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A millennial summer temperature reconstruction for northeastern Canada using oxygen isotopes in subfossil trees

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Figure 2. Illustration of the sampling strategy. From year 1000 to 2006, cohorts are represented in red for subfossil stem segments (C0-C11), and in green for living trees (CV)
Table 1. Summary of the verification statistics for calibrations using the linear scaling and simple linear regression methods for different periods, and using the measured maximal temperature series.
Figure 4. (a) Comparison between reconstructed (i-STREC, black line) and observed (blue line) JJA maximal temperature and mean square values on the entire period of calibration
Fig. 4b). These periods are in agreement with the general knowledge of the temperature trends observed globally for the last millennium and correspond to the Medieval Climate Anomaly (MCA) and the LIA, respectively (IPCC, 2013;
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