山东科学

• 环境与生态 •    

豫东北三次龙卷环流背景、环境条件和雷达特征分析

马慧妍   

  1. 濮阳市气象局,河南 濮阳 457000
  • 收稿日期:2025-10-29 接受日期:2026-05-13 上线日期:2026-07-06
  • 通信作者: 马慧妍 E-mail:25239692@qq.com
  • 作者简介:马慧妍(1982—),女,本科,工程师,研究方向为短期气象预报预警服务。E-mail:25239692@qq.com
  • 基金资助:
    中国气象局河南省农业气象保障与应用技术重点实验室应用技术研究基金(KF202446)

Analysis of the synoptic background, environmental conditions, and radar characteristics of three tornadic circulations in Northeastern Henan

MA Huiyan   

  1. Puyang Meteorological Bureau,Puyang457000, China
  • Received:2025-10-29 Accepted:2026-05-13 Online:2026-07-06
  • Contact: MA Huiyan E-mail:25239692@qq.com

摘要: 为深入认识河南龙卷形成机理,提高龙卷监测预警业务精准性。利用常规气象探测资料、ERA5再分析资料、多普勒雷达等资料,对河南省东北部3次龙卷过程的环流背景、环境条件和雷达特征进行对比分析,凝练了本地龙卷预报预警指标。结果表明:(1)3次龙卷均发生于6~7月豫东北濮阳市平原地区,“22・6”及“23・7”龙卷出现于中午前后,“09・7”龙卷发生在傍晚,“09・7”、“23・7”龙卷伴随区域性短时强降水,“22・6”龙卷伴有局地短时强降水和小冰雹。(2) 3次龙卷过程虽均产生于东北冷涡背景下,但不同于高空冷平流强迫型“22・6”龙卷,“09・7”和“23・7”龙卷属于暖平流强迫型;三者均有地面辐合线或中尺度气旋为其提供动力条件。(3) 3次龙卷过程低抬升凝结高度和强低层垂直风切变,“09・7”、“23・7”龙卷近地面湿层厚、低层垂直风切变更强;而“22・6”龙卷干层明显且湿球零度层低,850和500 hPa温差最大。(4) 3次龙卷的对流母体在产生龙卷前均呈现回波中心增强并向弓形/钩状/涡旋状转型的特征,速度图上低层气旋性辐合与中层旋转上升共存,“22・6”龙卷回波强度最强,但涡旋特征弱且结构浅薄;“09・7”龙卷涡旋强度及旋转厚度最深厚型,速度切变最强;“23・7”龙卷回波强度最弱且TVS值最低,但垂直厚度较深厚。本研究为龙卷灾害性天气的预报预警服务提供参考依据。

关键词: 龙卷, 豫东北, 环流背景, 环境条件, 雷达特征

Abstract: To gain an in-depth understanding of the formation mechanisms of tornadoes in Henan and enhance the accuracy of tornado monitoring and early warning operations, this study comparatively analyzes the synoptic background, environmental conditions, and radar characteristics of three tornado events in northeastern Henan Province using conventional meteorological observations, ERA5 reanalysis data, and Doppler radar data, and summarizes local tornado forecasting and warning indicators. The results show that: (1) All three tornadoes occurred over the plain areas of Puyang City in northeastern Henan during June–July. The “22・6” and “23・7” tornadoes occurred around midday, whereas the “09・7” tornado occurred in the evening. The “09・7” and “23・7” events were accompanied by regional short-duration heavy rainfall, whereas the “22・6” tornado featured localized short-duration heavy rainfall and minor hail.(2) Although all three events developed under the influence of the Northeast China Cold Vortex, unlike the upper-level cold advection-forced “22•6” tornado, the “09•7” and “23•7” tornadoes were warm advection-forced. Surface convergence lines or mesoscale cyclones provided dynamic forcing for all events. (3) All three events exhibited low lifting condensation levels and strong low-level vertical wind shear. The “09・7” and “23・7” tornadoes featured thicker near-surface moisture layers and stronger low-level wind shear, whereas the “22・6” event showed a pronounced dry layer, a lower wet-bulb zero level, and the greatest temperature difference between 850 and 500 hPa. (4) Prior to tornadogenesis, the parent convective systems of all three events showed enhanced echo centers and evolved into bow-shaped, hook-shaped, or vortex-like structures. Velocity fields exhibited the coexistence of low-level cyclonic convergence and mid-level rotational ascent. The “22・6” event had the strongest echo intensity but weak vortex signatures and a shallow structure; the “09・7” tornado had the strongest vortex intensity and deepest rotational thickness; the “23・7” event had the weakest echo intensity and lowest tornado vortex signature value (potentially radar-limited), but a greater vertical depth. This study provides a reference for forecasting and warning services for tornadic severe weather.

Key words: tornado, Northeast Henan, synoptic background, environmental conditions, radar characteristics

中图分类号: 

  • P445

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