Preprints
https://doi.org/10.5194/egusphere-2026-6317
https://doi.org/10.5194/egusphere-2026-6317
11 Nov 2026
 | 11 Nov 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Climate-Driven Temperature Changes in the Future Impair China's Terrestrial Carbon Sink Capacity

Bowen Xu, Jiani Tan, Yujian Wang, Jinglei Wu, Haixia Dai, Ling Huang, and Li Li

Abstract. The terrestrial carbon sink modulates the rise of atmospheric CO2, yet its long-term persistence under climate warming remains poorly constrained, largely due to nonlinear temperature responses of ecosystem carbon fluxes. Here we integrate eddy-covariance observations, process-based simulations, and interpretable machine learning to quantify the nonlinear temperature dependence of China's net ecosystem productivity (NEP) and project changes in terrestrial carbon sinks to 2060 across shared socioeconomic pathways. Site-scale observations reveal vegetation-specific turning points in NEP–temperature relationships, yielding a broad range of NEP temperature thresholds spanning 15–25 °C. Aggregated to the national scale, NEP remains stable between 0 and 18 °C, peaks near 20 °C (18–22 °C), and declines beyond this optimum threshold, implying that sustained warming could weaken terrestrial carbon sequestration. A controlled sensitivity experiment with uniform 0.5 °C warming reduces national NEP by 0.17 PgC yr–1, corresponding to a 31 % loss of the terrestrial carbon sink. Extending this framework to 2060, our projections show national NEP reductions of 24 %, 27 %, and 56 % under SSP1-2.6, SSP2-4.5, and SSP5-8.5, respectively. Across all three scenarios, grasslands exhibit the highest proportional vulnerability to warming, with NEP losses ranging from 44 % to 171 %, whereas forests show comparatively modest relative NEP declines (7–23%). While land-use and vegetation dynamics can partially offset these sink losses, such buffering effects remain localized and are overwhelmed by nationwide warming-driven carbon sink reduction. Our findings demonstrate that this warming-triggered NEP decline diminishes the capacity of terrestrial ecosystems to buffer atmospheric CO2 accumulation and mitigate climate change. This study illustrates how threshold-line nonlinear NEP-temperature responses weaken terrestrial carbon sink contributions toward China’s carbon peaking and carbon neutrality goals.

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Bowen Xu, Jiani Tan, Yujian Wang, Jinglei Wu, Haixia Dai, Ling Huang, and Li Li

Status: open (until 23 Dec 2026)

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Bowen Xu, Jiani Tan, Yujian Wang, Jinglei Wu, Haixia Dai, Ling Huang, and Li Li

Data sets

Calibrated WRF-VPRM Model Projections of Monthly Terrestrial Carbon Fluxes (GEE, RES, NEP) for China (2020–2060) under SSP126, SSP245, and SSP585 Scenarios J. Tan et al. https://zenodo.org/records/20424094

Bowen Xu, Jiani Tan, Yujian Wang, Jinglei Wu, Haixia Dai, Ling Huang, and Li Li
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Latest update: 12 Nov 2026
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Short summary
We quantified how rising temperatures alter China's terrestrial carbon sink, using in-situ carbon flux measurements, process-based ecosystem simulations, and interpretable machine learning. We found that national terrestrial carbon sink peaks at surface temperature of 18–22 ºC, and warming beyond this threshold weakens carbon storage. We found widespread carbon sink loss by 2060 under warming, although shifts in land use and improved plant greenness can locally buffer this decline.
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