Abstract

Gross primary production (GPP) determines the amounts of carbon and energy that enter terrestrial ecosystems. However, the tremendous uncertainty of the GPP still hinders the reliability of GPP estimates and therefore understanding of the global carbon cycle. In this study, using observations from global eddy covariance (EC) flux towers, we appraised the performance of 24 widely used GPP models and the quality of major spatial data layers that drive the models. Results show that global GPP products generated by the 24 models varied greatly in means (from 92.7 to 178.9 Pg C yr−1) and trends (from −0.25 to 0.84 Pg C yr−1). Model structure differences (i.e., light use efficiency models, machine learning models, and process-based biophysical models) are an important aspect contributing to the large uncertainty. In addition, various biases in currently available spatial datasets have found (e.g., only 57% of the observed variation in photosynthetically active radiation at the flux tower locations was explained by the spatial dataset), which not only affect GPP simulation but more importantly hinder the simulation and understanding of the earth system. Moving forward, research into the efficacy of model structures and precision of input data may be more important for global GPP estimation.

Highlights

  • Terrestrial gross primary production (GPP) or the total photosynthetic uptake of carbon by plants plays a critical role in maintaining the global carbon balance between the biosphere and atmosphere

  • Model was not evaluated at a global scale because of the difficulty in estimating the water stress in the light use efficiency (LUE)-evaporative fraction (EF) model, which cannot be readily derived from satellite observations

  • Model LUE-EF simulated the amplitude of the variations close to the data amplitude of eddy covariance (EC)-towers (SD ratio = 0.93)

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Summary

Introduction

Terrestrial gross primary production (GPP) or the total photosynthetic uptake of carbon by plants plays a critical role in maintaining the global carbon balance between the biosphere and atmosphere. The estimation of terrestrial GPP by existing models remains highly uncertain, with global estimates ranging widely between 92.7 to 168.7 Pg C yr−1 [1,2,3]. This large uncertainty poses a serious obstacle to quantifying and understanding the global carbon cycle [4]. It is broadly agreed that, to reduce the Remote Sens. 2021, 13, 168 uncertainty of GPP estimation and advance carbon cycle science, it is crucial to consider:. Large structural differences can be observed among GPP models

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