Combination of Ground- and Space-Based Data to Establish a Global Ionospheric Grid Model

被引:28
作者
Chen, Peng [1 ,2 ]
Yao, Wanqiang [1 ]
Zhu, Xuejun [1 ]
机构
[1] Xian Univ Sci & Technol, Coll Geomat, Xian 710054, Peoples R China
[2] Chinese Acad Sci, State Key Lab Geodesy & Earths Dynam, Wuhan 430077, Peoples R China
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2015年 / 53卷 / 02期
关键词
Constellation Observation System for Meteorology; Ionosphere; and Climate (COSMIC); global ionospheric grid model; Global Navigation Satellite System; satellite altimetry; total electron content (TEC); BIASES; MAPS; VTEC; TEC;
D O I
10.1109/TGRS.2014.2333522
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The global ionospheric maps (GIMs) that are established using ground-based Global Navigation Satellite System (GNSS) data are important means to study the variations of the ionosphere. However, the uneven distribution of ground GNSS stations, which particularly exist at large gaps in the vast ocean areas, results to low accuracy and reliability of GIMs in the marine region and other areas that lack GNSS sites. The ocean altimetry satellite's orbit can cover most of the marine areas, and dual-frequency signals can obtained vertical total electronic content (VTEC) at the nadir track. Low-Earth-orbit occultation observations also obtain much global ionospheric uniform distribution information. The combination of the space-based ionospheric data and ground-based GNSS observation data can effectively improve the accuracy and reliability of GIM in marine areas. However, the systematic bias that exists between ionospheric data obtained by different systems must also be considered during the data combination. This paper used both ground-based GNSS data and space-based data to establish a global ionospheric model, whereas the systematic bias between the space-based ionospheric data and ground-based GNSS data can be seen as parameters to estimate. The results show that, by adding space-based data, the accuracy of GIM on the ocean areas has been improved to make up the deficiencies of the existing GIMs.
引用
收藏
页码:1073 / 1081
页数:9
相关论文
共 29 条
[1]  
Abramowitz M, 1965, APPL MATH SER, V55, P1046
[2]   Global Ionosphere Maps of VTEC from GNSS, satellite altimetry, and formosat-3/COSMIC data [J].
Alizadeh, M. M. ;
Schuh, H. ;
Todorova, S. ;
Schmidt, M. .
JOURNAL OF GEODESY, 2011, 85 (12) :975-987
[3]   International Reference Ionosphere 2007: Improvements and new parameters [J].
Bilitza, D. ;
Reinisch, B. W. .
ADVANCES IN SPACE RESEARCH, 2008, 42 (04) :599-609
[4]   Temporal and spatial variability of the bias between TOPEX- and GPS-derived total electron content [J].
Brunini, C ;
Meza, A ;
Bosch, W .
JOURNAL OF GEODESY, 2005, 79 (4-5) :175-188
[5]   GPS slant total electron content accuracy using the single layer model under different geomagnetic regions and ionospheric conditions [J].
Brunini, C. ;
Azpilicueta, F. .
JOURNAL OF GEODESY, 2010, 84 (05) :293-304
[6]  
Cui X., 2005, Generalized Surveying Adjustment
[7]   Systematic differences between VTEC obtained by different space-geodetic techniques during CONT08 [J].
Dettmering, Denise ;
Heinkelmann, Robert ;
Schmidt, Michael .
JOURNAL OF GEODESY, 2011, 85 (07) :443-451
[8]   Radio occultation electron density profiles from the FORMOSAT-3/COSMIC satellites over the Brazilian region: A comparison with Digisonde data [J].
Ely, C. V. ;
Batista, I. S. ;
Abdu, M. A. .
ADVANCES IN SPACE RESEARCH, 2012, 49 (11) :1553-1562
[9]   A SIMPLE, CONVENIENT FORMALISM FOR ELECTRON-DENSITY PROFILES [J].
FOX, MW .
RADIO SCIENCE, 1994, 29 (06) :1473-1491
[10]  
Gao YZ, 2002, RRD APP CHE, V1, P1