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气象:2022,48(9):1140-1152
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基于GPM/DPR数据的北疆地区降雪云宏观结构和微物理特征分析
王智敏,施丽娟,汪会,殷占福,李圆圆,冯婉悦
(中国气象局人工影响天气中心,北京 100081;新疆维吾尔自治区人工影响天气办公室,乌鲁木齐 830002;中国气象局气象探测中心,北京 100081;新疆维吾尔自治区气象技术装备保障中心,乌鲁木齐 830002)
Analysis of Macro Structure and Microphysical Characteristics of Snow Clouds in Northern Xinjiang Based on GPM/DPR Data
WANG Zhimin,SHI Lijuan,WANG Hui,YIN Zhanfu,LI Yuanyuan,FENG Wanyue
(CMA Weather Modification Centre, Beijing 100081;Xinjiang Weather Modification Office, Urumqi 830002;CMA Meteorological Observation Centre, Beijing 100081;Meteorological and Technical Equipment Support Center of Xinjiang, Urumqi 830002)
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投稿时间:2021-06-23    修订日期:2022-05-16
中文摘要: 利用GPM/DPR双频降水雷达资料、FY-2E卫星资料和地面降水实况,对新疆北部四次成熟期降雪过程的红外亮温、水平分布和垂直结构特征进行了分析。结果表明:降雪云团的云顶亮温集中在210~245 K,降雪云主要为层状云,中云对降水率贡献最大,近地面降水率多分布于0.5~2.0 mm·h-1,回波顶高主要集中在3.0~4.5 km范围内,回波顶高与近地表降水率强弱变化存在正相关;雷达反射率因子(Z)范围在22~35 dBz,强回波中心高度主要分布在1.25~4.50 km;质量加权平均直径(Dm)为1.01~1.25 mm和粒子数浓度(dBNw)为32~36的配置贡献的降水最多,对应的高度范围为2.19~2.50 km和2.13~2.67 km;近地表由碰撞-聚并过程产生的大粒子较多,近地表附近Dm达到了2.33~3.00 mm,Z和Dm朝地面几乎恒定或稍有增加,Z和Dm数值大小与地表降水量变化呈正相关特征。
Abstract:Based on GPM/DPR dual-frequency precipitation radar, FY-2E satellite and surface precipitation data, the infrared brightness temperature, horizontal distribution and vertical structure characteristics of the four snowfall processes during mature period in northern Xinjiang are analyzed. The results show that the cloud top brightness temperature of the snowfall is concentrated at 210-245 K, and the snowfall clouds are mainly stratiform clouds. The middle clouds contribute the most to the precipitation intensity, and the near-surface precipitation rate is mostly distributed between 0.5-2.0 mm·h-1. The echo top height in areas with high precipitation rate is mainly concentrated in the range of 3.0-4.5 km, and there is a positive correlation between the echo top height and the variation of near-surface precipitation rate. The range of radar reflectivity factor (Z) is between 22-35 dBz, and the height of the strong echo center is mainly distributed in 1.25-4.50 km. The configuration with mass weighted average diameter (Dm) of 1.01-1.25 mm and particle number concentration (dBNw) of 32-36 contributes the most precipitation, and the corresponding heights are 2.19-2.50 km and 2.13-2.67 km. Near the surface, there are more large particles produced by the collision-convergence process, and the Dm reaches 2.33-3.00 mm near surface. Toward the surface, Z and Dm are almost constant or slightly increase, and the values of Z and Dm are positively correlated to the variation of surface rainfall.
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基金项目:国家重点研发计划(2018YFC0406602)、中国气象局云雾物理环境重点开放实验室开放课题(2020Z00712)、中国气象局西北区域人影建设研究试验项目(RYSY201902)和新疆气象局引导性计划项目(YD202201、YD202203)共同资助
引用文本:
王智敏,施丽娟,汪会,殷占福,李圆圆,冯婉悦,2022.基于GPM/DPR数据的北疆地区降雪云宏观结构和微物理特征分析[J].气象,48(9):1140-1152.
WANG Zhimin,SHI Lijuan,WANG Hui,YIN Zhanfu,LI Yuanyuan,FENG Wanyue,2022.Analysis of Macro Structure and Microphysical Characteristics of Snow Clouds in Northern Xinjiang Based on GPM/DPR Data[J].Meteor Mon,48(9):1140-1152.