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一种短时强降水雷达客观识别方法研究

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文章统计分析了 2004-2021年6-8月凉城地区43次短时强降水,367条回波强度廓线数据,通过对雷达回波廓线分析,提取描述回波廓线底层回波强度等6个参量,确定凉城地区出现短时强降水的识别阈值.结果表明:雷达回波强度廓线近地面1 km回波强度分布比较均匀,以中位数为中心,均匀向两端分布,Zmax、ET、TOP、VIL、KILD分布较不均匀,均呈右偏,其中VIL、VILD分布右偏严重,Z、Zmax、VIL、VILD数据分布呈单峰状,ET、TOP数据分布呈双峰状;在雷达回波强度廓线特征量小提琴图形分析基础上,采用25%分位数作为雷达识别短时强降水参数阈值,初选出阈值为:廓线强度最大值>26.1dBz,廓线近地面 1km 回波强度>24.2dBz,ET>5.3 km,TOP>2.0 km,VIL>0.2 kg·m2,VILD>0.06g·m3,阈值总体上低于我国中东部地区;应用2017年6-8月样本进行检验,凉城地区雨强R≥10.0 mm·h-1及4.9 mm·h-1 ≤R<10.0 mm·h-1预报命中率、空报率明显高于一般性降水(1.0 mm·h-1≤R<4.9 mm·h-1),漏报率明显低于一般性降水.短时强降水逐小时TS评分小于0.15,一般性降水逐小时TS评分为0.46.运用此方法对提高凉城地区短时强降水预报命中率有一定的参考价值.
An Objective Identification Method on Short-term Heavy Rainfall Based on Radar
Based on 367 echo intensity profile data,43 short-term heavy rainfall events in Liangcheng area from June to August between 2004 and 2021 were statistically analyzed.Six parameters describing the bottom echo intensity and other aspects of the echo profiles were extracted to determine the identification thresholds for short-term heavy rainfall in Liangcheng,by analyzing radar echo profiles.The results showed that the echo intensity distribution of radar echo profiles within 1 km above ground was relatively uniform,with the median as the center,evenly distributed towards both ends.The distributions of Zmax,ET,TOP,VIL,and VILD were relatively uneven,which were all skewed to the right,with VIL and VILD exhibiting severe right skewness.The Z,Zmax,VIL,and VILD showed unimodal characteristics,while ET and TOP showed bimodal characteristics.Based on the violin graphic analysis of radar echo intensity profile characteristics,the 25th percentile was used as the identification threshold for short-term heavy rainfall.The selected thresholds were maximum profile intensity>26.1 dBz,echo intensity with 1 km above ground>24.2 dBz,ET>5.3 km,TOP>2.0 km,VIL>0.2 kg·m-2,and VILD>0.06 g,m-3.These thresholds were generally lower than those in central and eastern China.The identification effects of these thresholds on short-term heavy rainfalls from June to August in 2017 were evaluated.It was found that the hit ratios and false alarm ratios of rainfalls with R≥10.0 mm·h-1 and 4.9 mm·h-1≤R<10 mm·h-1 were significantly higher than those of rainfalls with R between 1.0 mm·h-1 and 4.9 mm·h-1,while the missed forecast ratios were significantly lower.The hourly TS of short-term heavy rainfall was less than 0.15,and the hourly TS of general precipitation was 0.46.The application of this method had a certain reference value for improving the forecast accuracy of short-term heavy rainfall in Liangcheng area.

Short-term heavy rainfallObjective methodIdentification threshold

刘诗韵、许晶、贾雪婷、姬佳琪、高帆

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乌兰察布市气象局,内蒙古乌兰察布 012000

鄂尔多斯市气象局,内蒙古鄂尔多斯 017010

商都县气象局,内蒙古 商都 013400

兴安盟气象局,内蒙古乌兰浩特 137400

成都信息工程大学大气科学学院,四川成都 610225

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短时强降水 客观方法 识别阈值

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.(5)