lower αCO in their central kiloparsec.
5.2. Direct Comparison of αCO with Virial Mass Measurements
In several cases, our αCO measurements overlap with previous 12CO J = (1–0) virial mass based studies. Bolatto et al. (2008) derived GMC properties and virial masses for NGC 2976 and 3077. Their results for NGC 3077 are in good agreement with previous studies by Meier et al. (2001) and Walter et al. (2002). Recently, Donovan Meyer et al. (2012) and Donovan Meyer et al. (2013) determined αCO in the central regions of NGC 6946 and 4736, respectively, using virial masses. In Table 10, we provide a summary of the galaxies in our sample with existing literature measurements. Figure 14 shows a comparison between these literature virial mass-based αCO measurements with the values derived in this study. In almost all cases, we find a lower αCO using the dust-based technique than the virial mass technique.
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Standard image High-resolution imageTable 10. Literature αCO Measurements
Galaxy | Regan et al. (2001) | 3σ Below MW | Literature αCO Measurements | |
---|---|---|---|---|
Central Excess? | αCO (This Study) | Type | Reference | |
NGC 0628 | N | N | ||
NGC 2976 | ... | N | VM | B08 |
NGC 3077 | ... | N | VM | B08 |
NGC 3351 | Y | Y | ||
NGC 3521 | N | N | ||
NGC 3627 | Y | Y | ||
NGC 4321 | Y | Y | ||
NGC 4631 | ... | N | ML | I09 |
NGC 4736 | Y | Y | VM | DM13 |
NGC 5055 | Y | Na | ||
NGC 6946 | Y | Y | VM, ML | DM12a, IB01, MT04, W02 |
NGC 7331 | N | N | ML | IB99 |
Notes. VM: virial mass; ML: multi-line modeling. a2.6σ below MW αCO. References. B08: Bolatto et al. (2008); DM12a: Donovan Meyer et al. (2012); DM13: Donovan Meyer et al. (2013); I09: Israel (2009b); IB99: Israel & Baas (1999); IB01: Israel & Baas (2001); M01: Meier et al. (2001); MT04: Meier & Turner (2004); R01: Regan et al. (2001); W02: Walsh et al. (2002).
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For NGC 2976, Bolatto et al. (2008) found conversion factors ∼4 times larger than the MW value, on average. Almost all of our measurements for NGC 2976 show αCO being consistent with the MW value, within their uncertainties. The central solution pixel has αCO a factor of 4–5 below the MW value. In contrast, the virial mass and dust-based techniques are in agreement for NGC 3077, both returning a conversion factor consistent with that of the MW. The center of NGC 6946 stands out in our study as a place with a particularly low αCO. However, virial mass measurements find αCO more consistent with the MW value. Figure 14 illustrates that the discrepancy decreases with radius for NGC 6946—many of the points with galactocentric radii closer to r25 ∼ 0.2 agree with our dust-based measurements. We will discuss the discrepancy between the virial and dust-based αCO values in galaxy centers further in Section 6.3. It is interesting to note that the normalcy of NGC 3077, currently undergoing a starburst, compared to the also highly star-forming centers of 4736 and 6946, suggests that conditions other than just high star-formation surface density must contribute to determining αCO.
5.3. Direct Comparison with Multi-line Modeling Techniques
The center of NGC 6946 has been observed extensively in molecular gas lines and modeled in a variety of ways. Israel & Baas (2001) modeled 12CO and 13CO lines plus [C i] (492 GHz) observations and found a conversion factor ∼10 times lower than the MW value in the center. Using LVG modeling of multiple CO isotopomers including 12C18O, Walsh et al. (2002) found a conversion factor 4–5 times below the MW value. Similarly, Meier & Turner (2004) used an LVG analysis of C18O observations, in addition to multiple CO lines, to argue that the central region had a conversion factor four times below the MW value. All of these studies suggest a central αCO between 4–10 times lower than the MW value, in good agreement with what we observe with dust, but in contrast with the virial mass results.
Several other galaxies in our sample have been modeled with multi-line techniques, however they are at high inclination and therefore do not have reliable αCO measurements from our work. Israel (2009b) used multiple 12CO and 13CO lines plus [C i] (492 GHz) observations toward the central region of NGC 4631 to constrain αCO and found a value six times lower than the standard MW value. Similarly, Israel & Baas (1999) argued for αCO ∼ 5 times lower than the MW value in the center of NGC 7331. In both of these highly inclined galaxies, we find αCO a factor of two or more higher than the MW αCO. This result is due to the failure of our technique at high inclinations.
5.4. Comparison with CO Exponential Disk Profiles
Regan et al. (2001) found that approximately half of their sample of galaxies observed in the BIMA SONG survey showed excess CO emission in their centers compared to the extrapolation of their best-fit exponential disk profile. They argued that this result could be due to enhanced reservoirs of molecular gas in the centers or a change in the conversion factor. Table 6 lists the central excess classification for the galaxies in our sample studied by Regan et al. (2001). Indeed, we find that in every case where these authors found excess CO above the exponential profile, we find a conversion factor significantly below the MW value. Conversely, for the three galaxies we have observed and that they found to not have an excess, we find conversion factors consistent with the MW value or slightly higher. Similar results are found when comparing with the radial profiles determined from the HERACLES CO maps we utilize in this study (see radial profiles in Schruba et al. 2011). In general, the offset between the central αCO and galaxy average αCO from our measurements is similar in magnitude to the excess observed at the centers compared to the extrapolated exponential disk profile.
6. DISCUSSION
6.1. Drivers of αCO Variations
In the following, we explore the correlations or lack thereof between αCO and parameters that may influence it. Since our resolution elements are large compared to an individual GMC, our αCO value is an average over a population of GMCs, including any molecular gas that may be in a more diffuse phase and not in self-gravitating clouds.
