Tank et al. Dissolved C flux from circumboreal catchments

Table S1: Results of the regression analyses shown in Fig. 4.  
In all cases, the independent variable is the contribution of 
groundwater flux to total discharge.  The dependent variable 
is as noted.  r indicates the analysis of the residuals of the 
daily model results.  

LEGEND:
JN: June
AU: August
INT: Intercept
COEFF: Coefficient
p: p-value

VARIABLE      JN_INT   JN_COEFF JN_p   AU_INT   AU_COEFF  AU_p     
Permafrost    73.616   -1.874   0.017  77.958   -1.638    0.003
HCO3-, r      -5.556   0.646    0.082  -1.984   0.351     0.081
HCO3-:DOC, r  -0.673   0.119    0.283  -2.217   0.281     0.009
DOC, r        2.295    -0.855   0.112  1.574    -0.397    0.131