干旱气象 ›› 2025, Vol. 43 ›› Issue (2): 265-276.

• 论文 • 上一篇    

云南省一次罕见飑线过程发生机制分析

杨芳园1,3 ,杨素雨2,3 ,甄廷忠1 ,杨竹云2,3 ,李晓鹏1 ,胡勇华4 ,石宝灵1
  

  1. 1. 云南省昆明市气象局,云南 昆明 650034;2. 云南省气象台,云南 昆明 650034;3. 中国气象局横断山区(低纬高原)灾害性
    天气研究中心,云南 昆明 650034;4. 云南省玉溪市红塔区气象局,云南 玉溪 653100
  • 出版日期:2025-04-30 发布日期:2025-05-13

Mechanism analysis of a rare squall line process in Yunnan Province

YANG Fangyuan1,3 , YANG Suyu2,3 , ZHEN Tingzhong1 , YANG Zhuyun2,3 ,  LI Xiaopeng1 , HU Yonghua4 , SHI Baoling1   

  1. 1. Kunming Meteorological Bureau of Yunnan Province, Kunming 650034, China;
    2. Meteorological Observatory of Yunnan Province, Kunming 650034, China;
    3. Research Center for Disasrous Weather over Hengduan Mountains & Low-Latitude Plateau, CMA, Kunming 650034, China;
    4. Hongta District Meteorological Bureau of Yunnan Province, Yuxi 653100, Yunnan, China
  • Online:2025-04-30 Published:2025-05-13

摘要:

基于地面自动站、多波段天气雷达、实况探空及欧洲中期天气预报中心(European Centre for Medium-Range Weather Forecasting,ECMWF)第 5代再分析资料 ERA5,对 2022年 7月 7日云南省一次罕见飑线天气过程的环境条件、中尺度特征及维持机制进行了分析。结果表明,此次飑线过程发生在大陆高压与副热带高压辐合区内,环境场具有较强对流不稳定能量、中等强度垂直风切变及明显的高层干冷空气入侵特征。C波段雷达反射率和径向速度的变化与地面大风、冰雹的发生有很好的对应关系,飑线特征明显,近地层入流急流明显,伴随速度模糊和阵风锋特征;降雹单体具有三体散射、中层辐合和风暴顶辐散特征;X波段双偏振相控阵雷达的高时空分辨率观测显示,成熟冰雹云的强反射率因子超过 55 dBZ,强上升气流附近存在明显的差分反射率(ZDR)柱,垂直伸展至高于湿球温度 0 ℃层的高度;双偏振参数还表明,冰雹降落过程中伴有降水。分析认为,地面辐合线的持续维持、风暴内
部上升气流与倾斜下沉气流共存,以及低层辐合与高层辐散配合,是此次飑线得以维持的主要机制。

关键词: 飑线, 中尺度特征, 双偏振量, 地面辐合线

Abstract:

Based on ground automatic station, multi-band weather radar and sounding data, and the fifth generation atmospheric re⁃
analysis ERA5 from the European Centre for Medium-Range Weather Forecasts (ECMWF), the environmental conditions, mesoscale
characteristics and maintenance mechanisms of a rare squall line weather process in Yunnan Province on 7 July 2022 were analyzed. The results show that this squall line occurred within the convergence zone of the continental high and subtropical high, with environmental conditions characterized by strong convective available potential energy, moderate vertical wind shear, and significant intrusion of high-level dry and cold air. Changes in C-band radar reflectivity and radial velocity were closely associated with the occurrence of strong surface winds and hail. The squall line exhibited distinct features, with a pronounced inflow jet near the surface layer, accompanied by velocity ambiguity and gust front characteristics. The hail cells exhibited characteristics such as three-body scattering, midlevel convergence, and storm-top divergence. High spatial and temporal resolution observations from the X-band dual-polarization phased array radar showed that mature hail clouds had a strong reflectivity factor exceeding 55 dBZ. At the same time, a prominent differential reflectivity (ZDR) column was observed near the strong updraft, with vertical extension exceeding the height of the wet-bulb temperature 0 ℃ layer. Dual-polarization parameters further indicated that precipitation occurred during the hailfall process. The analysis found that the long-term maintenance of ground convergence lines, the coexistence of strong updrafts and tilted downdrafts within the storm, and the coupling of low-level convergence with high-level divergence was the main mechanisms sustaining this squall line.

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