Evaluation of the ZWD/ZTD Values Derived from MERRA-2 Global Reanalysis Products Using GNSS Observations and Radiosonde Data

被引:15
|
作者
Huang, Liangke [1 ,2 ]
Guo, Lijie [1 ,2 ]
Liu, Lilong [1 ,2 ]
Chen, Hua [3 ]
Chen, Jun [3 ]
Xie, Shaofeng [1 ,2 ]
机构
[1] Guilin Univ Technol, Coll Geomat & Geoinformat, Guilin 541004, Peoples R China
[2] Guilin Univ Technol, Guangxi Key Lab Spatial Informat & Geomat, Guilin 541004, Peoples R China
[3] Wuhan Univ, Sch Geodesy & Geomat, Wuhan 430079, Peoples R China
关键词
zenith tropospheric delay; zenith wet delay; GNSS; MERRA-2; SLANT DELAYS; WATER-VAPOR; MODEL; INTERFEROMETRY; TEMPERATURE;
D O I
10.3390/s20226440
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Tropospheric delay is one of the main errors affecting high-precision positioning and navigation and is a key parameter of water vapor detection in the Global Navigation Satellite System (GNSS). The second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) is the latest generation of reanalysis data collected by the National Aeronautics and Space Administration (NASA), which can be used to calculate tropospheric delay products with high spatial and temporal resolution. However, there is no report analyzing the accuracy of the zenith tropospheric delay (ZTD) and zenith wet delay (ZWD) calculated from MERRA-2 data. This paper evaluates the performance of the ZTD and ZWD values derived from global MERRA-2 data using global radiosonde data and International GNSS Service (IGS) precise ZTD products. The results are as follows: (1) Taking the precision ZTD products of 316 IGS stations from around the world from 2015 to 2017 as the reference, the average root mean square (RMS) of the ZTD values calculated from the MERRA-2 data is better than 1.35 cm, and the accuracy difference between different years is small. The bias and RMS of the ZTD values show certain seasonal variations, with a higher accuracy in winter and a lower accuracy in summer, and the RMS decreases from the equator to the poles. However, those of the ZTD values do not show obvious variations according to elevation. (2) Relative to the radiosonde data, the RMS of the ZWD and ZTD values calculated from the MERRA-2 data are better than 1.37 cm and 1.45 cm, respectively. Furthermore, the bias and RMS of the ZWD and ZTD values also show some temporal and spatial characteristics, which are similar to the test results of the IGS stations. It is suggested that MERRA-2 data can be used for global tropospheric vertical profile model construction because of their high accuracy and good stability in the global calculation of the ZWD and ZTD.
引用
收藏
页码:1 / 20
页数:19
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