首页|FY-3G降水测量雷达海洋定标精度检验与评估

FY-3G降水测量雷达海洋定标精度检验与评估

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2023年4月发射的风云三号气象卫星G星(FY-3G)是我国首颗专用降水测量卫星,双频降水测量雷达(pre-cipitation measurement radar,PMR)是该颗卫星上最核心的仪器.基于2023年7月数据,利用海洋定标理论模型,模拟海洋表面后向散射截面,与观测海洋表面后向散射截面进行比对,实现对PMR定标精度的初步评估.通过与国外星载双频降水测量雷达(global precipitation measurement,dual-frequency precipitation radar,GPM DPR)海洋定标检验结果比对,评估FY-3G PMR定标的准确性.海洋定标精度检验结果表明:FY-3G PMR Ku波段在入射角小于15°时观测值与模型模拟值的偏差较小,此时FY-3G PMR的偏差为1.65~2.73 dB,偏差标准差为0.74~1.82 dB.FY-3G PMR Ka波段在18°入射角时偏差小于0.27 dB,偏差的标准差为3.49 dB.FY-3G PMR与GPM DPR的定标偏差存在较为固定的偏差,差异主要源自于数据本身的后向散射统计特性,各入射角下FY-3G PMR Ku与Ka波段海洋表面后向散射数据稳定性与GPM DPR相当.
Validation and Evaluation of Ocean Calibration Accuracy of FY-3G Precipitation Measurement Radar
FY-3G precipitation satellite launched in April 2023 is the first dedicated precipitation measurement satellite in China.The dual-frequency precipitation measurement radar(PMR)is the core instrument on the satellite.Because the backscattering performance of the vast ocean area is relatively stable,the calibra-tion accuracy of the on-orbit radar can be tested by studying the backscattering cross-section of the sea sur-face.FY-3G PMR level 1 data in July 2023 and GPM DPR(global precipitation measurement,dual-fre-quency precipitation radar)level 2A data are used to analyze the mean value and mean square error of the global sea surface backscattering cross section under no-rain conditions to evaluate the radar performance.At the same time,the theoretical model of ocean surface backscattering is studied to simulate the sea sur-face backscattering cross-section under the condition of no rain,and the sea surface backscattering cross-section is compared with the actual radar measurement,so as to realize the preliminary evaluation of FY-3G PMR calibration accuracy.Furthermore,the accuracy of FY-3G PMR calibration is evaluated by the ocean calibration test results of GPM DPR data.Test results of ocean calibration accuracy show that when the incidence angle of FY-3G PMR Ku-band is less than 15°,the deviation between the observed value and the model simulation value is small.The deviation of FY-3G PMR ranges from 1.65 to 2.73 dB,while the standard deviation ranges from 0.74 to 1.82 dB.The deviation of FY-3G PMR Ka-band at an 18° incidence is less than 0.27 dB,and the standard deviation of the deviation is 3.49 dB.The calibration deviation of FY-3G PMR and GPM DPR is relatively constant,with the difference is primarily attributed to the back-scattering statistical characteristics of the data itself.The stability of the backscattering data of FY-3G PMR Ku-and Ka-band sea surfaces at each incidence angle is comparable to that of GPM DPR.Gas attenu-ation is not considered at the moment.In the future,the impact of gas attenuation on the Ku-and Ka-band ocean calibration accuracy validation will be further evaluated,and the systematic deviation of FY-3G PMR will be corrected.

precipitation measurement radarFY-3Gbackscattering cross sectionocean calibrationac-curacy validation

袁梅、尹红刚、商建、江柏森、杨润峰、谷松岩、张鹏

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国家卫星气象中心(国家空间天气监测预警中心),北京 100081

许健民气象卫星创新中心,北京 100081

中国气象局遥感卫星辐射测量和定标重点开放实验室,北京 100081

北京遥测技术研究所,北京 100076

中国气象局气象探测中心,北京 100081

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降水测量雷达 FY-3G 后向散射截面 海洋定标 精度检验

2024

应用气象学报
中国气象科学研究院 国家气象中心 国家卫星气象中心 国家气候中心 国家气象信息中心 中国气象局气象探测中心

应用气象学报

CSTPCD北大核心
影响因子:1.459
ISSN:1001-7313
年,卷(期):2024.35(5)