在西藏高原东南部有两种类型的暴雨
Dianbin Cao1, Xuelong Chen2, Deliang Chen3
1Alpine Paleoecology and Human Adaptation Group (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Motuo Observation and Research Center for Earth Landscape and Earth System, Chinese Academy of Sciences, Linzhi 860712, China.
Science bulletin
|January 4, 2025
概括
西藏高原东南部的夏季大雨是由两个主要的循环类型驱动的:西藏高原型 (TPVT) 和中度低谷型 (MLTT). 了解这些模式是预测区域降雨量的关键.
科学领域:
- 气象学 天气学
- 气候学 气候学 气候学
- 大气科学 大气科学
背景情况:
- 西藏高原东南部 (SETP) 经历了夏天的大量降水.
- 导致SETP降水的大规模大气循环模式尚未完全理解.
研究的目的:
- 识别和描述与SETP中夏季大雨相关的主要大气循环类型.
- 阐明导致这些降水事件的动态机制.
主要方法:
- 使用等级聚类来对大气循环模式进行分类.
- 分析的重点是旋流异常,湿度趋同和喷流流位移.
主要成果:
- 确定了两种主要循环类型:西藏高原旋风类型 (TPVT,56.6%) 和中度低谷类型 (MLTT,43.4%).
- 这两种类型都与正旋转异常,湿度趋同和西向喷流转移相关.
- TPVT事件涉及向东的潜在旋进展,而MLTT事件与外热带低谷入侵有关.
结论:
- 这项研究阐明了SETP夏季大降雨的复杂动态.
- 识别的循环模式为区域气象事件预测提供了洞察力.
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