环境科学
二氧化碳
泥炭
全球变暖
气候变化
碳纤维
生态系统
温室气体
碳循环
大气科学
地下水位
地球大气中的二氧化碳
生产力
固碳
碳汇
基质(水族馆)
表(数据库)
蒸散量
水文学(农业)
生态系统呼吸
降水
环境化学
温室效应
作者
Quan Quan,Jian Zhou,Paul J. Hanson,Daniel Ricciuto,Stephen D. Sebestyen,David J. Weston,Jeffrey P. Chanton,Rachel Wilson,Joel E. Kostka,Yu Zhou,Ning Wei,Lifen Jiang,Melanie A. Mayes,Jonathan M. Stelling,Andrew D. Richardson,Mirindi Eric Dusenge,Danielle A. Way,J. M. Warren,Yiqi Luo
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2025-10-23
卷期号:390 (6771): 367-370
被引量:6
标识
DOI:10.1126/science.adv7104
摘要
Extreme drought events are predicted to increase with climate change, yet their impacts on ecosystem carbon dynamics under warming and elevated carbon dioxide (eCO2) remain unclear. In a peatland experiment with five warming treatments each under ambient carbon dioxide (aCO2) and eCO2 (+500 parts per million), a 2-month extreme drought in 2021 reduced net ecosystem productivity by 444.0 ± 65.8 and 736.6 ± 57.8 grams of carbon per square meter at +9°C under aCO2 and eCO2, respectively-228.6 ± 56.8% and 381.9 ± 83.4% of the reduction at +0°C under aCO2. This exacerbation was driven by warming-induced water table decline, prolonged low water tables, and CO2-enhanced substrate availability through increased plant carbon inputs. Findings indicate that future climate will greatly amplify carbon loss during extreme drought, reinforcing positive carbon-climate feedbacks.
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