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首页> 外文期刊>Journal of hydrometeorology >Assessment of SCaMPR and NEXRAD Q2 Precipitation Estimates Using Oklahoma Mesonet Observations
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Assessment of SCaMPR and NEXRAD Q2 Precipitation Estimates Using Oklahoma Mesonet Observations

机译:使用俄克拉荷马州Mesonet观测值评估SCaMPR和NEXRAD Q2降水估计

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Although satellite precipitation estimates provide valuable information for weather and flood forecasts, infrared (IR) brightness temperature (BT)-based algorithms often produce large errors for precipitation detection and estimation during deep convective systems (DCSs). As DCSs produce greatly varying precipitation rates below similar IR BT retrievals, using IR BTs alone to estimate precipitation in DCSs is problematic. Classifying a DCS into convective-core (CC), stratiform (SR), and anvil cloud (AC) regions allows an evaluation of estimated precipitation distributions among DCS components to supplement typical quantitative precipitation estimate (QPE) evaluations and to diagnose these IR-based algorithm biases. This paper assesses the performance of the National Mosaic and Multi-Sensor Next Generation Quantitative Precipitation Estimation System (NMQ Q2), and a simplified version of the Self-Calibrating Multivariate Precipitation Retrieval (SCaMPR) algorithm, over the state of Oklahoma using Oklahoma Mesonet observations. While average annual Q2 precipitation estimates were about 35% higher than Mesonet observations, strong correlations exist between these two datasets for multiple temporal and spatial scales. Additionally, the Q2-estimated precipitation distribution among DCS components strongly resembled the Mesonet-observed distribution, indicating Q2 can accurately capture the precipitation characteristics of DCSs despite its wet bias. SCaMPR retrievals were typically 3-4 times higher than Mesonet observations, with relatively weak correlations during 2012. Overestimates from SCaMPR retrievals were primarily caused by precipitation retrievals from the anvil regions of DCSs when collocated Mesonet stations recorded no precipitation. A modified SCaMPR retrieval algorithm, employing both cloud optical depth and IR temperature, has the potential to make significant improvements to reduce the wet bias of SCaMPR retrievals over anvil regions of a DCS.
机译:尽管卫星降水估算为天气预报和洪水预报提供了有价值的信息,但是基于红外(IR)亮度温度(BT)的算法通常会在深度对流系统(DCS)期间为降水检测和估算产生较大的误差。由于DCS产生的降水速率大大低于类似的IR BT检索值,因此仅使用IR BT估算DCS的降水量是有问题的。将DCS分为对流核心(CC),层状(SR)和砧云(AC)区域,可以评估DCS组件之间的估计降水分布,以补充典型的定量降水估计(QPE)评估并诊断这些基于红外的算法偏差。本文使用俄克拉荷马州Mesonet观测资料评估了俄克拉荷马州国家镶嵌和多传感器下一代定量降水估算系统(NMQ Q2)的性能以及自校正多元降水检索(SCaMPR)算法的简化版本。 。虽然第二季度的年平均降水量估计数比Mesonet观测值高约35%,但这两个数据集之间在多个时空尺度上都存在很强的相关性。另外,Q2估计的DCS组件之间的降水分布与Mesonet观测到的分布非常相似,这表明Q2可以精确捕获DCS的降水特征,尽管存在湿偏。 SCaMPR反演通常是Mesonet观测值的3-4倍,在2012年间相关性相对较弱。SCaMPR反演的高估主要是由于并置Mesonet站没有降水而从DCS砧区的降水反演所致。一种改进的SCaMPR检索算法,同时利用云的光学深度和IR温度,有可能进行重大改进,以减少DCS砧区域上SCaMPR检索的湿偏。

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