人为反应性的全球净气候影响
Cheng Gong1, Hanqin Tian2,3, Hong Liao4
1Max Planck Institute for Biogeochemistry, Jena, Germany. cgong@bgc-jena.mpg.de.
Nature
|July 24, 2024
概括
人为反应性 (Nr) 通过影响气溶,甲和碳封存,对全球气候产生净冷却效应. 未来的减排需要减少温室气体排放以缓解气候变化.
科学领域:
- 环境科学
- 气候科学
- 大气化学
背景情况:
- 自工业化前以来,人类活动在地球系统中显著增加了活性 (Nr).
- 增加的Nr有助于增肥和空气污染,对全球气候的复杂影响仍然不完全理解.
研究的目的:
- 量化人为反应性 (Nr) 的净气候影响.
- 在不同的排放场景下预测Nr的未来气候影响.
主要方法:
- 使用气候建模来评估由人类造成的辐射强迫.
- 分析了气溶载荷,甲寿命,陆地碳封存,氧化和臭氧的影响.
- 用了三个代表性的未来预测场景.
主要成果:
- 在2019年 (相对于1850年) 中,人为Nr导致了0.34 W m-2的净负辐射强迫.
- 这种冷却是由于气溶的增加,甲寿命的缩短以及碳封存的增强,超过了N2O和臭氧的变暖.
- 未来的Nr减少预计会减弱这种冷却效应,而N2O引起的变暖可能会增加.
结论:
- 反应性对气候系统具有显著的冷却作用.
- 缓解气候变化需要同时解决气体污染和温室气体排放问题.
- 与Nr相关的环境保护目标必须与气候缓解战略相结合,符合"巴黎协定".
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