环境科学
蒸散量
水循环
碳循环
陆地生态系统
碳纤维
气候变化
用水效率
用水
大气科学
初级生产
陆生植物
地球大气中的二氧化碳
全球变暖
大气碳循环
二氧化碳
生态学
生态系统
灌溉
生物
材料科学
地质学
复合材料
复合数
作者
Lei Cheng,Lu Zhang,Ying‐Ping Wang,Josep G. Canadell,Francis H. S. Chiew,Jason Beringer,Longhui Li,Diego G. Miralles,Shilong Piao,Yongqiang Zhang
标识
DOI:10.1038/s41467-017-00114-5
摘要
Abstract Quantifying the responses of the coupled carbon and water cycles to current global warming and rising atmospheric CO 2 concentration is crucial for predicting and adapting to climate changes. Here we show that terrestrial carbon uptake (i.e. gross primary production) increased significantly from 1982 to 2011 using a combination of ground-based and remotely sensed land and atmospheric observations. Importantly, we find that the terrestrial carbon uptake increase is not accompanied by a proportional increase in water use (i.e. evapotranspiration) but is largely (about 90%) driven by increased carbon uptake per unit of water use, i.e. water use efficiency. The increased water use efficiency is positively related to rising CO 2 concentration and increased canopy leaf area index, and negatively influenced by increased vapour pressure deficits. Our findings suggest that rising atmospheric CO 2 concentration has caused a shift in terrestrial water economics of carbon uptake.
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