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Evaluation of Precipitation Estimates by at-Launch Codes of GPM/DPR Algorithms Using Synthetic Data from TRMM/PR Observations

机译:使用来自TRmm / pR观测的合成数据的Gpm / DpR算法的启动代码评估降水估计

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摘要

The Global Precipitation Measurement (GPM) Core Observatory will carry a Dual-frequency Precipitation Radar (DPR) consisting of a Ku-band precipitation radar (KuPR) and a Ka-band precipitation radar (KaPR). In this study, 'at-launch' codes of DPR precipitation algorithms, which will be used in GPM ground systems at launch, were evaluated using synthetic data based upon the Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (PR) data. Results from the codes (Version 4.20131010) of the KuPR-only, KaPR-only, and DPR algorithms were compared with 'true values' calculated based upon drop size distributions assumed in the synthetic data and standard results from the TRMM algorithms at an altitude of 2 km over the ocean. The results indicate that the total precipitation amounts during April 2011 from the KuPR and DPR algorithms are similar to the true values, whereas the estimates from the KaPR data are underestimated. Moreover, the DPR estimates yielded smaller precipitation rates for rates less than about 10 mm/h and greater precipitation rates above 10 mm/h. Underestimation of the KaPR estimates was analyzed in terms of measured radar reflectivity ({f Z}-{f m}) of the KaPR at an altitude of 2 km. The underestimation of the KaPR data was most pronounced during strong precipitation events of {f Z}-{f m} lt {f 18}~{f dBZ} (high attenuation cases) over heavy precipitation areas in the Tropics, whereas the underestimation was less pronounced when the {f Z}-{f m}gt 26~{f dBZ} (moderate attenuation cases). The results suggest that the underestimation is caused by a problem in the attenuation correction method, which was verified by the improved codes.
机译:全球降水测量(GPM)核心观测站将搭载双频降水雷达(DPR),该雷达由Ku波段降水雷达(KuPR)和Ka波段降水雷达(KaPR)组成。在这项研究中,将使用基于热带降雨测量任务(TRMM)降水雷达(PR)数据的合成数据对将在发射时在GPM地面系统中使用的DPR降水算法的“启动”代码进行评估。将仅使用KuPR,仅使用KaPR和DPR算法的代码(版本4.20131010)的结果与基于真实数据中假定的墨滴大小分布计算的“真实值”以及TRMM算法在海拔高度为2的标准结果进行计算海洋2公里。结果表明,KuPR和DPR算法在2011年4月的总降水量与真实值相似,而KaPR数据的估算值却被低估了。此外,DPR估算得出,当速率低于约10 mm / h时,降水量较小,而高于10 mm / h时,降水量较大。根据在2 km高度下KaPR的实测雷达反射率({ bf Z}-{ bf m})分析了KaPR估计的低估。在热带地区强降水地区{{bf Z}-{ bf m} lt { bf 18}〜{ bf dBZ}(高衰减情况)的强降水事件中,KaPR数据的低估最为明显,而当{ bf Z}-{ bf m} gt 26〜{ bf dBZ}(中等衰减情况)时,低估不那么明显。结果表明,低估是由衰减校正方法中的一个问题引起的,这已通过改进代码进行了验证。

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