陆地与大气的过程加剧了近期非洲地区的复合干旱和热浪
Ibraheem A Raji1, Akintomide A Akinsanola1, Thierry N Taguela1
1Department of Earth and Environmental Sciences, University of Illinois Chicago, Chicago, IL, USA.
The Science of the total environment
|January 30, 2026
概括
非洲的复合干旱和热浪事件正在增加,特别是在赤道地区. 这种加剧是由更强的陆地-大气合驱动的,导致更大的社会经济风险.
科学领域:
- 气候科学 气候科学
- 大气科学 大气科学
- 环境科学 环境科学
背景情况:
- 全球变暖加剧了复合干旱和热浪 (CDHW) 事件.
- 由于适应能力有限和气候极端的暴露,非洲面临着更大的脆弱性.
研究的目的:
- 分析非洲各地CDHW事件的最新趋势.
- 诊断CDHW事件的基础陆地大气驱动因素.
主要方法:
- 使用了ERA5和NCEP-2再分析数据集 (1980-2024年).
- 对CDHW事件进行了趋势分析和变化点分析.
- 研究了陆地与大气的相互作用和大规模的气候模式.
主要成果:
- 在赤道非洲确定了一个CDHW热点,频率,持续时间和规模显著增加.
- 检测到2005年后CDHW加剧的转变,这是由加强陆地与大气的合驱动的.
- 由于净向下辐射增加和降水减少导致垂直动力学减弱而导致的变暖.
- 将CDHW强化与大西洋南部振荡,印度洋双极和太平洋十年振荡的增加影响联系在一起.
结论:
- 结合的陆地和大气的过程对非洲的复合极端事件进行了关键调节.
- 由于温度升高和土壤湿度降低,加强了陆地与大气的合,从而放大了CDHW频率.
- 大规模的气候模式在非洲近期CDHW加剧中发挥着越来越重要的作用.
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