For an individual, self-gravitating, turbulence-supported molecular cloud, there are several key parameters that influence αCO: the density and temperature of the gas and the fraction of the mass that exists in the "CO-dark" phase (where H2 self-shields and CO is photodissociated). The general dependence of αCO on density and temperature can be illustrated using a simple model—a spherical, homogeneous cloud where self-gravity is opposed primarily by turbulence and 12CO J = (1–0) is optically thick. Following the derivation in Draine (2011),
Here, n3 is the H nucleon density nH = 103n3 cm−3 and Tex is the excitation temperature. Real molecular clouds are certainly not spherical and homogenous, but this model allows us to understand the basic dependence of αCO on density and temperature (note that simulated molecular clouds with a non-spherical, non-homogenous structure show similar basic scalings; Shetty et al. 2011). Molecular clouds with increased density will have higher αCO while clouds with increased temperature will have lower αCO.
Because CO is optically thick at solar metallicity, the abundance of C or O does not directly influence αCO. However, metallicity may indirectly influence αCO by altering the density or temperature structure of the gas, since the heating and cooling rates may be affected by metallicity or correlate with metallicity. At lower metallicities, the transition between ionized and neutral carbon to CO may shift relative to the H i/H2 transition due to a lack of dust shielding, leading to layers of "CO-dark" H2 (Tielens & Hollenbach 1985; van Dishoeck & Black 1988; Wolfire et al. 1993; Kaufman et al. 1999; Bell et al. 2006). αCO will increase when there are significant amounts of gas in these layers. Recent work by Wolfire et al. (2010) used PDR modeling and a spherical model for a turbulent molecular cloud to study variations in the conversion factor. These authors found that the "dark molecular gas" fraction (i.e., the fraction of the molecular cloud mass where H2 exists but CO is photodissociated) depends primarily on the extinction through the cloud or the DGR. Studies of simulated molecular clouds have also found a dependence of αCO on extinction through the cloud (Glover & Mac Low 2011).
The simple model we have described above assumes that the cloud's self-gravity is balanced by turbulence. If there are other forces that contribute to the virial equation, αCO may be altered. For a self-gravitating cloud, an increase in the pressure on the surface of the cloud will lead to a larger velocity dispersion. Because CO is optically thick, the amount of emission that "escapes" in the CO line is directly tied to the velocity dispersion of the cloud and increasing the velocity dispersion increases the CO emission for the same mass of H2. Therefore, if a self-gravitating cloud were subject to significant external pressure, we would expect a lower αCO. Conversely, if magnetic fields play an important role in supporting the cloud, this effect would lower the velocity dispersion and raise αCO. In ultra-luminous infrared galaxies (ULIRGs), the molecular gas may not be in individual self-gravitating clouds, but instead in a large-scale molecular medium where stellar mass contributes to the gravitational potential (e.g., Downes & Solomon 1998). In this case, the velocity dispersion is larger than what would be expected from the gas mass alone and the CO emission is enhanced for a given gas mass (resulting in a lower αCO).
In a ∼kiloparsec region of a galaxy, many individual molecular clouds will be averaged together in our measurement. Therefore, another factor that could contribute to the variation of our measured αCO is changes in the cloud populations. In addition, any significant component of diffuse CO emission would be included as well. Several studies have suggested that CO emission from diffuse gas may not be negligible, even in the local area of the MW (Liszt & Lucas 1998; Goldsmith et al. 2008). Interestingly, it appears that locally, αCO is similar in diffuse molecular gas and self-gravitating GMCs (Liszt et al. 2010). Recent work by Liszt & Pety (2012) has shown that under differing environmental conditions, the conversion factor appropriate for diffuse gas can vary substantially. Therefore, depending on the amount of diffuse molecular gas and the local conditions in a galaxy, αCO may be very different from what is observed in the local area of the MW. The contribution of diffuse molecular gas with a different αCO has been cited previously as a cause for discrepancies between different techniques for measuring αCO in M51 (Schinnerer et al. 2010).
To summarize our theoretical expectations, αCO measured in ∼kiloparsec regions of nearby galaxies can vary as a function of environment for many reasons: changes in the excitation temperature and density of the gas or contributions from pressure or magnetic support in self-gravitating clouds; envelopes of "CO-dark" gas; changes in the molecular cloud population; or contributions from diffuse CO emission. Unfortunately, directly measuring temperature, density, and velocity dispersion in large samples of extragalactic GMCs is challenging due to the need to resolve individual clouds in multiple molecular gas emission lines. Therefore, we are left with more indirect tracers of changes to the GMC properties. In Section 4.6, we examined the correlation of αCO with , qPAH, metallicity, Σ*, ΣSFR, ΣD, and galactocentric radius.
The average radiation field , measured from the dust SED, could influence αCO through the gas excitation temperature. If photoelectric heating dominates over other heat sources (e.g., cosmic rays) at the τCO ∼ 1 surface, then the intensity of the radiation field may play a role in determining Tex (Wolfire et al. 1993). Likewise, qPAH and metallicity could both influence the efficiency of the photoelectric effect (Bakes & Tielens 1994; Röllig et al. 2006), thereby changing the heating rate. We expect that ΣSFR should be responsible for higher in many regions. Enhanced SFRs leading to higher radiation field intensities has been suggested as the explanation for the observed high αCO in several outer-disk molecular clouds in M33 (Bigiel et al. 2010). If the gas excitation temperature were affected by the radiation field or photoelectric heating, we would expect negative correlations (i.e., lower αCO at higher , ΣSFR, qPAH, etc.). The correlations we observe between αCO and , qPAH, and ΣSFR are generally weak. and αCO show the strongest association and the slope of the trend is negative, with lower αCO at higher . This result is consistent with the expectation of higher radiation field intensities leading to warmer molecular gas temperatures, but the correlation is weak and other variables may play a more important role.
