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A Radar-based Technique for the Identiflcation of Convective and Stratiform Precipitation using the FLNN with Its Application to Estimation of Precipitation

机译:一种基于雷达的技术,用于鉴定使用Flynn的对流和层状沉淀,其应用于沉淀估算

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@@ 1. Introduction The improvement for radar data derived quantitative precipitation estimation (QPE) has been a challenge task in radar meteorology since the first weather radar was used to measure precipitation in 1940s (Cheng,1994). This is due to many factors affecting the accuracy for radar derived precipitation. One of most important factors is the variation of the relationship (Z-I) between radar observed reflectivity (Z) and precipitation intensity (l). It is generally accepted that the Z-l relationships may be much different for different precipitation types. Therefore, there have been many methods presented to classify the convective and stratiform precipitation echo of radar, which were use to estimate precipitation using different Z-/ relationships (Steiner et al., 1995, Rosenfeld et al. ,1995, Houze 1997, Biggerstaff et al. , 2000). Following this methodology in this paper, fuzzy neural network (FNN) was presented to identify precipitation types from radar echoes, which were applied to QPE using different Z-l relationships.
机译:@@ 1.引言雷达数据有所改善,得到的定量降水估计(QPE)已经在雷达气象学挑战的任务,因为第一个气象雷达是用来衡量在20世纪40年代(程,1994年)沉淀。这是因为影响了雷达的派生沉淀精度的因素很多。之一的最重要的因素是雷达观察到的反射率(Z)和降水强度(L)之间的关系(Z-Ⅰ)的变化。人们普遍认为,Z-L关系,对于不同类型的降水太大的不同。因此,已经有许多方法来给出分类对流和层状云降水雷达,这是使用以估计沉淀使用不同的Z- /关系(Steiner等,1995年,罗森菲尔德等人,1995年,1997年厚泽,比格斯塔夫的回声等人,2000)。继在本文所述方法,模糊神经网络(FNN)提出,从雷达回波,其使用不同的Z-L关系应用到QPE识别降水类型。

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