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An improved weighted mean temperature (T-m) model based on GPT2w with T-m lapse rate

机译:基于GPT2W具有T-M流失率的改进的加权平均温度(T-M)模型

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Global pressure and temperature 2 wet (GPT2w) is an empirical model providing the mean values plus annual and semiannual amplitudes of weighted mean temperature (T-m), which makes it a widely used tool in converting zenith wet delay (ZWD) to precipitable water vapor (PWV) in GNSS meteorology. The model meets the needs of real-time T-m anywhere in the world without relying on any other meteorological observations compared with traditional T-m calculation methods. It outperforms the other empirical T-m models released in recent years. Due to the lack of the T-m vertical adjustment in the model, the accuracy of T-m estimated by the model is subject to certain constraints, especially at sites which have large altitude differences compared with the GPT2w grid points. We explored the T-m lapse rate for the vertical adjustment using 10 years of 37 monthly mean pressure level data from the European Center for Medium-Range Weather Forecasts (ECMWF) and extended the GPT2w model to a new one called the GPT2wh model. Three schemes with different height ranges were established to fit the T-m lapse rate, and the most appropriate scheme was selected by adopting the goodness of fit measures, including the coefficient of determination (R-squared) and the root mean square error (RMSE). In addition to the mean value, annual and semiannual amplitudes for T-m lapse rate on a regular 1 degrees grid were determined and stored in the GPT2wh model. The performance of the new model was assessed against the GPT2w model using different data sources in 2011, i.e., the ECMWF data and globally distributed radiosonde data. The numerical results show that the GPT2wh model outperforms the GPT2w model with an improved RMSE of 7.36/5.00/2.45/1.37/0.51/0.03 K at different height levels in the ECMWF comparison. In comparison with the radiosonde data, the mean RMSE of the GPT2wh model improves by 0.33 K from 4.16 to 3.83 K, i.e., an approximately 8% improvement against the GPT2w model. The impact of T-m on GNSS-PWV was analyzed, showing that the GPT2wh model can effectively improve the accuracy of the converted PWV.
机译:全球压力和温度2湿(GPT2W)是提供平均值加上加权平均温度(TM)的平均值和半壮大(TM)的实证模型,这使其成为将Zenith湿延迟(ZWD)转换为可降水水蒸气( PWV)在GNSS气象中。该模型符合世界上任何地方的实时T-M的需求,而无需依赖与传统的T-M计算方法相比任何其他气象观测。它优于近年来发布的其他实证T-M型号。由于模型中缺乏T-M垂直调整,由该模型估计的T-M的精度受到某些约束,特别是与GPT2W网格点相比具有大海拔差异的站点。我们探讨了使用来自欧洲中距离预测中心(ECMWF)的10年37月平均压力水平数据的垂直调整的T-M流逝速率,并将GPT2W模型扩展到称为GPT2WH模型的新产品。建立了具有不同高度范围的三种方案以适应T-M渗透率,并且通过采用拟合措施的良好来选择最合适的方案,包括确定系数(R角)和根均方误差(RMSE)。除了常规1度网格上的T-M渗透率的平均值,确定并储存在GPT2WH模型中。使用不同的数据来源在2011年的不同数据来源评估新模型的性能,即ECMWF数据和全局分布式无线电探测数据。数值结果表明,GPT2WH模型优于GPT2W模型,在ECMWF比较中的不同高度水平的改善的RMSE为7.36 / 5.00 / 2.45 / 1.37 / 0.51 / 0.03K。与无线电探测器数据相比,GPT2WH模型的平均RMSE从4.16到3.83k,即对GPT2W模型的大约8%的改善提高了0.33k。分析了T-M对GNSS-PWV的影响,表明GPT2WH模型可以有效地提高转化的PWV的准确性。

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