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