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4D wet refractivity estimation in the atmosphere using GNSS tomography initialized by radiosonde and AIRS measurements: results from a 1-week intensive campaign

机译:4D湿法折射率估计在大气中使用无线电探空仪和空气测量初始化的GNSS断层扫描:由1周密集型运动的结果

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A Global Navigational Satellite System (GNSS) tomography system is implemented in the Lisbon area, Portugal, to estimate the water vapor dynamics at a local scale. A field experiment was carried out, in which a series of temporary GNSS stations were installed, increasing the network from 9 permanent stations to a total of 17 GNSS stations. A radiosonde campaign was also performed with high sampling launches, at 4-h intervals, for 1 week. A time series of hourly 3D wet refractivity solutions were obtained during the radiosonde campaign. Radiosonde and Atmospheric Infrared Sounder (AIRS) measurements were used to compute wet refractivity profiles to initialize and update the tomography solutions. The dependence of the GNSS tomography solution on the initial conditions obtained from both radiosonde and AIRS measurements, and their updating frequencies are studied. It is found that the GNSS tomography continuous measurement of the atmospheric refractivity provides solutions with an RMS mean of about 2 g/m(3).
机译:全球航行卫星系统(GNSS)断层扫描系统在里斯本地区,葡萄牙,以局部规模估计水蒸气动力学。进行了现场实验,其中安装了一系列临时GNSS站,从9个永久站增加了网络,总共17个GNSS站。 RADIOSonde广告系列也进行了高采样推出,以4小时间隔进行1周。在无线电探空仪运动期间获得了一时间时间3D湿折射率解决方案。无线电钻石和大气红外发声器(Airs)测量用于计算湿折射率配置文件以初始化和更新断层扫描解决方案。 GNSS断层扫描解决方案对从无线电钻孔和空气测量获得的初始条件的依赖性以及其更新的频率。发现GNSS断层扫描的连续测量大气折射率提供率为约2g / m(3)的RMS平均值。

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