Global ecosystems currently provide a sink for roughly one quarter of anthropogenic carbon emissions (Friedlingstein et al., 2022), and the climate-driven variations in this carbon sink therefore have significant implications for long-term changes in climate. Direct quantification of net and gross ecosystem productivity at regional to global scales is elusive, however, given the spatial heterogeneity of the global land surface and the sparse nature of direct observations of land-atmosphere carbon exchange, and contributes significant uncertainty to the global carbon budget (Friedlingstein et al., 2022;Le Quéré et al., 2018).