Extended Data Fig. 7: Regional changes in the impact of climate drivers on negative GPP extremes between the 2000–2016 and 1982–1998 study periods.
From: Increasing impact of warm droughts on northern ecosystem productivity over recent decades
The cumulative negative GPP anomalies attributed to each of the climate drivers were calculated for each period and the associated changes were then expressed as the difference between the two study periods (2000–2016 minus 1982–1998; ΔGPP). The corresponding increased (decreased) ΔGPP (expressed as negative (positive) values) between the two periods (barplots) were derived from the median of the three individual datasets. The presented error bars were estimated through the corresponding minimum and maximum of the three datasets. Regions that experienced a consistent increase in ΔGPP in all three datasets are highlighted (pink regions).
