首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >New paradigm for statistical validation of satellite precipitation estimates: Application to a large sample of the TMPA 0.25° 3-hourly estimates over Oklahoma
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New paradigm for statistical validation of satellite precipitation estimates: Application to a large sample of the TMPA 0.25° 3-hourly estimates over Oklahoma

机译:卫星降水估计数据统计验证的新范例:在俄克拉荷马州大样本TMPA 0.25°3小时估计中的应用

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It is well acknowledged that space-based and ground-based radar estimates of rainfall are both affected by several sources of uncertainties; nevertheless, the latter are generally used as ground reference for the validation of the former. In this way, it is difficult to assess what portion of the observed discrepancies is solely due to the targeted satellite errors and what is the impact of the radar-rainfall errors. The authors propose a novel approach for the validation of satellite-based rainfall estimates, in which an empirically based radar-rainfall error model is used to account for deterministic and random uncertainties in radar-rainfall estimates. Using an easy-to-interpret metric, the approach can be used to answer probabilistic questions such as "Given radar and satellite rainfall estimates, what is the probability that the true rainfall is larger (smaller) than the satellite estimate"? The results are based on a large sample (6 years) of the Tropical Rainfall Measuring Mission (TRMM) Multisatellite Precipitation Analysis (TMPA) 0.25-degree 3-hourly satellite-rainfall estimates and hourly radar-rainfall product (aggregated at the satellite space-time scale) from the Oklahoma City WSR-88D radar (KTLX). This study shows how the TMPA satellite product tends to overestimate the high rainfall values and underestimate the low values and how it tends to perform better during the hot season (June to September). Moreover, the authors demonstrate how the presence of errors in the ground-based radar could significantly affect the results of the satellite product evaluation.
机译:众所周知,天基和地基雷达对降雨的估计都受到多种不确定性因素的影响;但是,后者通常被用作对前者进行验证的基础参考。这样,很难评估观察到的差异的哪一部分完全是由于目标卫星误差,以及雷达降雨误差的影响是什么。作者提出了一种新颖的方法来验证基于卫星的降雨估计,其中,基于经验的雷达降雨误差模型用于解释雷达降雨估计中的确定性和随机不确定性。使用一种易于理解的度量标准,该方法可用于回答概率问题,例如“给出雷达和卫星的降雨量估计值,那么实际降雨量大于(小于)卫星估计值的概率是多少?”结果是基于热带降雨测量任务(TRMM)多卫星降水分析(TMPA)0.25度的3小时每小时卫星降雨估计值和每小时雷达降雨产物的总样本(6年)(在卫星空间-时间刻度)来自俄克拉荷马城WSR-88D雷达(KTLX)。这项研究表明TMPA卫星产品如何倾向于高估高降雨值而低估低降雨值,以及在高温季节(6月至9月)如何表现更好。此外,作者演示了地面雷达中错误的存在如何严重影响卫星产品评估的结果。

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