We see a weak trend of αCO with metallicity. Since our observations are limited to regions with metallicities similar to or higher than that of the MW, we may not expect to see a strong correlation between αCO and metallicity. The fraction of gas mass in the layer where CO is photodissociated is predicted to be ∼30% at the MW metallicity/DGR (Wolfire et al. 2010). Thus, increasing the DGR should only have a minimal effect on the conversion factor at MW metallicity and above. To illustrate this point, in Figure 15 we plot our αCO measurements as a function of metallicity and overlay the Leroy et al. (2011) Local Group measurements and the models of Wolfire et al. (2010) and Glover & Mac Low (2011). The model predictions are normalized to αCO = 4.4 M☉ pc−2 (K km s−1)−1 at the MW metallicity (i.e., 12+log(O/H) = 8.5 in PT05 and 8.8 in KK04; from the Orion Nebula). Both models assume a linear scaling of the DGR with metallicity and a fixed gas mass surface density for molecular clouds. The model predictions are discussed in detail in Leroy et al. (2013). In both calibrations, our measurements do not extend into the regime where "CO-dark" H2 dominates αCO. We note that an investigation of the αCO–DGR relationship using our results would require taking into account the strong correlation of the uncertainties in these parameters.
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Standard image High-resolution imageThe strongest correlation we observe for αCO is that with Σ*. This correlation is the only one that is stronger than the correlation of αCO with galactocentric radius r25. In essence, our definition of r25 is based on a scale length of the stellar disk, defined by a B-band surface brightness, so it is possible the stronger correlation of αCO with Σ* is due to it being a better proxy for the disk scale length than r25. In addition, of the environmental parameters we have available for our analysis, Σ* is the most straightforward to measure and may show the smallest systematic uncertainties. αCO/Σ* may be the strongest correlation simply because the other parameters are more uncertain. The question remains, however, as to why αCO would correlate with the stellar mass surface density. There are a number of possibilities: pressure contributions to GMC virial balance, enhanced fractions of diffuse CO emission correlated with ISM pressure, changes to the population of GMCs, or other effects. We do not speculate here about what causes this correlation, but rather note that observations of multiple molecular gas lines at GMC resolution will help understand these trends and are possible with ALMA.
Although we see some evidence for weak correlations between αCO and environmental variables, it is not possible with this dataset to distinguish the cause of these variations. Our primary result is that in regions with ICO > 1 km s−1 in these galaxies, αCO is mostly insensitive to environment except in the central regions. This result may be due to our limited S/N for each individual αCO measurement plus the relatively small range of environmental conditions we probe. Another possibility is that in the disks of most galaxies, the properties of molecular gas are insensitive to environment because most of the gas resides in molecular clouds that are not under significant external pressure or subject to enhanced turbulence or magnetic fields. The conversion factor appropriate for such clouds should be similar to the standard MW value.
6.2. Comparison with Galaxy Simulations
Because of the resolution of our observations, our measurements average over a population of molecular clouds. This result means that environmental variations in the cloud population can also be responsible for changes in αCO. Therefore, it is interesting to compare our results to what has been found with galaxy simulations, despite the fact that these simulations are forced to adopt a sub-grid model that prescribes αCO for unresolved clouds. In Figure 16, we show our measured αCO values as a function of the average ICO in each solution pixel. Due to our completeness cut, we have no points below 1 K km s−1. The mean and standard deviation of the αCO measurements in bins of 0.25 K km s−1 are shown with black circles and error bars.
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Standard image High-resolution imageOverlaid on Figure 16 we show the predictions of two recent simulations. Feldmann et al. (2012, F12) couples full galaxy simulations with the Glover & Mac Low (2011) cloud-based conversion factor predictions assuming a fixed gas temperature and either a constant line width of 3 km s−1 or a virial scaling. The Narayanan et al. (2012, N12) predictions include sub-grid semi-analytic models for the chemical and thermal state of the gas and dust. In the N12 models, the temperature of the molecular gas is not fixed and depends on heating by cosmic rays and, in dense regions, on energy transfer with dust. For both models, it is necessary to adopt a filling factor or clumping correction due to the difference in resolution between the simulations and our observations. The simulations of F12 and N12 both have ∼60–70 pc resolution, so we apply the same correction to both. For purposes of comparing with the trend of our observed αCO as a function of CO integrated intensity, we have adopted a filling factor correction of three. This correction factor is larger than purely the ratio of the resolutions because our beam will contain more than one molecular cloud. Verifying that this absolute scaling is correct would require a more detailed investigation that is beyond the scope of this paper.
We find that the predicted trends of αCO with CO integrated intensity from N12 and F12 match the average observed behavior well, although both underpredict αCO in the central regions of some galaxies. There is considerable scatter around this trend, however. F12 argue that on ∼kiloparsec scales metallicity is the primary driver of the conversion factor variations. This metallicity dependence reflects, to first order, the Glover & Mac Low (2011) dependence between αCO and extinction through the cloud with the addition that F12 assume a metallicity-dependent DGR. Our αCO results do not show a strong dependence on metallicity, but may not extend to low enough metallicities to clearly distinguish such variations. N12 do see a decrease in αCO in regions with high SFR surface densities due to enhanced gas temperatures and velocity dispersions, similar to what we have found in some galaxy centers.
6.3. Low Central αCO and Discrepancies with Virial Mass Based Measurements
For some galaxy centers in our sample, we measure αCO values lower than the typical MW value by factors of 5–10. Interestingly, the virial mass-based αCO measurements for several of these regions do not agree with the values found here, instead recovering αCO values close to that of the MW. From Figure 14, we found that the discrepancy between virial mass and dust-based αCO decreases with radius for NGC 6946—suggesting that this discrepancy is a property of the galaxy centers rather than an issue with the resolution of the virial mass techniques (which tends to be comparable to the size of the GMCs). For NGC 6946, results of multi-line modeling studies are generally in much better agreement with our results. In the following, we discuss processes that could lower αCO measured from dust and multi-line modeling techniques, while leaving virial mass-based αCO values similar to those of the MW.
