Extended Data Figure 6: Spatial pattern of the contribution of precipitation to NEE exchange in 2011.
From: Contribution of semi-arid ecosystems to interannual variability of the global carbon cycle
This is calculated as the difference between NPP (a) and Rh (b) with the all-climate forcing varied and NEE simulated with the precipitation climatology. This is the same as in Fig. 2c but for component fluxes of NEE.
