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. Author manuscript; available in PMC: 2020 Feb 5.
Published in final edited form as: J Geophys Res Atmos. 2018 Feb 21;123(7):3704–3723. doi: 10.1002/2017JD027900

Table 2.

Summary of the Coefficients of the Linear Regression Equation

Species Bottom/Top
Middle/Top
Bottom/Middle
m b r n p m b r n p m b r n p

Na 0.36 1.74 0.98 6 < 0.01 0.09 1.09 0.23 6 0.66 0.99 0.91 0.80 6 0.06
Cl 0.42 1.51 0.99 6 < 0.01 −0.11 1.51 −0.15 7 0.75 1.16 0.68 0.90 6 0.01
NO3 0.31 1.14 0.72 6 0.11 −0.19 1.34 −0.30 7 0.51 1.13 0.27 0.94 6 < 0.01
NSS SO42− 0.22 1.07 0.75 6 0.09 −0.08 1.01 −0.42 6 0.41 0.99 0.21 0.97 6 < 0.01
MSA 0.21 0.79 0.85 6 0.03 −0.03 1.07 −0.08 7 0.86 0.61 0.43 0.97 6 < 0.01
Oxalate 0.21 2.42 0.38 5 0.53 −1.19 4.41 −0.32 5 0.60 0.76 1.58 0.35 5 0.56
NO2 0.13 0.45 0.70 6 0.12 0.15 0.86 0.24 7 0.60 0.27 0.66 0.28 6 0.59
Formate 0.18 1.37 0.39 5 0.52 −0.14 1.22 −0.47 4 0.53 0.42 1.95 0.33 3 0.79
Fe 0.23 2.27 0.49 6 0.32 −0.25 1.70 −0.50 5 0.39 1.22 0.87 0.75 6 0.09

Note. The table is an extension of Figure 7, showing the coefficients of the linear regression equation of the form y = mx + b, where x is the ratio of lower-to-higher altitude values of τ and y is the ratio of lower-to-higher altitude values for species air-equivalent concentrations. The number of data points is denoted as n. Correlation coefficients (r) and p values are also reported.