For self-gravitating GMCs, all three techniques should derive a lower αCO if the gas excitation temperature were changing independently of the other variables. In contrast, if the velocity dispersion of the cloud changed due to external pressure or additional sources of turbulence, the virial and dust techniques could arrive at different results. In such a situation, the measured line width would suggest a larger virial mass and the cloud's CO emissivity would also increase. Thus, one could derive a conversion factor similar to the MW value from the comparison of CO to virial mass since both have increased. Oka et al. (1998a) have suggested that external pressure in the Galactic center can account for up to an order of magnitude change in the conversion factor. However, Donovan Meyer et al. (2012) found that GMCs in NGC 6946 did not generally show enhanced velocity dispersions at a given size or luminosity, in contrast to the Galactic center clouds identified by Oka et al. (1998b). At the resolution of our CO maps, we cannot distinguish between changes in GMC internal velocity dispersion (which would affect αCO) and changes in the velocity dispersion within the population of clouds, so we cannot test whether there is enhanced velocity dispersion in GMCs with our measurements.
It is possible that molecular gas in the centers of some galaxies is not in self-gravitating GMCs. If that is the case, the velocity dispersion may reflect other hydrodynamical processes and the virial mass estimate will be incorrect. For instance, if the molecular gas is not in GMCs but rather in a larger-scale molecular medium that is gravitationally bound to the stars and gas, the velocity dispersion will be larger and more CO emission will be produced for a given amount of gas. This explanation has been suggested by Downes et al. (1993) and Downes & Solomon (1998) to explain the properties of molecular gas in the nuclear disks of ULIRGs (see also recent work by Papadopoulos et al. 2012). Another option is a contribution to the CO emission from diffuse molecular gas, which could potentially have a lower αCO than GMCs (Liszt et al. 2010).
The dust-based and multi-line modeling αCO results may agree better than the virial results in galaxy centers because they do not assume a relationship between the velocity dispersion and the mass of molecular gas, which would cause issues in the cases outlined above. At the moment, only NGC 6946 (out of our i < 65° galaxies) has both virial and multi-line modeling results. In the other galaxies, we may be able to find some indication of how optical depth, excitation, and velocity dispersion affect αCO by examining the ratios of 12CO and 13CO lines. A. Usero et al. (in preparation) present measurements of 13CO and 12CO lines toward regions of several HERACLES galaxies. Selecting all of their pointings toward the disks of galaxies in our sample (in regions above our ICO and inclination cuts), the uncertainty weighted mean of R12/13 = 12CO J = (1–0)/13CO J = (1–0) is 8.24 ± 0.11. The only galaxy centers with 13CO measurements are NGC 0628, 3184, 5055, and 6946. NGC 0628, 3184, and 5055 show R12/13 values consistent with or slightly lower than the average disk value. NGC 6946, on the other hand, has R12/13 = 18.53 ± 0.81. The high R12/13 for the center of NGC 6946 has been noted in several previous studies (Paglione et al. 2001; Israel & Baas 2001; Meier & Turner 2004).
6.4. Dust-to-gas Ratio
As shown in Figures 12 and 13, we observe a good correlation of the DGR with metallicity. Unlike most previous studies of the DGR resolved within galaxies, we made no assumption about αCO in determining these values. Although we do not probe a wide range of metallicity due to the limitations on CO S/N, it is clear in Figure 13 in particular that the DGR is correlated with metallicity with less than a factor of two scatter over 0.5 dex in metallicity. A linear dependence of the DGR on metallicity suggests a constant fraction of heavy elements are locked up in dust grains. Chemical evolution and dust life-cycle models have varying predictions for the dependence of the DGR on metallicity (Dwek 1998; Lisenfeld & Ferrara 1998; Hirashita et al. 2002). Most of the dramatic differences between the models, however, occur at lower metallicities and observations of dwarf galaxies may provide more leverage on distinguishing between models (e.g., Herrera-Camus et al. 2012).
6.5. Recommendations on Choosing αCO
Due to the requirements on CO S/N to apply the technique we have used, our measurements only tell us about αCO above ICO = 1 K km s−1 in the galaxies we have targeted. Generally, this requirement limits us to the inner parts of galaxies (<r25), where metallicities are comparable to those in the MW disk. However, these are the regions where H2 contributes most significantly to the total gas mass (Schruba et al. 2011), so applying our conversion factor results to unresolved galaxies should work reasonably well for recovering the total H2 mass. A forthcoming paper extending our study to the H i dominated regions of the KINGFISH galaxies will test this assertion. Note that our recommendations are only applicable to spiral galaxies with metallicity similar to that of the MW.
For an unresolved galaxy, we recommend adopting our galaxy-based average αCO of 3.1 M☉ pc−2 (K km s−1)−1 with uncertainty of 0.3 dex (a factor of ∼2). These values are the mean and standard deviation of the average value for all galaxies with inclinations less than 65°.
In dealing with resolved galaxies, we recommend adopting a flat radial αCO profile for regions with ICO > 1 K km s−1, except in the central ∼0.1r25, where the average αCO is a factor of two lower. When dealing with a single galaxy, our average radial profile from Figure 7 suggest that the αCO values have ∼0.2 dex of scatter in each radial bin (0.3 dex for the central bin). Therefore, for studies of molecular gas within a single galaxy, the relative values of αCO adopted from this profile have a factor of ∼1.5 uncertainty. When comparing resolved galaxies, it is necessary to further recognize that the absolute normalization of the radial profiles, i.e., the galaxy average value, has an additional 0.3 dex uncertainty.
