2024年7月山东龙卷群发事件的可能成因:Rossby波包活动与中小尺度条件OA
Possible causes of tornado outbreak in Shandong Province in July 2024:Rossby wave packets and convective conditions
龙卷事件致灾性极强,本文基于ERA5 再分析数据集,研究了龙卷事件中对流层上层Rossby波包的传播特征及其对龙卷生成的可能影响,并分析了2024 年7 月5 日山东龙卷群发事件中龙卷发生潜势的多项物理参数指标.结果表明:此次事件由西南涡加深形成的温带气旋引发,而Rossby波包对温带气旋的增强起到了重要作用.对流层上层Rossby波包起源于巴尔喀什湖地区,以每天13.3 经距的群速度沿巴尔喀什湖—天山山脉—河套地区—山东路径传播,于 7 月 5 日抵达菏泽上空.波包对菏泽地区环流扰动的影响使得上层反气旋环流与低层气旋环流的扰动增强,有利于深厚上升气流的形成与维持.低空急流与中上层西风槽共同作用有利于超级单体发展;中小尺度环境条件显示,菏泽地区对流有效位能(CAPE)峰值接近2 500 J·kg-1,低层垂直风切变(SHR1)超过10 m·s-1,低层风暴相对螺旋度(SRH1)与合成指标强龙卷指标(STP)、超级单体复合指数(SCP)、低层能量—螺旋度指标(EHI1)在龙卷发生前显著超过阈值,较为精确地指示了强龙卷发生的潜势.研究结果利于加深对龙卷形成机理的理解并为预报提供科学线索.
Tornadoes are well known as the extremely strong convective systems that usually caused severe disasters and huge economic losses.On 5 July 2024,Shandong experienced an outbreak event of tornadoes.By using the daily and hourly atmospheric dataset from ERA5 reanalysis,the possible causes of this tornado outbreak event were investigated by analyzing changes in the potential parameters of convective conditions and the propagation of Rossby wave packets in the upper troposphere.Results demonstrate that the tornado outbreak was triggered by a deepening extratropical cyclone originating from a southwest vortex that migrated eastward from Sichuan Basin.The strengthening of this extratropical cyclone was caused by the eastward propagation of upper tropospheric Rossby wave packet at a group velocity of 13.3° longitude per day.This wave packet originated from the Balkhash Lake region on July 2 and migrated eastward along the path of Balkhash Lake-Tianshan Mountains-Hetao Region-Shandong Province.As the wave packet reached Heze city on July 5,the outbreak of tornadoes occurred.This Rossby wave packet approaching Heze strengthened both the anticyclonic disturbancein the upper troposphere and the cyclonic circulation system in the lower troposphere,facilitating the formation and maintenance of deep convection.Moreover,the combined effects of the low-level jet stream and the mid-upper-level trough were also conducive to the development of supercells.Occurrences of tornadoes were intrinsically determined by meso-and micro-scale environmental conditions.The maximum Convective Available Potential Energy(CAPE)in the Heze area approached 2 500 J·kg-1 whereas the low-level vertical wind shear(SHR1)exceeded 10 m·s-1.Low-level storm relative helicity(SRH1),Significant Tornado Parameter(STP),Supercell Composite Parameter(SCP),and low-level energy-helicity index(EHI1)significantly surpassed their respective thresholds prior to the tornado occurrence,accurately indicating the strong potential for tornado outbreak in this Heze area.All results above are helpful to deepen the understanding of tornado genesis and provide usefulscientific clues to forecastingoccurrences of tornado events.
戴昊乐;管兆勇;叶德超
南京信息工程大学 气候系统预测与变化应对全国重点实验室/气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心,南京 210044南京信息工程大学 气候系统预测与变化应对全国重点实验室/气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心,南京 210044南京信息工程大学 气候系统预测与变化应对全国重点实验室/气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心,南京 210044
天文与地球科学
Rossby波包龙卷潜势指标夏季山东省
Rossby wave packetstornadopotential parameterboreal summerShandong Province
《气象科学》 2026 (1)
34-47,14
国家重点研发计划重点专项(2019YFC1510201)公益性行业(气象)科研专项(GYHY201406024)江苏省PAPD项目
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