Simulated time series (10-year means) of a changes in GDD0 and b changes in fraction of land surface covered by forest, shown as deviations from the preindustrial mean (1,000–250 yr BP). Both are calculated for the area north of 60°N. The preindustrial means for GDD0 and forest fraction are 1,287 degree days and 0.37, respectively
Averaged over the area north of 60°N, the GDD0 index decreases moderately by 210 from 1,490 to 1,280 degree days (Fig. 16 a).
Since temperature is one of the main factors controlling vegetation cover at the high northern latitudes, the shortening of the growing season is responsible for a decrease in the fractional forest cover by 0.09 (from 0.45 to 0.36, Fig. 16 b).
However, compared to the 100 km southward tree line shift found in proxy records in the MacKenzie delta, the model appears to have overestimated the response of the vegetation, as seen in the strong reduction in forest fraction in Fig. 16 a, b..
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