In the case where additional information about the galaxy is available, such as profiles of stellar mass surface density, SFR surface density, or line ratios of 12CO (2–1)/(1–0) or 12CO/13CO, we suggest using these maps to pick out regions that may have αCO values very different from the mean. These regions have Σ* ≳ 1000 M☉ pc−2, ΣSFR ≳ 0.1 M☉ yr−1 kpc−2, or R21 ≳ 1 at our working resolution of ∼1 kpc. In these regions, αCO can be 5–10 times lower than the MW αCO, and are often systematically lower than the average radial profile.
7. SUMMARY AND CONCLUSIONS
The availability of high angular resolution far-IR maps from the Herschel Space Observatory and sensitive 12CO J = (2–1) and H i maps has recently allowed us to trace dust and gas mass surface densities in nearby galaxies on ∼kiloparsec scales. On these scales, we expect (and have verified) that the DGR is approximately constant. Therefore, we are able to combine the dust mass surface density maps with matched resolution CO and H i data to solve simultaneously for αCO and the DGR. The solution technique finds the αCO that best minimizes the scatter in the DGR values in ∼kiloparsec regions across the galaxies. We have performed a thorough investigation into the efficacy of this technique, using data from the KINGFISH key program on Herschel, the large IRAM 30 m survey HERACLES, and the THINGS H i survey with the VLA. Our tests show that above ICO ∼ 1 K km s−1, we reliably achieve accurate solutions for αCO. We have used a fixed ratio between the (2–1) and (1–0) lines to present our αCO results on the more typically used 12CO J = (1–0) scale and have shown using literature measurements that variations in the line ratio do not affect our results in these galaxies.
We find that the average αCO for the galaxies in our sample is 3.1 M☉ pc−2 (K km s−1)−1. This value is slightly lower than the MW αCO = 4.4 M☉ pc−2 (K km s−1)−1, but the MW value is well within the standard deviation of our measurements. Treating all 782 solutions independently (instead of weighting each galaxy equally), we find αCO = 2.6 M☉ pc−2 (K km s−1)−1 with 0.4 dex standard deviation. In all averages, we have removed galaxies with inclinations higher than 65° since our solution pixel samples gas along the line-of-sight with a range of DGRs and therefore does not conform to our main assumption—that the DGR is constant in the solution pixels.
Within the galaxies, we observe a relatively flat αCO profile as a function of galactocentric radius aside from in the galaxy centers. Normalizing each galaxy by its average αCO, the average galaxy shows a factor of ∼2 lower αCO in its center. In several galaxies, this central value can be factors of three or more lower than the galaxy average. In several notable cases, the central αCO value is factors of 5–10 lower than the standard MW αCO = 4.4 M☉ pc−2 (K km s−1)−1.
We have investigated the correlations between αCO and environmental parameters in an attempt to isolate factors that drive variations in αCO. The strongest correlation we find is between αCO and stellar mass surface density (Σ*). If the strength of this correlation relative to the other parameters is real and not due to issues with measuring the other parameters, there are a number of possible explanations for why αCO should depend on stellar mass surface density. These explanations include the influence of ISM pressure on both molecular clouds and a more diffuse molecular medium. Distinguishing among these possibilities will require ALMA observations that resolve individual GMCs in multiple molecular gas lines across a range of extragalactic environments.
We do not observe a strong correlation between αCO and metallicity in our galaxies. In the range of metallicities we have sampled, this conclusion is not unexpected. The abundance of C or O does not play a major role in determining αCO at these metallicities since CO is optically thick in molecular clouds. The metallicity primarily influences αCO through the effects of dust shielding (due to the dependence of the DGR on metallicity). Models and simulations have suggested that dust shielding can influence the amount of gas in "CO-dark" layers of GMCs, but at MW metallicity, only ∼30% of the gas is in this layer. At lower metallicities, a strong dependence of αCO on metallicity has been observed using the same technique we employ (Leroy et al. 2011).
In the centers of several galaxies, we find αCO values 5–10 times lower than that of the MW αCO. These regions are also significantly below the average αCO for their galaxy. Comparison of our measured αCO with values from the literature shows good agreement between our dust-based results and multi-line modeling results. In contrast, our αCO values in these regions can be much lower than αCO determined from virial mass-based techniques. The discrepancy with virial mass measurements becomes smaller at larger galactocentric radii, suggesting this discrepancy is a particular property of the gas in galaxy centers. At the resolution of our observations, the central region with low αCO is unresolved (≲kiloparsec). We suggest several explanations for the low αCO value and the fact that it is not reflected in virial masses: ISM pressure contributions to GMC virial balance, increases in molecular gas temperature, and/or a more diffuse molecular medium similar to what is found in ULIRGs. With the limited amount of 13CO and other molecular line observations in this region, it is not possible to distinguish among these scenarios, but NGC 6946 at least shows some evidence for lower CO optical depth toward its center. As explored in Leroy et al. (2013), these galaxy centers show enhanced star-formation efficiencies when we apply our αCO, close to what is seen along the "starburst sequence" in ULIRGs (e.g., Daddi et al. 2010).
In addition to αCO, we also simultaneously measure the DGR in all of our regions. On average, we find log(DGR) = −1.86 when all solution pixels are treated equally, with a standard deviation of 0.22 dex. When we force each galaxy to contribute equally, the average is essentially indistinguishable from the MW DGR. Unlike αCO, the DGR is well correlated with metallicity, with a slope slightly shallower than linear (although this slope is mainly due to NGC 3184 being offset from the main trend; removing this object from the sample produces a slope consistent with a linear relation). The approximately linear dependence of the DGR on metallicity agrees with the predictions of dust evolution models, but our measurements do not cover a wide enough metallicity range to distinguish among them.
