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An improved GNSS tropospheric tomography method with the GPT2w model

机译:具有GPT2W模型的改进的GNSS对流层断层扫描方法

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The GNSS tropospheric tomography technique has been proven to be a powerful tool for three-dimensional water vapor reconstruction. In most previous studies, the signals leaving the side face of the tomography area are ignored as having invalid information, which wastes valuable observations and decreases signal coverage of the research area. To include the contribution of such signals to the final tomographic result, an improved tropospheric tomography approach, which makes the most use of GNSS observations by combining the data derived from the empirical Global Pressure and Temperature 2 wet model, is proposed. Compared to the conventional method, the proposed method can adaptively use the signals penetrating from the model's side face to the tomographic model, which increases the number of voxels crossed by rays and improves the stability of the tomography model. Numerical results in Hong Kong over the period of day of year 124-150, 2013 show that the internal accuracy of the tomographic model based on the proposed method increases by 9.8% when compared to the conventional method. The RMS errors of the integrated water vapor derived from the proposed method are 4.1 and 4.6 mm, respectively, while the values derived from the conventional method are 5.0 and 5.4 mm, respectively, when compared to the radiosonde and European Centre for Medium-Range Weather Forecasts (ECMWF) products. In addition, compared to the conventional method, the accuracy of the water vapor density profile derived from the tomographic result of the proposed method has been enhanced by 25% and 12.5% when the radiosonde and ECMWF data are considered as the reference, respectively. Such results indicate a good performance of the proposed method for GNSS troposphere tomography.
机译:GNSS对流层断层摄影技术已被证明是三维水蒸气重建的强大工具。在最先前的研究中,忽略留下断层摄影区域的侧面的信号被忽略为具有无效信息,这浪费了有价值的观察和降低了研究区域的信号覆盖范围。为了将这些信号的贡献与最终的断层结果包括,提出了一种改进的对流层断层扫描方法,这是通过组合源自经验全球压力和温度2湿模型的数据来实现GNSS观测的。与传统方法相比,所提出的方法可以自适应地使用从模型的侧面穿透到断层模型的信号,这增加了射线交叉的体素数并提高了断层摄影模型的稳定性。与常规方法相比,在124-150年的一年内,在香港的数值结果显示,基于所提出的方法的断层模型的内部精度增加了9.8%。衍生自提出的方法的集成水蒸气的RMS误差分别为4.1和4.6mm,而常规方法的值分别与无线电电池和欧洲中等范围的天气中心相比,分别为5.0和5.4mm预测(ECMWF)产品。另外,与常规方法相比,当辐射电池和ECMWF数据被视为参考时,从所提出的方法的断层突起的精度得到增强了25%和12.5%。这种结果表明了GNSS对流层断层扫描的提出方法的良好性能。

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