Comparing Discrete and Empirical Troposphere Delay Models: A Global IGS‐Based Evaluation

全球导航卫星系统应用 天顶 大地基准 对流层 气象学 均方误差 环境科学 卫星 经验模型 仰角(弹道) 均方根 卫星系统 大地测量学 计算机科学 遥感 全球定位系统 数学 地质学 统计 地理 模拟 电信 物理 量子力学 天文 几何学
作者
Yifan Yao,Fei Yang,Jian Li,Lei Wang,Jing Zheng,Ruiqin Hao,Tairan Xu
出处
期刊:Radio Science [Wiley]
卷期号:59 (6)
标识
DOI:10.1029/2024rs007950
摘要

Abstract Zenith tropospheric delay (ZTD) is an important atmospheric parameter in radio‐space‐geodetic techniques such as Global Navigation Satellite System (GNSS), which is pivotal for GNSS positioning, navigation and meteorology. The Vienna Mapping Function (VMF) data server is a widely utilized source for implementing ZTD, offering two types of models, that is, the empirical one and the discrete one with Grid‐wise and Site‐wise models. Therefore, to evaluate the accuracy of these models becomes the focus of this article. Specifically, this study investigates their performances in terms of calculation of ZTD, using the hourly values derived from the International GNSS Service data as references. The results show that the root mean square err (RMSE) of the Site‐wise, Grid‐wise and global pressure and temperature 3 model are 11.71/13.03/38.56 mm, respectively, indicating the discrete model performs generally better than the empirical model, and the Site‐wise model is the better of the two discrete models. From the perspective of spatial resolution, the performance of these three models in ZTD calculation shows obvious influences of latitude changes and elevation differences. From the temporal analysis, the accuracy of the discrete model shows differences over different UTC epochs, while the empirical model can only express the seasonal ZTD characteristics with the average RMSE at different epochs being similar, the specifically values are 39.67, 39.26, 39.38 and 39.18 mm at UTC 0:00, 6:00, 12:00 and 18:00, respectively. The histogram and boxplot well indicate the accuracy differences of the three models in different seasons. Additionally, the time series of three models at different latitudes were also explored in this research. These explorations are conducive to the selection of appropriate models for calculating ZTD based on specific requirements.
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