从1973年到2007年,在全球范围内,清的天空可见度在陆地上下降了
Kaicun Wang1, Robert E Dickinson, Shunlin Liang
1Department of Geography, University of Maryland, College Park, MD 20742, USA. kcwang@umd.edu
概括
自20世纪80年代中期以来,由气溶引起的全球变暗已经增加,减少了太阳辐射. 虽然欧洲正在变得更加明亮,但其他大陆的可见度正在恶化和变暗.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 环境科学 环境科学
背景情况:
- 气溶通过降低可见度显著影响地球表面的太阳辐射.
- 全球变暗,以减少太阳辐射为特征,一直观察到20世纪80年代中期.
研究的目的:
- 从1973年到2007年,在陆地上创造一个全球气候学反向可见度的气候学.
- 在气溶光学深度和太阳辐射影响方面解释可见性变化.
主要方法:
- 对35年 (1973-2007) 的陆地反向可见度的分析.
- 解释有关气溶光学深度和落入太阳辐射的可见性趋势.
主要成果:
- 气溶对全球变暗的贡献在整个分析期间均增加.
- 自20世纪80年代中期以来,欧洲的知名度有所提高 (欧洲亮化).
- 在南亚和东亚,南美洲,澳大利亚和非洲的可见度有所下降,导致陆地上的全球净变暗.
结论:
- 这项研究确立了一种长期趋势,即由于气溶导致陆地上的全球变暗增加.
- 可见性趋势的区域差异很明显,欧洲变得更亮,而其他大陆则变暗.
- 气溶驱动的可见性变化对全球发生的太阳辐射有重大影响.
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