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在过去的70年里,在新疆北部地区地区性暴风雪的占主导地位的综合图案和基本特征
Chunyang Li1, Abuduwaili Abulikemu2, Xin Xu3
1Xinjiang Key Laboratory of Oasis Ecology, College of Geography and Remote Sensing Sciences, Xinjiang University, Urumqi, China.
Scientific reports
|July 2, 2025
概括
极地活动推动了新疆北部的暴风雪. 不同的形模式和喷流变化影响风暴频率,强度和水分传输,揭示了关键的大气动力学.
科学领域:
- 大气科学 大气科学
- 气象学 天气学
- 气候学 气候学 气候学
背景情况:
- 区域性暴风雪在新疆北部 (NX) 带来了重大挑战.
- 了解这些事件背后的预测模式和大气动态对于预测和缓解至关重要.
研究的目的:
- 在NX中使用客观方法分类暴风雪事件.
- 为了识别与极地活动相关的明显的同视模式.
- 分析喷流和水分传输对暴风雪特征的影响.
主要方法:
- 使用PCT客观分类方法.
- 从1953年到2022年,分析了134个地区的暴风雪事件.
- 采用了观察和重新分析数据.
主要成果:
- 确定了与极地活动相关的四种主要的综合类型.
- 发现66.4%的事件与异常极旋模式和33.6%与二极旋相关.
- 证明上层和下层喷流变化直接影响暴风雪的频率,分布和水分传输.
结论:
- 极地活动是北极地区暴风雪的关键驱动因素.
- 不同的synoptic类型具有独特的形成机制.
- 大规模的循环系统从根本上决定了进入和离开该地区的水分运输模式.
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