The results presented here suggest a picture where αCO is slightly lower than the typical value of 4.4 M☉ pc−2 (K km s−1)−1 in the disks of most galaxies, and mainly constant as a function of radius despite changes in metallicity, radiation field intensity, and SFR surface density. Galaxy centers appear to be a different regime, where external pressure or changes in the character of molecular gas (i.e., mostly confined to self-gravitating GMCs versus a more diffuse molecular medium) may bring about large changes in αCO. Through the galaxy, however, the DGR appears to be an approximately linear function of metallicity. The simple behavior of the DGR provides a unique tool to study the ISM in nearby galaxies, if we can obtain measurements of metallicity gradients with trustworthy calibration.
We thank the referee for useful comments that helped to improve the quality of the manuscript. K.S. thanks R. Shetty, S. Glover, R. Klessen, D. Narayanan, and A. Stutz for helpful conversations. The authors thank R. Feldmann and N. Gnedin for helpful comments regarding the comparison of our measurements to their simulations. K.S. is supported by a Marie Curie International Incoming Fellowship. A.D.B. wishes to acknowledge partial support from a CAREER grant NSF-AST0955836, NASA-JPL1373858, and from a Research Corporation for Science Advancement Cottrell Scholar award.
This work is based on observations made with Herschel. Herschel is an ESA space observatory with science instruments provided by European-led Principal Investigator consortia and with important participation from NASA. PACS has been developed by a consortium of institutes led by MPE (Germany) and including UVIE (Austria); KU Leuven, CSL, IMEC (Belgium); CEA, LAM (France); MPIA (Germany); INAF-IFSI/OAA/OAP/OAT, LENS, SISSA (Italy); IAC (Spain). This development has been supported by the funding agencies BMVIT (Austria), ESA-PRODEX (Belgium), CEA/CNES (France), DLR (Germany), ASI/INAF (Italy), and CICYT/MCYT (Spain). SPIRE has been developed by a consortium of institutes led by Cardiff University (UK) and including University of Lethbridge (Canada); NAOC (China); CEA, LAM (France); IFSI, University of Padua (Italy); IAC (Spain); Stockholm Observatory (Sweden); Imperial College London, RAL, UCL-MSSL, UKATC, University of Sussex (UK); and Caltech, JPL, NHSC, University of Colorado (USA). This development has been supported by national funding agencies: CSA (Canada); NAOC (China); CEA, CNES, CNRS (France); ASI (Italy); MCINN (Spain); SNSB (Sweden); STFC (UK); and NASA (USA). HIPE is a joint development by the Herschel Science Ground Segment Consortium, consisting of ESA, the NASA Herschel Science Center, and the HIFI, PACS and SPIRE consortia. This research has made use of the NASA/IPAC Extragalactic Database (NED) which is operated by the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration. This research has made use of NASA's Astrophysics Data System Bibliographic Services.
APPENDIX A: TECHNIQUE FOR SIMULTANEOUSLY DETERMINING THE DGR AND αCO
Prior to choosing the technique described in Section 3, we explored a variety of possible ways to simultaneously constrain the DGR and αCO. The various techniques represent, in essence, different ways to judge how uniform the DGR is in the region in question, at any given value of αCO. After defining these variations on the essential technique, we construct simulated datasets with a known αCO and DGR and realistic statistical errors and intrinsic scatter to test the solution techniques. These simulated data tests allow us to optimize the performance of the technique given the properties of our dataset.
A.1. Potential Techniques
The general procedure for finding the most "uniform" DGR in the solution pixel given spatially resolved measurements of , ΣD, and ICO is to step through a grid of αCO values, calculate the DGR at each sampling point in the solution pixel using that αCO, measure some statistic that can be used to judge how uniform the DGR values are across the region, and, finally, either minimize or maximize that statistic as a function of αCO. Below, we describe the various statistics we have tested to judge the uniformity of the DGR values in a given region. The reason we investigate all of these possible statistics is because each weights outliers differently, and it is not obvious a priori which will work best to recover the underlying αCO. For techniques that involve minimizing scatter in the DGR, we use three different statistics to measure scatter: the standard deviation (RMS), the median absolute deviation (MAD), and a robust estimator of the standard deviation from Tukey's biweight (BIW; Press et al. 2002).
- 1.Minimum fractional scatter in the DGR (FS). At each value of αCO, we calculate the DGR for all points in the region in question. We then divide each DGR value by the mean DGR in the region and measure the scatter of the resulting values (with RMS, MAD, and BIW statistics).
- 2.Minimum logarithmic scatter in the DGR (LS). At each αCO, we calculate the scatter of the logarithm of the DGR values (with RMS, MAD, and BIW). This technique is similar to the minimization of fractional scatter, but with a different weighting for the individual points. This method also throws away data points with negative values, since their logarithm is undefined.
- 3.Maximum correlation coefficient of ΣD and ΣGas (LC or RC). At each value of αCO, we compute the linear correlation (LC) and rank correlation (RC) coefficients between ΣD and Σgas = + αCOICO. The best αCO value will maximize the correlation between these two quantities.
- 4.Minimum χ2 of best-fit plane to ICO, , and ΣD (PF). The ΣD, , and values describe a plane with two free parameters. At each value of αCO, we fit a plane to the measurements to determine the DGR. The best value of αCO will be the one that minimizes the χ2 of the best-fit plane.
- 5.Minimum correlation coefficient of the DGR versus ICO/ (CHC). In this technique, we search for the αCO value that minimizes the correlation of the DGR with ICO/. This technique weights the points differently depending on how much local Σgas depends on αCO.
A.2. Definition of the "Solution Pixel" Size and Location
A key aspect of the technique we use to constrain the DGR and αCO is defining the region over which we assume there to be one value each of the DGR. Under ideal circumstances, the regions would be as small as possible given the resolution of the maps. Realistically, however, there are several considerations that must be taken into account when defining the regions, including covering an adequate range of CO/H i ratios, having enough points to measure scatter accurately, and keeping the region to ∼kiloparsec scales over which it is reasonable to assume that the DGR is indeed constant.
