Abstract

Variability in climate exerts a strong influence on vegetation productivity (gross primary productivity; GPP), and therefore has a large impact on the land carbon sink. However, no direct observations of global GPP exist, and estimates rely on models that are constrained by observations at various spatial and temporal scales. Here, we assess the consistency in GPP from global products which extend for more than three decades; two observation‐based approaches, the upscaling of FLUXNET site observations (FLUXCOM) and a remote sensing derived light use efficiency model (RS‐LUE), and from a suite of terrestrial biosphere models (TRENDYv6). At local scales, we find high correlations in annual GPP among the products, with exceptions in tropical and high northern latitudes. On longer time scales, the products agree on the direction of trends over 58% of the land, with large increases across northern latitudes driven by warming trends. Further, tropical regions exhibit the largest interannual variability in GPP, with both rainforests and savannas contributing substantially. Variability in savanna GPP is likely predominantly driven by water availability, although temperature could play a role via soil moisture‐atmosphere feedbacks. There is, however, no consensus on the magnitude and driver of variability of tropical forests, which suggest uncertainties in process representations and underlying observations remain. These results emphasize the need for more direct long‐term observations of GPP along with an extension of in situ networks in underrepresented regions (e.g., tropical forests). Such capabilities would support efforts to better validate relevant processes in models, to more accurately estimate GPP.

Highlights

  • Gross primary production (GPP), the amount of carbon fixed by photosynthesis per unit area in time, is the pathway for transferring atmospheric CO2 to the terrestrial biosphere

  • We compared trends and interannual variability (IAV) in climate‐driven GPP based on the three global products, FLUXCOM, TRENDYv6, and remote sensing derived light use efficiency model (RS‐light‐use efficiency (LUE)) at large spatial scales

  • We found that individual FLUXCOM ensemble members do not agree on the direction of the GPP trend (Figure S5), the large uncertainty in estimates based on the ensemble mean

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Summary

Introduction

Gross primary production (GPP), the amount of carbon fixed by photosynthesis per unit area in time, is the pathway for transferring atmospheric CO2 to the terrestrial biosphere. It is the largest carbon flux in the Earth system, and as such any small change can significantly alter the net carbon balance at the surface, atmospheric CO2 concentrations, and subsequently feedbacks to climate (Friedlingstein et al, 2014). GPP responds to changes in atmospheric CO2 concentrations, nutrient availability, and climate Land use and land cover change (e.g., deforestation) alter the spatial distribution of vegetation and impact GPP and carbon uptake

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