Comparison of ZTD derived from CARRA, ERA5 and ERA5-Land over the Greenland based on GNSS

被引:8
作者
Jiang, Chunhua [1 ,2 ,3 ]
Gao, Xiang [1 ]
Wang, Shuaimin [4 ]
Zhu, Huizhong [1 ]
Xu, Aigong [1 ]
An, Qianfang [1 ]
Zhu, Meizhen [1 ]
Liu, Guangsheng [1 ]
机构
[1] Liaoning Tech Univ, Sch Geomatics, Fuxin 123000, Peoples R China
[2] State Key Lab Geoinformat Engn, Xian 710054, Peoples R China
[3] Chinese Acad Sci, Innovat Acad Precis Measurement Sci & Technol, State Key Lab Geodesy & EarthsDynam, Wuhan 430077, Peoples R China
[4] Hebei Univ Engn, Coll Min & Geomatics, Handan 056038, Peoples R China
基金
中国国家自然科学基金;
关键词
Zenith tropospheric delay; Meteorological parameters; CARRA; ERA5; ERA5-Land; GNSS; TROPOSPHERIC DELAY; WATER-VAPOR; REANALYSIS; TEMPERATURE; PROGRAM; PRODUCT; SYSTEM; CHINA; MODEL;
D O I
10.1016/j.asr.2023.09.002
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
High-accuracy reanalysis products are beneficial to the retrieval and modeling of zenith tropospheric delay (ZTD) in GNSS positioning and the study of GNSS Meteorology. The performance of meteorological parameters and ZTD derived from Copernicus Arctic Regional ReAnalysis (CARRA), ERA5 and ERA5-Land over the Greenland covering the year of 2020 are comprehensively compared and analyzed in this study. Firstly, the accuracies of the atmospheric pressure, temperature and water vapor pressure retrieved from three reanalysis data are compared with the observations obtained from 6 radiosondes and 30 automatic weather stations. The results show that the accuracy of temperature data from ERA5 pressure-level in the height range of 23-30 km is higher than that of CARRA pressurelevel. The atmospheric pressure, temperature and water vapor pressure from CARRA single-level are superior to those of ERA5 singlelevel and ERA5-Land. Secondly, the ZTD derived from CARRA, ERA5 and ERA5-Land are compared with GNSS final ZTD data from 37 UNAVCO stations. The Root Mean Square error (RMS) values of ERA5 pressure-level ZTD is 6.7 mm, showing slightly better accuracy than CARRA pressure-level ZTD of 10.7 mm. The RMS values of ZTD derived from CARRA single-level, ERA5 single-level and ERA5-Land based on the Saastamoinen model are 11.9 mm, 13.4 mm and 22.7 mm, respectively, which indicates that CARRA single-level ZTD shows best consistency with GNSS ZTD among three single-level reanalysis data. Moreover, the reanalysis-derived ZTD show obviously poorer accuracy in warm-season than that in cold-season.(c) 2023 COSPAR. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:4692 / 4706
页数:15
相关论文
共 50 条
[1]   ESTIMATION OF TROPOSPHERIC DELAY FOR MICROWAVES FROM SURFACE WEATHER DATA [J].
ASKNE, J ;
NORDIUS, H .
RADIO SCIENCE, 1987, 22 (03) :379-386
[2]   EASILY IMPLEMENTED ALGORITHM FOR TROPOSPHERIC RANGE CORRECTION [J].
BLACK, HD .
JOURNAL OF GEOPHYSICAL RESEARCH, 1978, 83 (NB4) :1825-1828
[3]   Accuracy of NCEP/NCAR reanalyses and ECMWF analyses in the lower stratosphere over Antarctica in 2005 [J].
Boccara, G. ;
Hertzog, A. ;
Basdevant, C. ;
Vial, F. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D20)
[4]  
Boehm J, 2007, J GEODESY, V81, P679, DOI 10.1007/s00190-007-0135-3
[5]   Development of an improved empirical model for slant delays in the troposphere (GPT2w) [J].
Boehm, Johannes ;
Moeller, Gregor ;
Schindelegger, Michael ;
Pain, Gregory ;
Weber, Robert .
GPS SOLUTIONS, 2015, 19 (03) :433-441
[6]   THE ARCTIC SYSTEM REANALYSIS, VERSION 2 [J].
Bromwich, D. H. ;
Wilson, A. B. ;
Bai, L. ;
Liu, Z. ;
Barlage, M. ;
Shih, C. -F. ;
Maldonado, S. ;
Hines, K. M. ;
Wang, S. -H. ;
Woollen, J. ;
Kuo, B. ;
Lin, H. -C. ;
Wee, T. -K. ;
Serreze, M. C. ;
Walsh, J. E. .
BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2018, 99 (04) :805-828
[7]   Assessment of Temperature and Specific Humidity Inversions and Their Relationships in Three Global Reanalysis Products over the Arctic Ocean [J].
Chang, Liang ;
Wen, Shiqiang ;
Gao, Guoping ;
Han, Zhen ;
Feng, Guiping ;
Zhang, Yang .
JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY, 2021, 60 (04) :493-511
[8]   Assessment of ZTD derived from ECMWF/NCEP data with GPS ZTD over China [J].
Chen, Qinming ;
Song, Shuli ;
Heise, Stefan ;
Liou, Yuei-An ;
Zhu, Wenyao ;
Zhao, Jingyang .
GPS SOLUTIONS, 2011, 15 (04) :415-425
[9]  
Documentation I F S, 2007, Cy31r1, Operational implementation 12 September 2006. Part IV: Physical processes
[10]   Wind-Driven Freshwater Export at Cape Farewell [J].
Duyck, E. ;
Gelderloos, R. ;
de Jong, M. F. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2022, 127 (05)