2001-2019年全球表面氨度的演变:大小,模式和驱动因素
Jiageng Ma1,2, Hao Shi1, Yingjie Zhu2
1State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences (CAS), Beijing 100085, PR China.
Environmental science & technology
|March 10, 2025
概括
全球氨 (NH3) 度因人类活动和气候变化而增加. 这项研究绘制了2001-2019年的这些变化,确定了热点和主要驱动因素,如肥料使用和温度.
科学领域:
- 大气化学和环境科学
- 全球变化和空气质量研究
- 循环和环境影响研究.
背景情况:
- 氨 (NH3) 是大气中主要的性气体,对空气质量,生态系统和人类健康产生重大影响.
- 预计NH3度的升高将在全球范围内增加,这是由于正在进行的全球变化和强化的人为排放.
- 了解NH3的空间和时间动态对于环境管理和政策制定至关重要.
研究的目的:
- 以高分辨率 (0.1°×0.1°) 从2001年到2019年估计表面氨 (NH3) 度的全球变化.
- 确定NH3度升高的热点,并分析这些变化背后的驱动因素.
- 开发和验证一种用于估计大气NH3度的新型规模适应型建模方法.
主要方法:
- 利用地面观测,对 (有机和无机) 肥料应用的网格数据,气象数据和辅助信息.
- 开发了一种新的规模适应方法:一个集成随机森林模型,包含旋转四树分区和盒子-Cox转换.
- 根据观察到的NH3模式验证了模型,实现了高精度 (R2 = 0.91,斜率 = 0.82整体;R2 = 0.79,斜率 = 0.70用于测试).
主要成果:
- 全球表面NH3度从2001年的1.44μg m−3 yr−1增加到2019年的1.51μg m−3 yr−1.
- 在南亚北部,中国北部,萨赫勒地区,南美东南部和美国中部发现了NH3升高的热点.
- 将NH3的增加归因于中国的SO2排放减少和肥料使用增加,以及南亚的投入. 温度影响了非洲,南美洲和大洋洲的NH3.
结论:
- 该研究提供了全球NH3度变化的高分辨率估计,并确定了关键的贡献因素.
- 这些发现支持对全球循环及其环境影响的研究,为有针对性的管理策略提供信息.
- 开发的建模算法有效地捕获异质数据中的复杂模式,解决大气研究中的升级挑战.
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