在厄尔尼诺夏季,印度季风降雨量更为极端
Spencer A Hill1, Destiny Zamir Meyers2, Adam H Sobel3,4
1Department of Earth and Atmospheric Sciences, City College of New York, New York, NY, USA.
概括
厄尔尼诺现象加剧了印度的每日极端降雨, 这种反直觉的发现与对流浮力增加有关,
科学领域:
- 气候学
- 大气科学
- 天气学
背景情况:
- 印度夏季季风期间的极端降雨带来重大风险.
- 厄尔尼诺现象通常会抑制印度夏季季风的降雨.
研究的目的:
- 调查印度厄尔尼诺现象期间每天极端降雨的反直觉加剧.
- 确定这种现象背后的大气驱动因素.
主要方法:
- 从1901年到2020年的观测数据分析.
- 检查对流浮性,包括未稀释的不稳定性和混合效应.
主要成果:
- 厄尔尼诺现象加剧了印度每天的极端降雨.
- 考虑到不稳定性和稀释性,增加的对流浮力是关键因素.
- 尽管季风降雨总量普遍减少,但这种效应仍然存在.
结论:
- 厄尔尼诺对印度季风的影响是复杂的,
- 这些发现表明,在其他热带地区也有类似的影响.
- 该框架可用于研究每小时极端和气候变化趋势.
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