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Tree-ring stable isotopes for regional discharge reconstruction in eastern Labrador and teleconnection with the Arctic Oscillation.

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Academic year: 2021

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Figure

Fig. 1    Location of Lab 32 and  Lab 65 sites (black stars) and  hydrological stations (black  cir-cles) used for reconstruction and  validation in the lower Churchill  River region, Labrador
Fig. 2    Tree-ring δ 13 C corrected and de-trended (a) and δ 18 O de-
Fig. 3    Tree-ring δ 13 C series at
Table 1    Significant statistical correlations between the tree-ring iso- iso-topic series and hydroclimatic variables (all correlations are  signifi-cant at p < 0.05, n = 41)
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