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Plant uptake of CO <sub>2</sub> outpaces losses from permafrost and plant respiration on the Tibetan Plateau

Da Wei, Yahui Qi, Yaoming Ma, Xufeng Wang, Weiqiang Ma, Tanguang Gao, Lin Huang, Hui Zhao, Jianxin Zhang, Da Wei

2021Proceedings of the National Academy of Sciences164 citationsDOIOpen Access PDF

Abstract

Significance Cold regions contain vast stores of permafrost carbon. Rapid warming will cause permafrost to thaw and plant respiration to accelerate, with a resultant loss of CO 2 , but could also increase the fixation of CO 2 by plants. A network of 32 eddy covariance sites on the Tibetan Plateau, which has the largest store of alpine permafrost carbon on Earth, shows that this region functions as a net CO 2 sink. Our sensitivity analyses, experiments, and model simulations consistently showed that the fixation of CO 2 by plants outpaces the loss of CO 2 from permafrost and accelerates plant respiration. This indicates a plant-dominated CO 2 balance on the Tibetan Plateau, which could provide a negative feedback to climate warming.

Topics & Concepts

PermafrostEnvironmental sciencePlateau (mathematics)Eddy covarianceAtmospheric sciencesSink (geography)Carbon sinkClimate changeCarbon cycleCarbon fibersRespirationPhysical geographyEcologyGeologyEcosystemBiologyGeographyBotanyMaterials scienceComposite materialComposite numberCartographyMathematicsMathematical analysisClimate change and permafrostCryospheric studies and observationsClimate variability and models