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通辽市两次特大暴雪天气过程的卫星云图和雷达回波特征分析

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利用常规观测资料、ERA5(0.25˚×0.25˚)逐1 小时再分析资料,对通辽市2020 年 11 月 17-19 日特大暴雪天气过程(过程 1)和 2021 年 11 月 6-10 日特大暴雪天气过程(过程 2)卫星云图和水汽图和雷达回波特征进行对比分析.结果表明:高空深厚冷涡(低槽)强烈发展和气旋入海后爆发性发展,强劲低空急流近距离输送充沛水汽是两次特大暴雪的有利环流形势.两次特大暴雪过程卫星云图出现斜压叶状云系演变为逗点云系再演变为螺旋云系,有明显的T形结构和暖锋后弯特征.降雪前期是回流降雪,降雪后期是冷输送带降雪.卫星云图各演变阶段较好地对应降雪的开始、加强、减弱等.在高空冷涡(低槽)强烈发展阶段,在冷涡的东南部—东北部—西北部有涡旋云系,对应降雪最强阶段.过程 2 的螺旋云带比过程 1 的螺旋云带更明显,降雪持续时间也较长.两次特大暴雪过程雷达回波呈均匀分布的片状层状云降水回波,回波强度变化和降雪大小有很好对应关系.过程1出现了典型的"零度层亮带",探空图有逆温层和融化层,"零度层亮带"和融化层均较好的指示降水相态.过程 2 回波移动与风场旋转一致,回波动画图呈现出气旋式旋转,回波的发展演变与冷涡强烈发展并旋转东移北上一致.
The Analysis of the Satellite Cloud Images and Radar Echo Characteristics of Two Excessive Snowstorms in TongLiao
The characteristics of satellite water vapor images and radar echoes of the excessive snowstorm processes during November 17 to 19,2020 and November 6 to 10,2021 in Tongliao were analyzed and compared,based on conventional observation data and ERA5(0.25˚×0.25˚)reanalysis data.The results showed that the favorable circulation patterns for both excessive snowstorms included the intense development of high-altitude cold vortex(low trough)and cyclone,and the close-range transport of abundant water vapor by low-level jet.The satellite cloud images of two excessive snowstorms showed a transition from baroclinic leaf cloud system to comma cloud system,and finally to spiral cloud system,with distinct T-shaped structures and back-bent warm fronts.The initial stage of snowfall was characterized by return flow snowfall,while the later stage was dominated by cold conveyor belt.The evolution stages of the satellite cloud images corresponded well to the beginning,strengthening,and weakening of snowfall.In the intense development stage of the high-altitude cold vortex(low trough),vortex cloud systems were observed in the southeast,northeast,and northwest of the cold vortex,corresponding to the strongest snowfall stage.The spiral cloud belt in the second snowstorm process was more obvious than that in the first snowstorm process,and the snowfall duration was also longer.The radar echoes of two excessive snowstorm processes were uniformly distributed flaky stratiform cloud precipitation echoes,with a good correlation between echo intensity and snowfall intensity.The first snowstorm process featured a typical zero-layer bright band,an inversion layer and a melting layer,which provided good indicators of precipitation phase.The echo movement of the second snowstorm process was consistent with wind field rotation,which showed a cyclonic rotation,while the evolution of the echoes were in line with the intense development and rotation of the cold vortex as it moved eastwards and northwards.

Excessive snowstormCharacteristics of water vapor cloud imagesRadar echoes characteristics

赵梅兰、祁雁文、张晨

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通辽市气象局,内蒙古 通辽 028000

特大暴雪 水汽云图特征 雷达图特征

2024

内蒙古气象
内蒙古气象局 内蒙古气象气象学会

内蒙古气象

影响因子:0.206
ISSN:1005-8656
年,卷(期):2024.(6)