To complement the hexagonal, half-beam spaced grid with which we sampled the original data (i.e., our "sampling points"), we again use hexagonal spacings to define the "solution pixels" as the individual samples can be divided naturally into concentric hexagons. We tested a variety of solution pixel sizes ranging from 19-point to 271-point hexagons.
We found that 37-point solution pixels were a good compromise between size and solution quality. Because of the underlying half-beam spaced sampling grid, the 37 point solution pixel contains ∼9 independent measurements. For the next smallest possible hexagon (19-points), there are not sufficient numbers of independent measurements to reliably judge the scatter in the DGR.
In order to fully sample the map, the center of each hexagonal pixel is offset by 1/2 of the spacing from its neighbor. This technique results in the "solution pixels" not being independent—each neighboring pixel shares ∼40% of the same data (the oversampling can be exactly described as n2/(3n2 − 3n + 1) for concentric hexagons).
A.3. Test of the Solution Technique with Simulated Data
We have investigated the efficacy of the various techniques using simulated data modeled on our observations. Our goal is to identify the technique or techniques that return the most accurate values of αCO and the DGR over the range of conditions and S/N levels in our dataset. We also aim to characterize any biases in the recovered αCO as a function of input αCO and S/N. In performing these tests, it is important to model the simulated data on our real observations because the ability of the techniques to judge the DGR uniformity depends not only on the S/N of the measurements but also on the range of CO/H i ratios. Since CO and H i can be correlated, anti-correlated, or independent of each other on kiloparsec scales, depending on the state of the ISM, it is difficult to generate a reasonable set of simulated data from scratch that encompasses the range of CO/H i behaviors in the observations. Therefore, we expect the best test of the technique will come from simulated data that are closely modeled on the observations. In the following, we describe how the simulated data are generated and discuss the results of the test.
The simulated data are generated via a Monte Carlo procedure in which we randomly choose a galaxy from our sample (listed in Table 1) at SPIRE 350 μm resolution, choose a solution pixel, and create simulated data based on the selected CO, H i, and ΣD samples. For each trial, we randomly sample a range of αCO values between 0.5 and 50 M☉ pc−2 (K km s−1)−1 and intrinsic scatter per axis (evenly divided among the ICO, , and ΣD axes, for lack of better knowledge of the sources of intrinsic scatter) between 0.0 and 0.4 dex. We note that because of the properties of lognormal distributions, the scatter in the DGR is not simply the input intrinsic scatter per axis, so we approximate it after the fact using the input scatter per axis and the mean H2/H i ratio for the simulated measurements.
Our procedure is the following: (1) select the observations with the sampling described above, (2) use the ICO and measurements along with the random αCO value to create a simulated Σgas vector, (3) calculate the DGR value that preserves the average S/N level of the ΣD measurements and create a simulated, noise-free ΣD vector by multiplying the Σgas from step 2 by this DGR, (4) apply the randomly selected intrinsic scatter to each axis, and (5) add simulated measurement errors according to the observed uncertainties in the ICO, , and ΣD maps. These simulated measurements are then used as inputs to solve for αCO and the DGR using the techniques described above.
From this Monte Carlo simulation, we can then choose the technique that is the most robust (i.e., most frequently achieves a solution) and accurate (i.e., gets closest to the known input αCO). In Figure 17, we show the results of this simulation for the techniques we have outlined. The panels show (left) the mean difference between the input and recovered αCO value, (middle) the standard deviation of the difference of the input and recovered αCO, and (right) the percent of the Monte Carlo trials that achieve a solution. These values are binned in a two-dimensional space defined by the intrinsic scatter added to the simulated data and the median S/N of the simulated CO measurements.
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Standard image High-resolution imageIt is clear that the FS and LS techniques provide the least bias in the recovered αCO over the relevant range of intrinsic scatter and S/N (except for the FS_RMS, which is significantly biased at low CO S/N). The correlation coefficient (LC and RC), planefit (PF), and CO/H i correlation (CHC) techniques all provide much more limited regions with low bias in the recovered αCO, as well as having a lower fraction of solutions. In general, the MAD based techniques have slightly less bias toward the low CO S/N region, but show a larger scatter between the input and recovered αCO. Overall, we find that the LS_BIW (robust BIW mean of the logarithmic scatter) is the technique that shows the best performance in accuracy, precision, and robustness over the range of characteristics of our dataset.
In addition to helping us choose the best technique, the tests with simulated data also allow us to investigate how the measured minimum in the logarithmic scatter corresponds to the known intrinsic scatter added to the simulated data. In addition to being an interesting quantity scientifically, the measured scatter can also help us to identify which region of the parameter space a given solution falls in, thereby allowing us to judge how biased we expect it to be given our knowledge from these simulated data tests. Figure 18 shows a comparison of the known input intrinsic scatter with the measured minimum in the logarithmic scatter for the LS_BIW technique. Most of the outliers come from regions with low CO S/N. At very low levels of intrinsic scatter, the measured scatter is larger due to the influence of observational uncertainties. In general, however, the measured minimum log scatter is a very good proxy for the intrinsic scatter in the DGR.
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Standard image High-resolution imageBased on these results with simulated data, we can use the measured median CO S/N and the measured minimum of the scatter in the DGR values to predict how biased and how uncertain a given determination of αCO is for our dataset. To this end, we use the measured minimum in the DGR scatter as an estimate of the intrinsic DGR scatter (it is biased slightly higher, but this effect is minor and represents a conservative estimate of the intrinsic scatter). Then, using this value and the median CO S/N in the solution pixel, we interpolate in the grid presented in Figure 17 for "LS_BIW" to predict the bias inherent in the technique.
