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Table 2.

4D PCA results for MAGMA.

Method PC4(1) PC4(2) PC4(3) PC4(4) PC4 PC4 PC3 PC1 + PC2
12 + log(O/H) log log log(x) std. dev. proportion of variance
(PP04N2) (Mstar/M) (SFR/M yr−1)
(1) (2) (3) (4) (5) (6) (7) (8) (9)
x = MHI/M
PCA 0.920 −0.355 0.164 0.019 0.127 0.010 0.051 0.94
PPCA 0.95 ± 0.01 −0.29 ± 0.03 0.11 ± 0.03 −0.01 ± 0.01 0.14 0.01
BSPCA 0.92 ± 0.01 −0.36 ± 0.03 0.16 ± 0.03 0.02 ± 0.02 0.13 0.01
x = MH2/M
PCA 0.913 −0.378 0.133 0.079 0.124 0.010 0.051 0.94
PPCA 0.94 ± 0.01 −0.31 ± 0.03 0.09 ± 0.03 0.05 ± 0.02 0.14 0.01
BSPCA 0.91 ± 0.02 −0.38 ± 0.03 0.13 ± 0.03 0.08 ± 0.04 0.12 0.01
x = Mgas/M
PCA 0.917 −0.366 0.153 0.048 0.126 0.011 0.054 0.94
PPCA 0.95 ± 0.01 −0.24 ± 0.02 0.13 ± 0.02 −0.09 ± 0.03 0.14 0.02
BSPCA 0.91 ± 0.02 −0.37 ± 0.03 0.16 ± 0.03 0.05 ± 0.03 0.13 0.01
x = /K km s−1 pc2
PCA 0.955 −0.185 0.181 −0.147 0.117 0.007 0.027 0.97
PPCA 0.97 ± 0.01 −0.16 ± 0.04 0.13 ± 0.02 −0.13 ± 0.03 0.13 0.01
BSPCA 0.95 ± 0.01 −0.18 ± 0.04 0.18 ± 0.03 −0.15 ± 0.02 0.12 0.01

Method PC4(1) PC4(2) PC4(3) PC4(4) PC4 PC4 PC3 PC1 + PC2
12 + log(O/H) log log log std. dev. variance variance variance
(KD02) (Mstar/M) (SFR/M yr−1) (MH2/M) (a)

PCA 0.86 −0.45 0.22 0.03 0.153 0.014 0.048 0.95
PPCA 0.92 ± 0.02 −0.37 ± 0.04 0.15 ± 0.04 0.02 ± 0.02 0.17 0.02
BSPCA 0.86 ± 0.03 −0.45 ± 0.04 0.22 ± 0.04 0.03 ± 0.03 0.15 0.01

Notes. In PCA, the relative signs of the PCs are arbitrary, thus we used the same conventions for all; this has no bearing on the inversion of the equation of the PC with the least variance. Column (6) reports the standard deviation of PC4 around the hyperplane, and Cols. (7)–(9) give the proportion of sample variance contained in PC4, PC3, and the sum of PC1 + PC2, respectively.

(a)

Here MH2 was calculated with αCO according to the exponential formulation of Wolfire et al. (2010) and Bolatto et al. (2013), using the KD02 metallicities.

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