1985年至2020年间全球不透气表面扩张造成的碳排放
Zhehua Li1, Wendi Liu1, Xiao Zhang2
1State Key Laboratory of Remote Sensing Science, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100094, China; International Research Center of Big Data for Sustainable Development Goals, Beijing 100094, China; University of Chinese Academy of Sciences, Beijing 100049, China.
The Science of the total environment
|August 31, 2024
概括
不透的表面膨胀 (ISE) 造成了显著的碳损失. 35年来,全球ISE释放了1.14 PgC,主要来自地表有机碳和生物质,影响了陆地生态系统.
科学领域:
- 环境科学 环境科学
- 生态生态学 生态生态学
- 气候变化研究 气候变化研究
背景情况:
- 不透的表面扩张 (ISE) 是由于城市化而覆盖自然土地的人工材料.
- 广泛的IEE导致陆地生态系统碳池的重大损失.
- 对ISE碳影响的全球评估受到数据可用性和不确定性的限制.
研究的目的:
- 量化1985年至2020年间全球ISE产生的碳排放量.
- 为了解决数据缺口和不确定性,以评估ISE对碳池的影响.
- 根据IPCC的指导方针提供全面的全球评估.
主要方法:
- 将全球土地划分为87个精细的地理区域.
- 综合多种数据产品:无透的地表数据,土地覆盖动态,生物质和地表有机碳 (TSOC).
- 利用生物质和TSOC密度的查找表 (LUT),并应用IPCC的碳排放估计方法.
主要成果:
- 全球IEE覆盖了5812万公,其中67.30%来自耕地侵占.
- 在过去的35年中,累计的碳排放量达到1.14±0.38千克碳 (PgC).
- 上层土壤有机碳占排放量的54.55%,生物质碳占排放量的45.45%.
结论:
- 全球ISE是承诺碳排放的重要来源.
- 了解ISE的碳足迹对于减缓气候变化和土地管理至关重要.
- 未来的研究应该专注于改进数据和改进准确碳核算模型.
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