A.4. Testing for Bias at High CO S/N and Low
One of the key results of our work is the measurement of low αCO values in the centers of some galaxies (see Section 6.3). These locations are outliers from the average solution pixel in the sense of having high CO S/N and often a relative deficiency in . Since these locations make up a small subset of all solution pixels, our Monte Carlo simulations from the previous section may not adequately judge the bias of the technique in these regions since they are not sampled frequently enough (only 26 out of ∼900 solution pixels). We therefore perform a separate Monte Carlo simulation for the galaxy centers in order to verify that these low αCO values are not due to biases in the technique (we have demonstrated that the average pixel in the sample is not biased using the experiment in the previous section).
The results of the technique are biased if the simulation returns an αCO systematically different from the true αCO. For this test, we will define several different αCO values. First, αCO, meas is the measured value for a given solution pixel; we do not know if this measured value is biased as it is only what we have measured for that pixel given the true data. Second, αCO, in is a known αCO value we have used to generate the simulated data. Finally, αCO, out is the αCO value that we recover for αCO, in using our solution technique.
The essence of this test is that we take a range of αCO, in values and map them to their αCO, out values by generating simulated data given αCO, in and running it through our solution technique. This simulated data generation proceeds as described in the previous section and is designed to preserve the CO/H i ratio and S/N of the measurements for a given pixel. In addition to observational noise, we also add intrinsic scatter between 0.01 and 0.1 dex to the simulated data, which reflects the level of intrinsic scatter we have found in the real solutions. For each solution pixel, we generate 104 random αCO, in values that span our range of αCO = 0.1–100.
With this simulation, we can determine for any given value of αCO, out which values of αCO, in ended up there. If a solution is biased, the correspondence between αCO, in and αCO, out will not be one-to-one. For example, a bias may make us consistently recover αCO, out = 1 M☉ pc−2 (K km s−1)−1 when αCO, in = 0.1 M☉ pc−2 (K km s−1)−1.
In judging the biases of the actual solutions for our central solution pixels, we then select all of the αCO, out measurements equal to αCO, meas and find the mean and standard deviation of the αCO, in values that gave those results. In Figure 19, we show a plot of the mean and standard deviation of the relation between the αCO, in values and the αCO, meas values. This figure shows that within the uncertainties of αCOmeas, none of the central pixel measurements show a bias.
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Standard image High-resolution imageIn addition, a second check on these low central αCO, at least for NGC 6946, is shown in Figure 20 where we show the minimization curve for several techniques toward its central solution pixel. All techniques agree within their errors, highlighting the minimum at αCO ∼ −0.4. This result emphasizes that the low αCO found in the center is not an artifact of the particular technique we are using, but can be recovered via minimization of scatter in the DGR, minimization of the correlation coefficient between CO/H i and the DGR, and minimization of the χ2 of the best-fit plane to CO, H i, and ΣD.
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Standard image High-resolution imageA.5. Summary of Investigations into the Solution Technique
To summarize, we have tested a number of variations on the basic technique of finding the most "uniform" DGR in a given region by stepping through a grid of αCO values. We created simulated data with known αCO and DGR intrinsic scatter matched to the range of S/N in our dataset. Via a Monte Carlo simulation, we found the robust mean of the logarithmic scatter to be the technique that spans the range of CO S/Ns and possible intrinsic DGR scatters with the highest accuracy and rate of success. Given knowledge of the CO S/N for a region and the measured minimum of the logarithmic scatter, we can use the simulated data tests to constrain how biased our αCO measurement can be. We have also specifically checked that the central regions of galaxies, which only comprise 26 pixels out of the sample, are not biased due to their sometimes unusual CO/H i ratios. We found no significant bias for these solutions and show in addition that a variety of techniques can reproduce the low central αCO solutions, not just the minimization of the DGR scatter.
A.6. Variations in R21
In Figure 21, we show the measured CO (2–1)/(1–0) line ratio in the solution pixels we have defined for each galaxy (the black points) and in radial profiles (colored lines). The assumed R21 is shown with a horizontal solid black line and factors of two above and below that value are marked with black dashed lines. There are variations in R21, but in regions with good CO S/N (the only regions in which we will achieve good solutions) these variations are generally less than a factor of two away from the R21 we have assumed. This deviation is within the uncertainties on the αCO solutions, which typically have 0.2 dex uncertainty, at minimum.
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Standard image High-resolution imageAPPENDIX B: ATLAS OF GALAXIES AND RESULTS
In this Appendix, we present the results for individual solution pixels in all of the galaxies we have considered. In the top panels of Figure 22, we show the H i, CO, and ΣD maps at matched resolution. The circles overlaid on these figures show the central position of each of the 37-point, hexagonal solution pixels in which we determine αCO. In the middle panel of these same figures, we show on the left the αCO values in color and the associated uncertainties on the right in gray scale. Solution pixels where the solution failed are omitted. Finally, in the bottom panels of the figures, we plot the measured αCO values as a function of galactocentric radius (r25). The color of the points in this plot reflects the uncertainties on the αCO values, as shown in the gray scale color table in the middle panel.
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Standard image High-resolution imageFootnotes
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We refer to the CO-to-H2 conversion factor in mass units throughout this paper. Including a factor of 1.36 for helium, XCO = 2 × 1020 cm−2 (K km s−1)−1 corresponds to αCO = 4.35 M☉ pc−2 (K km s−1)−1. αCO can be converted to XCO units by multiplying by a factor of 4.6 × 1019.
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In converting from column densities to mass surface densities, we account for helium with a factor of 1.36. For , this factor is included in the αCO term. We apply the helium correction to as well.
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The National Radio Astronomy Observatory is a facility of the National Science Foundation operated under cooperative agreement by Associated Universities, Inc.
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Data available at http://www.caha.es/sanchez/orion/.
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We use the IDL implementation of Tukey's biweight mean (Press et al. 2002) biweight_mean.pro.