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曾震瑜, 刘黎平, 郑佳锋, 邹明龙, 李博勇. 2021: 星载雷达DPR与地基雷达CR的匹配对比及系统偏差初探. 暴雨灾害, 40(3): 287-296. DOI: 10.3969/j.issn.1004-9045.2021.03.007
引用本文: 曾震瑜, 刘黎平, 郑佳锋, 邹明龙, 李博勇. 2021: 星载雷达DPR与地基雷达CR的匹配对比及系统偏差初探. 暴雨灾害, 40(3): 287-296. DOI: 10.3969/j.issn.1004-9045.2021.03.007
ZENG Zhenyu, LIU Liping, ZHENG Jiafeng, ZOU Minglong, LI Boyong. 2021: Matching comparison between Satellite radar DPR and ground-based radar CR and preliminary study of systematic error. Torrential Rain and Disasters, 40(3): 287-296. DOI: 10.3969/j.issn.1004-9045.2021.03.007
Citation: ZENG Zhenyu, LIU Liping, ZHENG Jiafeng, ZOU Minglong, LI Boyong. 2021: Matching comparison between Satellite radar DPR and ground-based radar CR and preliminary study of systematic error. Torrential Rain and Disasters, 40(3): 287-296. DOI: 10.3969/j.issn.1004-9045.2021.03.007

星载雷达DPR与地基雷达CR的匹配对比及系统偏差初探

Matching comparison between Satellite radar DPR and ground-based radar CR and preliminary study of systematic error

  • 摘要: 将GPM(Global Precipitation Measurement)卫星搭载的双频降水雷达DPR(Dual-frequency Precipitation Radar)和广东龙门观测站的地基Ka/Ku双波段雷达CR(Cloud Rader)在2019年4—9月的观测数据进行时空匹配,结合微雨雷达MRR(Micro Rain Rader)的雨滴谱数据对CR衰减订正处理,比较DPR与CR探测回波强度差异,最后对两者的系统偏差进行分析。结果表明:(1)DPR和CR探测到的回波强度随高度变化的趋势大体一致,零度层亮带高度基本一致,同样高度下DPR探测到的回波强度明显大于CR。(2)统计弱的非降水云算得CR双频系统偏差约为3.1 dBz。(3)雨强越强,CR天线罩水膜厚度越大,回波衰减越大。(4)逐库订正过程中利用雨滴谱数据计算衰减系数,CR在Ka与Ku波段的反射率因子订正量不超过4 dBz。(5)综合所有适配数据,CR与DPR的反射率因子在Ka波段内订正后平均系统偏差为15.7 dBz,在Ku波段内订正后平均系统偏差为14.4 dBz。虽然经订正处理后两部雷达间的系统偏差偏大,但对改善地基Ka/Ku双波段雷达的数据质量有明显的改善。

     

    Abstract: In this paper, the observation data measured by the dual-frequency precipitation radar DPR on board the GPM satellite and the ground-based Ka/Ku dual-band radar CR of the Guangdong Longmen Observatory from April to September 2019 are matched in time and space. Combining with the raindrop spectrum data of the micro rain radar MRR for the CR attenuation correction, we compare the difference of echo intensity detected by DPR and CR, and analyze the systematic differences between the two. The main result are as follows:(1) The distributions of precipitation echoes detected by DPR and CR have similar trends with height. The height of the brightband is basically the same. The echo intensity detected by DPR at the same altitude is significantly greater than that of CR.(2) For non-precipitating clouds, the systematic difference between Ku band and Ka band in CR is about 3.1 dBz.(3) The stronger the rainfall intensity, the greater the thickness of the water film of the CR's radome, and the greater the attenuation of the CR echo.(4) The raindrop spectrum data are used to calculate the attenuation coefficient in the process of bin by bin library correction, and the correction amount of the reflectivity factor of CR in the Ka and Ku bands does not exceed 4 dBz.(5) Integrating all the collocated data, the average systematic difference between the reflectivity factors of CR and DPR after the attenuation correction for the Ka band is 15.7 dBz, and that for the Ku band is 14.4 dBz. Although the systematic difference between the two radars after attenuation correction is still large, these results have significantly improved the data quality of the ground-based Ka/Ku dual-band radar.

     

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