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Operational Implementation of the ATOVS Processing Procedure in KMA and Its Validation

机译:KMA中ATOVS处理程序的操作实现及其验证

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The Korea Meteorological Administration (KMA) has processed the data from the advanced TOVS(ATOVS) onboard NOAA-16 satellite since May 2001. The operational production utilizes the AAPP(ATOVS and AVHRR Processing Package) of EUMETSAT and IAPP (International ATOVS ProcessingPackage) of the University of Wisconsin. For the initial guess profiles, the predicted fields (usually 6 to 12hour forecasted fields) from the global aviation model of NOAA/NCEP are used. The average number ofprofiles retrieved from the ATOVS data is about 1,300 for each morning and afternoon orbit at about 18 and06 UTC, respectively. The retrieved temperature and dew point temperatures are provided to forecastersin real time and used for initialization of prediction models. With the advanced microwave sensor (AMSU;Advanced Microwave Sounding Unit), accuracy of the ATOVS products is expected to be better than thatof the TOVS products, especially in cloudy conditions. Indeed, the preliminary results from a validationstudy with the collocated radiosonde data during a 8-month period, from May to December 2001, for theEast Asia region show an improved accuracy of the ATOVS products for cloudy skies versus the TOVS,especially for higher altitudes. The RMS (Root Mean Square) difference between the ATOVS productsand radiosonde data is about 1.3℃ for both clear and cloudy conditions, except for near the ground and athigher altitudes, at around 200 hPa. There is no significant temporal variation of the error statistics at allpressure levels. In case of the water vapor mixing ratio, the largest difference is shown at lower altitudes,while the accuracy is much better for the clear sky cases than the cloudy sky cases. The bias and RMSEat lower altitudes is about 0.557 g kg-1 and 2.5 g kg-1 and decrease significantly with increasing altitude.
机译:韩国气象局(KMA)自2001年5月起已经处理了NOAA-16卫星上先进TOVS(ATOVS)的数据。实际生产利用EUMETSAT的AAPP(ATOVS和AVHRR处理包)和IAPP(国际ATOVS处理包)进行了处理。威斯康星大学。对于初始猜测配置文件,使用来自NOAA / NCEP的全球航空模型的预测字段(通常为6到12小时的预测字段)。从ATOVS数据中检索到的轮廓的平均数量分别为每个上午和下午大约UTC时间18和06的轨道。检索到的温度和露点温度被实时提供给预报员,并用于预报模型的初始化。借助先进的微波传感器(AMSU;先进的微波探测单元),ATOVS产品的精度有望比TOVS产品的精度更高,尤其是在阴天条件下。的确,从2001年5月至2001年12月的8个月期间,对东亚地区的无线电探空仪数据进行的验证研究得出的初步结果表明,与TOVS相比,多云天空的ATOVS产品的精度有所提高,尤其是在较高海拔的地区。在晴朗和多云的条件下,ATOVS产品与探空仪数据之间的RMS(均方根)差约为1.3℃,除了在地面附近和在200 hPa处较高的高度外。在所有压力水平下,误差统计量都没有明显的时间变化。在水蒸气混合比的情况下,在较低的高度处显示出最大的差异,而在晴朗天空情况下的准确度要比多云天空情况好得多。在较低高度处的偏差和RMSE分别约为0.557 g kg-1和2.5 g kg-1,并且随着海拔的升高而显着降低。

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