地球不同地理区域天顶湿延迟和天顶对流层总延迟的分析与估算

Jabir Shabbir Malik
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引用次数: 0

摘要

对GPS/GLONASS联合精确点定位(PPP)方法估算的天顶对流层延迟(ZTD)和天顶湿延迟(ZWD)进行了综合分析。为此,实验利用低、赤道和高纬度地区国际GNSS服务站(IGS)冬夏两季收集的数据集进行。结果表明:高纬度站点冬季和夏季的ZWD分别在0.05 ~ 0.08 m和0.14 ~ 0.17 m之间;而低洼地区气象站冬季和夏季的ZWD值分别在0.12 ~ 0.15 m和0.06 ~ 0.09 m之间。此外,中部地区在两个不同季节的ZWD估计相对相似。此外,ZTD估计值与相应的IGS对流层延迟地面值进行比较。结果表明,赤道ZTD的估计在两个季节中具有非常相似的趋势。而在极高纬度和极低纬度,ZTD变化较大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis and Estimation of Zenith Wet Delay and Zenith Tropospheric Total Delay at Earth’s different Geographical Areas
A comprehensive analysis is performed for the estimation of zenith troposphere delay (ZTD) and zenith wet delay (ZWD) from combined GPS/GLONASS precise point positioning (PPP) method. For this purpose, experiment is conducted from the dataset collected during winter and summer seasons from International GNSS service (IGS) stations at low, equator and high latitude areas. Results demonstrate that ZWD for the stations at higher latitude during winter and summer season is within 0.05 – 0.08 m and 0.14 – 0.17 m, respectively. While, estimates of ZWD for the stations at low region is within 0.12 – 0.15 m and 0.06 – 0.09 m for the winter and summer seasons, respectively. Furthermore, central regions have relative similar ZWD estimates during two different seasons. Additionally, ZTD estimates compare with respect to the corresponding IGS tropospheric delay ground values. Results demonstrate that estimates of ZTD at the equator has quiet similar trend during two seasons. While, at very high and very low latitude, large variation of ZTD is obtained.
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