Fig. 1: GPP losses attributed to hydroclimatic extremes during 1982-2016.
From: Hydroclimatic extremes contribute to asymmetric trends in ecosystem productivity loss
a Fraction (%) of global GPP losses associated with drought-heat extremes (DH), drought (D), drought-cold extremes (DC), heat extremes (H), cold extremes (C), wet-heat extremes (WH), wet-cold extremes (WC), and wet extremes (W). The spatial pattern of GPP losses associated with drought-heat extremes (b), drought (c), drought-cold extremes (d), heat extremes (e), cold extremes (f), wet-heat extremes (g), wet-cold extremes (h), and wet extremes (i). In (a), the bar show values averaged over all GPP datasets, and the error bars indicate one standard deviation between GPP products; blue lines within the bar indicate the 0.05 significant level. In (b–i), values for which less than half of the products are significant at the 0.1 level are masked in white. The results are based on GPP products and extreme indices with the removed linear trends as well as GLEAM soil moisture.
