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Assessment of Empirical Troposphere Model GPT3 Based on NGL’s Global Troposphere Products

机译:基于NGL全球对流层产品的经验对流层模型GPT3评估

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摘要

Tropospheric delay is one of the major error sources in GNSS (Global Navigation Satellite Systems) positioning. Over the years, many approaches have been devised which aim at accurately modeling tropospheric delays, so-called troposphere models. Using the troposphere data of over 16,000 global stations in the last 10 years, as calculated by the Nevada Geodetic Laboratory (NGL), this paper evaluates the performance of the empirical troposphere model GPT3, which is the latest version of the GPT (Global Pressure and Temperature) series model. Owing to the large station number, long time-span and diverse station distribution, the spatiotemporal properties of the empirical model were analyzed using the average deviation (BIAS) and root mean square (RMS) error as indicators. The experimental results demonstrate that: (1) the troposphere products of NGL have the same accuracy as the IGS (International GNSS Service) products and can be used as a reference for evaluating general troposphere models. (2) The global average BIAS of the ZTD (zenith total delay) estimated by GPT3 is −0.99 cm and the global average RMS is 4.41 cm. The accuracy of the model is strongly correlated with latitude and ellipsoidal height, showing obviously seasonal variations. (3) The global average RMS of the north gradient and east gradient estimated by GPT3 is 0.77 mm and 0.73 mm, respectively, which are strongly correlated with each other, with values increasing from the equator to lower latitudes and decreasing from lower to higher latitudes.
机译:对流层延迟是GNSS(全球导航卫星系统)定位的主要误差源之一。多年来,已经设计了许多方法,旨在准确地建模对流层延误,所谓的对流层模型。在过去的10年里,使用内华达地理仪实验室(NGL)计算的对流层数据超过10年的全球车站,这篇论文评估了经验对流层模型GPT3的性能,这是GPT的最新版本(全球压力温度)系列模型。由于大型站号,长时间跨越多样化的站分布,使用平均偏差(偏置)和根均线(RMS)误差作为指标,分析了经验模型的时空性质。实验结果表明:(1)NGL的对流层产品具有与IGS(国际GNSS服务)产品相同的准确性,可用作评估一般对流层模型的参考。 (2)GPT3估计的ZTD(Zenith总延迟)的全局平均偏差为-0.99cm,全局平均rms为4.41厘米。模型的准确性与纬度和椭圆形高度强烈相关,显示出明显的季节变化。 (3)由GPT3估计的北梯度和东梯度的全局平均均方根分别为0.77毫米和0.73毫米,其彼此强烈相关,从赤道增加到降低纬度和从下部降低到更高纬度的值。

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