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Assessment and quantification of meteorological data for implementation of weather radar in mountainous regions

机译:在山区实施气象雷达的气象数据评估和量化

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The scope of this paper is to improve observation and detection of hydro-meteorological hazard over the Grenoble region which is characterised by significant changes of terrain in altitude and geomorphology. The city of Grenoble is located at a height between 200 up to 500 m, installing the weather radar in this range of elevation leads to better quality measurements, but visibility and as well coverage capability will be reduced at the other sites of the affected region. Two locations are shortlisted for the implementation of the future weather radar in Grenoble; (i) Moucherotte (1920 m a.s.l.) and (ii) Saint Eynard (1365 m a.s.l.). Several simulation and data analysis are performed to get the clear picture about precipitation variability by considering meteorological data from individual ground stations and radio sounding data as well. Compared to previous work, in this study is considered climatology of the vertical structure of the rainfall. In this context, several statistical computations are done regarding 0 degrees C isotherm altitude. Concerning rainfall error estimation, ground clutter and screening effect, statistical calculations by using VISHYDRO code, are performed by for different quintiles for several elevation angles in both shortlisted sites. The results obtained from calculations carried out on two locations are almost similar. Also, significant under and over-estimation of rainfall error due to screening and ground clutter effect are detected. To achieve more accurate results, other sites need to be tested for further simulation. On the other hand since ground clutter, and screening effect at the Moucherotte is not too high compare with Saint Eynard, this site may be considered for implementing the future weather radar for observation of the meteorological processes over the Grenoble region.
机译:本文的范围是改进对格勒诺布尔地区水文气象灾害的观察和检测,该地区的特征是海拔高度和地貌的显着变化。格勒诺布尔市位于200至500 m之间的高度,将气象雷达安装在此海拔范围内可以提高质量测量的质量,但是在受影响区域的其他站点,可见度和覆盖能力将降低。入围了两个地点,以实施格勒诺布尔未来的天气雷达; (i)Moucherotte(1920 m.s.l.)和(ii)Saint Eynard(1365 m.s.l.)。通过考虑来自各个地面站的气象数据和无线电测深数据,进行了几次模拟和数据分析,以清晰了解降水变化。与以前的工作相比,本研究认为降雨的垂直结构是气候学。在这种情况下,完成了关于0摄氏度等温线高度的一些统计计算。关于降雨误差估算,地物杂波和遮挡效果,在入围地点的两个仰角上,由不同五分位数的几个仰角使用VISHYDRO代码进行统计计算。从在两个位置进行的计算获得的结果几乎相似。此外,还发现了由于筛选和地面杂波效应而导致的降雨误差的明显低估和高估。为了获得更准确的结果,需要测试其他站点以进行进一步的仿真。另一方面,由于地面杂乱以及在Moucherotte的屏蔽效果与Saint Eynard相比并不算高,因此可以考虑将该站点用于实施未来的天气雷达以观测格勒诺布尔地区的气象过程。

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