Heat and Drought Events Alter Biogenic Capacity to Balance CO₂ Budget in South-Western Europe.

For instance, we have identified with VPRM a positive trend in NEE (i.e., a decreasing trend in net carbon uptake) of croplands in the Central Massif of France (Figure 3e ) coinciding spatially with a drying trend in the region (Figure S12 in Supporting Information S1 ) (X.

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GOSIF presents a positive trend in GEE (spatial median of 5.50 g C m −2 year −2 and 52.5% of the vegetated areas showing significant increases), while positive VPRM GEE trends are more localized to the mountainous regions (3.58 g C m −2 year −2 and 25.3%).

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