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A maximum entropy approach to satellite quantitative precipitation estimation (QPE)

机译:卫星定量降水估计(QPE)的最大熵方法

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摘要

This paper presents a new algorithm to generate quantitative precipitation estimates from infrared (IR) satellite imagery using passive microwave (PMW) data from Special Sensor Microwave/Imager sensor (SSM/I) satellites as ancillary information. To generate the estimates, we model the probabilistic distribution function (PDF) of the rainfall rates through the maximum entropy method (MEM), applying a cumulative histogram matching (HM) technique to the IR brightness temperatures. This results in a straightforward algorithm that can be formulated as an algebraic expression, providing a simple method to derive rainfall estimates using only IR data. The main application of the method is the direct estimation of rainfall rates and accumulated rainfall from geostationary satellites, providing appropriate temporal and spatial resolutions (up to 15min/4km when the Meteosat Second Generation satellite becomes available). The proposed method can be easily applied at GOES or current Meteosat satellite reception stations to generate instantaneous rainfall rates estimates with little computational cost. Here we provide examples of applications using the Global Infrared Database and Meteosat images. Our results have been compared with GOES Precipitation Index (GPI) and validated against Global Precipitation Climatology Centre (GPCC)-land rain gauge measurements, at 5°, monthly accumulations. We have obtained correlations of 0.88 for the algorithm, while the GPI yields correlations of 0.85. Preliminary comparisons with other algorithms over Australia also show how the performances of the algorithm are similar to those of more complex models. Finally, we propose some improvements and fine-tuning procedures that can be applied to the algorithm.
机译:本文提出了一种新算法,该算法使用来自特殊传感器微波/成像器传感器(SSM / I)卫星的被动微波(PMW)数据作为辅助信息,从红外(IR)卫星图像生成定量降水估算。为了生成估计值,我们通过最大熵方法(MEM)对降雨率的概率分布函数(PDF)建模,将累积直方图匹配(HM)技术应用于IR亮度温度。这样就产生了一种简单的算法,可以将其公式化为代数表达式,从而提供了一种仅使用IR数据得出降雨量估算值的简单方法。该方法的主要应用是直接估计对地静止卫星的降雨率和累积降雨,提供适当的时间和空间分辨率(当Meteosat第二代卫星可用时,可达15分钟/ 4公里)。所提出的方法可以容易地应用于GOES或当前的Meteosat卫星接收站,以很少的计算成本生成瞬时降雨率估计。在这里,我们提供了使用全球红外数据库和Meteosat图像的应用程序示例。我们的结果已与GOES降水指数(GPI)进行了比较,并通过全球降水气候中心(GPCC)的陆地雨量计测量得到了验证,该数据在5°时每月累积。该算法的相关系数为0.88,而GPI的相关系数为0.85。与澳大利亚其他算法的初步比较还表明,该算法的性能与更复杂模型的性能如何相似。最后,我们提出了一些可以应用于该算法的改进和微调程序。

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