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Updated: Nov 26, 2025

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Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
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印度季风被北大西洋波浪拖出轨
P J Borah1,2, V Venugopal3,2,4, J Sukhatme1,2
1Centre for Atmospheric and Oceanic Sciences, Indian Institute of Science, Bangalore 560012, India.
概括
印度季风干旱通常由温暖的太平洋条件预测. 然而,近一半的过去干旱都显示出接近中性的太平洋气温,以及与中度罗斯比波相关的季末降雨突然减少.
科学领域:
- 气候学
- 大气科学
- 天气学
背景情况:
- 印度季风干旱预测传统上依赖于与热带赤道太平洋相关的季节性降雨缺口.
- 然而,这种模式并不能解释历史干旱事件的重要部分.
研究的目的:
- 调查印度季风干旱的特征和潜在机制,
- 确定改善干旱预测的替代预测因素.
主要方法:
- 分析过去一个世纪的历史干旱数据.
- 确定季后降雨模式及其与太平洋和大西洋气候变化的相关性.
- 对大气远程连接的研究,特别是罗斯比波动力学和形异常.
主要成果:
- 过去一个世纪的印度季风干旱几乎有一半发生在接近中性的太平洋温度下.
- 这些干旱的特点是季后性,突然的季后降雨不足.
- 一个重要的大气远程连接被确定,涉及来自中度的罗斯比波,特别是与北大西洋状异常相关.
结论:
- 印度季风干旱可以由独立于赤道太平洋条件的机制驱动.
- 与中度大气远程连接相关的季节性降雨缺口是一个关键的,但被低估的干旱驱动因素.
- 这种已识别的大气远程连接为提高印度季风干旱的预测性提供了新的途径,
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