永久冻土
环境科学
涡度相关法
大气科学
水槽(地理)
呼吸
碳汇
气候变化
碳纤维
高原(数学)
自然地理学
生态系统
碳循环
生态学
地质学
生物
植物
材料科学
地理
复合数
数学分析
地图学
数学
复合材料
作者
Da Wei,Yahui Qi,Yaoming Ma,Xufeng Wang,Weiqiang Ma,Tanguang Gao,Lin Huang,Hui Zhao,Jianxin Zhang,Xiaodan Wang
标识
DOI:10.1073/pnas.2015283118
摘要
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.
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