首页|基于S波段双偏振雷达的成都初春冰雹特征分析

基于S波段双偏振雷达的成都初春冰雹特征分析

扫码查看
为更好地开展成都冰雹天气的监测预报预警工作,利用成都S波段双偏振雷达探测资料,结合区域自动气象站以及常规观测资料,对成都初春冰雹的双偏振参量特征进行研究,重点分析冰雹云的精细结构,并与同年初春发生的短时强降水进行对比分析.结果表明:在高低空急流耦合形成强上升运动的动力条件下,高层冷平流结合地面冷空气共同触发了成都"3·16"冰雹天气.发展成熟的冰雹云,其中心反射率因子(ZH)超过70 dBZ且存在明显的悬垂强回波,差分反射率(ZDR)和相关系数(Correlation Coefficient,CC)分别集中在-2~1 dB和0.8~0.95,并伴有差分相移率(KDP)空洞和云体前侧的CC谷结构,同时在强上升气流附近存在典型的ZDR柱.伴随上升运动减弱,冰雹云前侧出现随距离递减的ZDR大值区,相反CC则呈现递增趋势.相较冰雹云,强降水对流云的ZH较小,而ZDR、CC明显偏大,且其前侧未出现悬垂强回波及明显的ZDR柱.
Characteristic analysis of early spring hail in Chengdu based on S-band polarization radar
In order to better carry out the monitoring,forecasting and early warning of hail weather in Chengdu,the characteristics of dual-polarization parameters of hail in early spring in Chengdu were studied by using the S-band dual-polarization radar detection of Chengdu,combined with the regional automatic weather station and conventional observation data.The fine structure of hail cloud was analyzed and compared with the short-term heavy precipitation in early spring of the same year.The results show that under the dy-namic condition of strong ascending motion formed by the coupling of the high and lower-level jets,the high-level cold advection com-bined with the surface cold air jointly triggered the hail weather of Chengdu"3·16".At the maturity stage,the central reflectivity factor(ZH)of hail cloud was more than 70 dBZ and there were obvious overhanging strong echo.Besides,the differential reflectivity(ZDR)and correlation coefficient(CC)of hail cloud were concentrated in-2-1 dB and 0.8-0.95,respectively,accompanied by specific differential phase shift rate(KDP)hole and CC valley structure in front of the cloud,and there was a typical ZDR column near strong updraft.With the weakening of the ascending motion,the ZDR large value area decreases with distance appeares in front of hail cloud,while CC shows in-creasing trend.Compared to hail cloud,the ZH of heavy precipitation convective cloud was smaller,while the ZDR and CC were signifi-cantly larger,and there was no overhanging strong echo and obvious ZDR column in front of the convective cloud.

dual-polarization radarhaildual-polarization signaturesChengdu

周聪、张涛、夏昕、张葵

展开 >

成都市气象台,四川 成都 610072

成都市气象局天府新区分局,四川 成都 610072

双偏振雷达 冰雹 偏振参量特征 成都

四川省科技计划重点研发项目高原与盆地暴雨旱涝灾害四川省重点实验室科技发展基金项目高原与盆地暴雨旱涝灾害四川省重点实验室科技发展基金项目

2023YFS0430SCQXKJYJXZD202308SCQXKJZD202103

2024

干旱气象
中国气象局兰州干旱气象研究所 中国气象学会干旱气象学委员会

干旱气象

CSTPCD
影响因子:1.9
ISSN:1006-7639
年,卷(期):2024.42(1)
  • 39