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March 21, 2026Atmosphere2 citationsOpen Access

Terrestrial Net Ecosystem Productivity on the Tibetan Plateau: Characteristics, Climate Drivers and Future Changes

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YLYiming LiMLMingwang LiYSYiming Su

Key Points

  • To assess the spatiotemporal variability of net ecosystem productivity (NEP) across the Tibetan Plateau and understand its climatic drivers.
  • Utilized the Community Land Model version 5.0 to investigate NEP from 1979 to 2018.
  • Conducted climate sensitivity experiments to evaluate different climate factors impacting NEP.
  • Projected future NEP changes from 2025 to 2100 under multiple Shared Socioeconomic Pathways.
  • The Tibetan Plateau primarily acted as a net carbon sink with a mean NEP of 23.96 g C m2 yr−1.
  • NEP exhibited a decreasing trend across most regions during 1979-2018.
  • Air temperature was found to be the major driver of NEP variability, influencing about 68% of changes.

Abstract

Variations in terrestrial carbon flux influence atmospheric CO2 exchange and related climate feedback, with Net ecosystem productivity (NEP) serving as a key metric for assessing ecosystem carbon source–sink dynamics. Given the vital ecological barrier function of the Tibetan Plateau (TP), understanding the spatiotemporal variability of NEP and its climatic controls is essential for elucidating carbon sink and climate interactions under ongoing climate change. The spatiotemporal dynamics of NEP across the TP from 1979 to 2018 are investigated using the process-based Community Land Model version 5.0 (CLM5.0). And climate sensitivity experiments are conducted to quantify the relative contributions of different climate factors to NEP variability. Furthermore, future changes in NEP for the period 2025–2100 under multiple Shared Socioeconomic Pathway (SSP) scenarios are projected. The results indicate that the TP functioned predominantly as a net carbon sink during the historical period, with a multi-year mean NEP of 23.96 g C m2 yr−1. Spatially, NEP showed a significantly increasing gradient from the northwest to the southeast. During 1979–2018, NEP exhibited an overall decreasing trend across most regions of the TP. Air temperature was identified as the dominant controlling factor, accounting for approximately 68% of the interannual NEP variability, followed by solar radiation (21%) and precipitation (11%). The dominant climatic drivers of NEP variation differ among regions: air temperature predominates in the southwestern and southeastern regions, radiation dominates in the northwestern and central areas, and precipitation exerts a controlling effect in the northern and western regions. Future projections suggest that NEP remains positive under all SSP scenarios, indicating that the TP is likely to persist as a carbon sink throughout the 21st century. This study provides important reference for the development of ecological protection, restoration planning, and regional carbon neutrality strategies.

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Cite This Study

Li et al. (2026) studied this question.

synapsesocial.com/papers/69be387d6e48c4981c678e3ahttps://doi.org/10.3390/atmos17030317
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