在20世纪30年代尘埃碗的原因上
Siegfried D Schubert1, Max J Suarez, Philip J Pegion
1Earth Sciences Directorate, National Aeronautics and Space Administration/Goddard Space Flight Center, Greenbelt, Maryland 20771, USA. schubert@gmao.gsfc.nasa.gov
概括
20世纪30年代美国的尘埃盆干旱主要是由不寻常的热带海面温度引起的. 陆地与大气的相互作用加剧了这种严重,广泛的干旱事件.
科学领域:
- 气候学 气候学 气候学
- 环境科学 环境科学
- 大气科学 大气科学
背景情况:
- 20世纪30年代见证了美国历史上最严重的干旱之一,影响了广大地区,造成了臭名昭着的尘暴.
- 这一时期,通常被称为尘埃碗,显著影响了大平原南部,墨西哥和加拿大.
研究的目的:
- 调查20世纪30年代北美干旱的主要驱动因素.
- 分析热带海洋表面温度和陆地-大气相互作用在干旱严重性的作用.
- 为了将20世纪30年代的干旱与20世纪其他北美干旱进行比较.
主要方法:
- 利用气候模型模拟干旱条件.
- 分析了20世纪30年代的异常热带海洋表面温度数据.
- 在干旱期间检查了大气和陆地表面的相互作用.
主要成果:
- 模型结果表明,异常的热带海面温度是造成20世纪30年代干旱的主要原因.
- 大气和陆地表面的相互作用显著放大了干旱的严重程度.
- 当将20世纪30年代的干旱与20世纪其他北美干旱进行比较时,观察到明显的差异.
结论:
- 热带海面温度是引发20世纪30年代美国干旱的关键因素.
- 陆地大气反加剧了干旱,增加了其破坏性影响.
- 20世纪30年代的干旱是理解严重,长期干旱事件的关键案例研究.
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