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Application of Cumulative Distribution Functions to Compositing Precipitable Water with Low Earth Orbit Satellite Data

机译:累积分布函数在低地球轨道卫星数据合成可降水量中的应用

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Precipitable water (PW) is a leading indicator of severe weather, such as heavy rainfall. The National Meteorological Satellite Center receives observation data directly from Low Earth Orbit (LEO) satellites, including NOAA-18, 19, MetOp-A, B, and Suomi-NPP, and generates level 2 products in near real time for the East Asia region. In this study, PW data were retrieved from the abovementioned sources and composited to determine meteorologically significant PW fields from all available data sources considering the boundary layer (BL), middle layer (ML), high layer (HL), and total column. Cumulative distribution function (CDF) matching was performed for PW retrieved from the five satellites within specific time windows in order to integrate them and minimize their differences. The PW composite data were matched to reference PW CDF data from the Unified Model (UM) Regional Data Assimilation Prediction System (RDAPS) analysis data, which are updated according to selected time windows. PW data were composited for 03:00-09:00, 09:00-15:00, 15:00-21:00, and 21:00-03:00 UTC time windows. PW data composited during the summer and winter seasons in 2015, 2016, and 2017 were then validated. The results show improvements in composite Total Precipitable Water and BL PW from Suomi-NPP of approximately 15% and 40% (RMSE), respectively.
机译:可降水量(PW)是恶劣天气(例如大雨)的主要指示。国家气象卫星中心直接从包括NOAA-18、19,MetOp-A,B和Suomi-NPP在内的低地球轨道(LEO)卫星接收观测数据,并为东亚地区近乎实时地生成2级产品。在这项研究中,从上述来源中获取了PW数据,并进行了综合分析,以确定所有可用的数据源在气象方面的重要PW字段,其中包括边界层(BL),中间层(ML),高层(HL)和总列。为了在特定时间窗口内从五颗卫星中检索到的PW进行累积分布函数(CDF)匹配,以整合它们并最大程度地减少它们之间的差异。将PW复合数据与来自统一模型(UM)区域数据同化预测系统(RDAPS)分析数据的参考PW CDF数据进行匹配,这些数据根据选定的时间窗口进行更新。 PW数据在UTC时间窗口03:00-09:00、09:00-15:00、15:00-21:00和21:00-03:00进行了合成。然后验证了2015年,2016年和2017年夏季和冬季合成的PW数据。结果表明,Suomi-NPP的复合总可沉淀水和BL PW分别提高了约15%和40%(RMSE)。

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