Emergent constraints on historical and future global gross primary productivity

Author:

Chen Xin1,Chen Tiexi123ORCID,Liu Yi Y.4,He Bin5,Liu Shuci6,Guo Renjie7,Dolman Han8

Affiliation:

1. School of Geographical Sciences Nanjing University of Information Science and Technology Nanjing China

2. Qinghai Provincial Key Laboratory of Plateau Climate Change and Corresponding Ecological and Environmental Effects Qinghai University of Science and Technology Xining China

3. School of Geographical Sciences Qinghai Normal University Xining China

4. School of Civil and Environmental Engineering University of New South Wales Sydney New South Wales Australia

5. College of Global Change and Earth System Science Beijing Normal University Beijing China

6. Department of Environment and Science Queensland Government Brisbane Australia

7. Faculty of Geographical Science Beijing Normal University Beijing China

8. NIOZ Royal Netherlands Institute for Sea Research Texel The Netherlands

Abstract

AbstractTerrestrial gross primary productivity (GPP) is the largest carbon flux in the global carbon cycle and plays a crucial role in terrestrial carbon sequestration. However, historical and future global GPP estimates still vary markedly. In this study, we reduced uncertainties in global GPP estimates by employing an innovative emergent constraint method on remote sensing‐based GPP datasets (RS‐GPP), using ground‐based estimates of GPP from flux towers as the observational constraint. Using this approach, the global GPP in 2001–2014 was estimated to be 126.8 ± 6.4 PgC year−1, compared to the original RS‐GPP ensemble mean of 120.9 ± 10.6 PgC year−1, which reduced the uncertainty range by 39.6%. Independent space‐ and time‐based (different latitudinal zones, different vegetation types, and individual year) constraints further confirmed the robustness of the global GPP estimate. Building on these insights, we extended our constraints to project global GPP estimates in 2081–2100 under various Shared Socioeconomic Pathway (SSP) scenarios: SSP126 (140.6 ± 9.3 PgC year−1), SSP245 (153.5 ± 13.4 PgC year−1), SSP370 (170.7 ± 16.9 PgC year−1), and SSP585 (194.1 ± 23.2 PgC year−1). These findings have important implications for understanding and projecting climate change, helping to develop more effective climate policies and carbon reduction strategies.

Funder

National Natural Science Foundation of China

Natural Science Foundation of Qinghai Province

Publisher

Wiley

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