Echo Feature Identification for Short-time Heavy Precipitation with S-band Observations

Xu Yunong, Su Debin, L. Yue
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Abstract

Short-time heavy precipitation refers to a weather phenomenon in which the precipitation intensity is somewhat large in a short time, or the rainfall reaches or exceeds a certain value in the specified short time of period, which is an important indicator to evaluate the occurrence of severe convective weather. To address a process of precipitation in Beijing area, this paper studies the characteristics of weather radar echo under the condition of short-time heavy precipitation by using the ground rainfall observation from automatic weather station (AWS) network and the observations from the CINRAD-SA radar in Beijing area. A comparative analysis of a short-time heavy rainfall in Beijing area is conducted based on surface gauge and radar observations to investigate the temporal, spatial distributions of precipitation and the characteristics of radar echo above the surface stations, and the cross validation of AWS and SA radar data are carried out as well. For rainfall accumulation in 6min, the characteristics of ground precipitation were analyzed. Then, the consistency of radar products and ground precipitation characteristics were studied by analyzing the echo structure and its motion feature and matching quantitative precipitation estimation (QPE) products with surface rainfall observation. The result shows that the temporal and spatial distribution of short-time heavy precipitation have greater uncertainty, however, weather radar echo can reflect the characteristics of short-term heavy precipitation on the ground to a certain extent, and under the condition of short-term heavy precipitation, S-band radar QPE has a good consistency with the precipitation observed on the ground.
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短时强降水s波段回波特征识别
短时强降水是指在短时间内降水强度较大,或在规定的短时间内降雨量达到或超过一定数值的天气现象,是评价强对流天气发生的重要指标。针对北京地区的一次降水过程,利用自动气象站(AWS)地面降水观测资料和北京地区CINRAD-SA雷达观测资料,研究了短时强降水条件下的天气雷达回波特征。利用地面测量和雷达观测资料对北京地区一次短时强降水进行了对比分析,探讨了降水的时空分布和地面台站雷达回波特征,并对AWS和SA雷达资料进行了交叉验证。对于6min的降水积累,分析了地面降水特征。然后,通过分析回波结构及其运动特征,并将定量降水估计(QPE)产品与地面降水观测数据进行匹配,研究雷达产品与地面降水特征的一致性。结果表明,短时强降水的时空分布具有较大的不确定性,但气象雷达回波能在一定程度上反映地面短时强降水的特征,在短时强降水条件下,s波段雷达QPE与地面观测降水具有较好的一致性。
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