Fig. 3: Spatial distribution of the sensitivity of SMJJA to LAIMAM and VPDJJA based on the three assessment methods. | npj Climate and Atmospheric Science

Fig. 3: Spatial distribution of the sensitivity of SMJJA to LAIMAM and VPDJJA based on the three assessment methods.

From: Summer atmospheric drying could contribute more to soil moisture change than spring vegetation greening

Fig. 3: Spatial distribution of the sensitivity of SMJJA to LAIMAM and VPDJJA based on the three assessment methods.

a represents the mean values of the sensitivities obtained by the three methods and the corresponding standard deviations. Different points correspond to the mean values of the results of the different methods, and the line gives the magnitude of the corresponding one standard deviation. (b–g) represent the spatial distribution of the sensitivities, respectively. The insets in the figure show the proportion of area occupied by positive sensitivities (blue) and negative sensitivities (brown).

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