滕州一次特大冰雹超级单体风暴参数演变的偏振雷达观测分析
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1.山东省气象防灾减灾重点实验室;2.山东科技大学测绘与空间信息学院;3.厦门市气象局

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P412.25

基金项目:

山东省自然科学基金面上项目(ZR2020MD052,ZR2021MD121,ZR2022MD072);国家自然科学基金(41675029);厦门市科技局项目(3502Z20214ZD4005),山东省气象局重点项目(2021sdqxz09,SDLD2022-02)


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Polarization radar observation and analysis of parameter evolution of a supercell storm with giant hail in Tengzhou
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    摘要:

    为为揭示产生直径7 cm及以上冰雹超级单体风暴的环境及雷达参量特征,基于济宁S波段双偏振雷达数据,结合探空和地面实况资料,对发生在滕州的一次特大冰雹超级单体风暴的环境物理量、风暴参数演变及偏振参量特征进行了分析。结果表明:(1)滕州强冰雹风暴产生在强的对流有效位能和中等强度深层垂直风切变环境条件下,850 hPa与500 hPa温差ΔT较大,对流层中上层较干,低层暖湿。(2)产生直径7 cm及以上冰雹的滕州超级单体风暴,由于大的冰雹浓度低造成降雹时平均最大反射率因子较低(64.82 dBZ),但具有较高的C-VIL(平均值82 kg·m-2)、ZDR柱深度(平均值2 km)及中气旋最大旋转速度(平均值25.2 m?s?1),意味存在较强上升气流可以托住大的冰雹。(3)ZDR柱顶高持续增高,同时C-VIL维持在80 kg·m-2以上,对特大冰雹产生与预警具有指示意义。ZDR柱顶高持续增高,表明风暴内上升气流强度持续加强,风暴会进一步发展。C-VIL维持在高值区,说明风暴具有丰富的冰雹粒子,出现特大冰雹的概率较高。(4)风暴发展旺盛阶段,超过60 dBZ强回波厚度接近8km,顶部到达10km左右高度,说明大冰雹已在高层生成,并同时有冰雹降到低层,揭示了冰雹云发展维持从而地面不断降雹的机制。

    Abstract:

    Abstract In order to reveal the environmental and radar parameter characteristics of a super hailstorm with hailstorms over 7cm and above, based on S-band dual-polarization radar data in Jining, combined with sounding and ground reality data, the environmental physical parameters, storm parameter evolution and polarization parameter characteristics of a super hailstorm in Tengzhou were analyzed.The results show that: (1) The Tengzhou severe hail storm occurred under strong convective effective potential energy and moderate intensity deep vertical wind shear environmental conditions,with relatively large temperature difference between 850 hPa and 500 hPa , drier middle and upper troposphere, warmer and wetter lower troposphere (2)Tengzhou supercell storm producing hail with a diameter of 7 cm or more has a lower average maximum reflectance factor (64.82 dBZ) due to the low concentration of larger hail, but with the higher C-VIL (average 82 kg·m-2), ZDR deep( average 2 km) and maximum rotation velocity of the medium cyclone (average 25.2 m?s?1) which mean that there is a strong updraft supporting larger hail. (3) The top height of the ZDR column continues to increase Indicating that the intensity of updrafts within the storm continues to strengthen and the storm will further develop, while the C-VIL remains above 80 kg·m-2, which has indicative significance for the occurrence and warning of severe hail.The C-VIL remains in the high-value area, indicating that the storm has abundant hail particles and a higher probability of experiencing severe hail.(4)During the vigorous stage of storm development, the strong echo thickness exceeding 60 dBZ is close to 8 km and the top reaches a height of about 10 km indicating that large hail has been generated in the upper layers, at the same time, hail descended to the lower layers,that revealed the mechanism of sustained development of hail clouds and continuous hail on the ground.

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  • 收稿日期:2024-05-17
  • 最后修改日期:2024-12-17
  • 录用日期:2025-04-11
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