由于CO2的增加,全球光合作用的历史增长受到限制
T F Keenan1,2, X Luo3,4,5, M G De Kauwe6,7,8
1Department of Environmental Science, Policy and Management, UC Berkeley, Berkeley, CA, USA. trevorkeenan@berkeley.edu.
Nature
|December 9, 2021
概括
全球陆地碳排放量正在增加, 这一过程极大地促进了全球光合作用,有助于减缓人类排放造成的大气二氧化碳的增加.
科学领域:
- 地球系统科学
- 生态学
- 气候科学
背景情况:
- 全球陆地碳汇正在扩大,吸收大量人为二氧化碳 (CO2).
- 由于大气中二氧化碳的增加,二氧化碳受精,被认为是这种碳汇的主要驱动因素.
- 目前对二氧化碳受精的影响的估计在不同的科学模型和观测数据之间存在很大差异.
研究的目的:
- 解决 CO2 的历史估计差异.
- 量化大气二氧化碳对全球光合作用的影响.
- 将陆地生物圈模型与全球碳预算数据联系起来.
主要方法:
- 利用新兴约束方法整合陆地生物圈模型.
- 结合1981年至2020年期间的全球碳预算估计.
- 量化了二氧化碳对全球光合作用的历史影响.
主要成果:
- 在1981年至2020年期间,二氧化碳施肥使全球年光合作用增加了11.85%±1.4%.
- 这相当于在研究期间碳增加了13.98±1.63倍.
- 这些发现有助于协调对二氧化碳对光合作用的影响的相互矛盾估计.
结论:
- 二氧化碳受精对全球光合作用产生了重大影响.
- 人为二氧化碳排放对全球生态系统产生了重大影响.
- 这项研究更准确地量化了陆地碳汇对二氧化碳的反应.
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