中国的千年陆地碳排放被过去四十年的碳汇所抵消
Weizhe Chen1, Philippe Ciais2, Kailiang Yu3
1State Key Laboratory of Geomicrobiology and Environmental Changes, Hubei Key Laboratory of Critical Zone Evolution, School of Earth and Planetary Sciences, China University of Geosciences, Wuhan, China. wzchen@cug.edu.cn.
Nature communications
|February 26, 2026
概括
中国中国中国中国.
科学领域:
- 地球和环境科学 地球和环境科学
- 气候科学 气候科学
- 生态生态学 生态生态学
背景情况:
- 中国的千年级气候和土地利用变化是显著的.
- 对土地碳动态的综合影响还没有得到充分的研究.
研究的目的:
- 从851年到2022年,量化中国陆地有机碳的时空变化.
- 调查这些碳动态的驱动因素.
主要方法:
- 使用了陆地表面模型.
- 用重建的气候和土地覆盖数据强制模型.
- 分析了千年时间尺度上的陆地有机碳变化.
主要成果:
- 中国工业化前的土地碳动态反映了全球趋势.
- 从1700年到1900年,土地碳排放量显著,主要是由于森林砍伐.
- 851-1980年的排放量被1980年后的碳汇所抵消.
结论:
- 森林植被和二氧化碳施肥导致了快速的碳捕获.
- 中国的陆地碳动态对全球有重大影响.
- 了解历史驱动因素对于未来的气候减缓至关重要.
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