Quiet and perturbed ionospheric representation according to the electron content from GPS signals

被引:32
作者
Brunini, C
Van Zele, MA
Meza, A
Gende, M
机构
[1] Natl Univ La Plata, Fac Ciencias Astron & Geofis, RA-1900 La Plata, Argentina
[2] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol Geofis, RA-1428 Buenos Aires, DF, Argentina
[3] Consejo Nacl Invest Cient & Tecn, Fac Ciencias Astron & Geofis, RA-1900 La Plata, Argentina
关键词
GPS; Global Positioning System; ionosphere; TEC;
D O I
10.1029/2002JA009346
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
[1] Signals from Global Positioning System (GPS) satellites received at the surface of the Earth have passed through the terrestrial atmosphere and are therefore affected by refraction in the ionosphere. A large number of permanent dual frequencies GPS tracking stations have been built up in the last years and their data have proved to be suitable to study the ionosphere. The main goal of this paper is to assess the capability of these observations to continuously and routinely monitor the ionosphere at a global scale. The interest was focused on retrieving the coefficients of a spherical harmonics expansion that describe the global distribution of the vertical total electron content (VTEC) from the GPS signal. To test our results, we compare them with other GPS-derived results, with VTEC values computed with the International Reference Ionosphere (IRI-95) model, and with direct VTEC determinations provided by Topex-Poseidon satellite. A large set of global VTEC maps with a time resolution of 2 hours was used to describe the evolution of this ionospheric variable at quiet geomagnetic periods during the year 1997. The outstanding features of the VTEC during the 15 May 1997 geomagnetic storm have also been studied. The results show that our method is able to identify large-scale features and seasonal variations of the VTEC in quiet conditions, as well as its variations during a large geomagnetic storm.
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页数:11
相关论文
共 39 条
[1]   GPS phase fluctuations in the equatorial region during sunspot minimum [J].
Aarons, J ;
Mendillo, M ;
Yantosca, R .
RADIO SCIENCE, 1997, 32 (04) :1535-1550
[2]   Ionospheric effects of the solar flares of September 23, 1998 and July 29, 1999 as deduced from global GPS network data [J].
Afraimovich, EL ;
Altyntsev, AT ;
Kosogorov, EA ;
Larina, NS ;
Leonovich, LA .
JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS, 2001, 63 (17) :1841-1849
[3]   The international GPS service (IGS): An interdisciplinary service in support of earth sciences [J].
Beutler, G ;
Rothacher, M ;
Schaer, S ;
Springer, TA ;
Kouba, J ;
Neilan, RE .
SATELLITE DYNAMICS, ORBIT ANALYSIS AND COMBINATION OF SPACE TECHNIQUES, 1999, 23 (04) :631-653
[4]  
chaer S, 1996, P IGS AN CTR WORKSH
[5]   PASSIVE DETECTION OF SPORADIC-E USING GPS PHASE MEASUREMENTS [J].
COCO, DS ;
GAUSSIRAN, TL ;
COKER, C .
RADIO SCIENCE, 1995, 30 (06) :1869-1874
[6]   VARIABILITY OF GPS SATELLITE DIFFERENTIAL GROUP DELAY BIASES [J].
COCO, DS ;
COKER, C ;
DAHLKE, SR ;
CLYNCH, JR .
IEEE TRANSACTIONS ON AEROSPACE AND ELECTRONIC SYSTEMS, 1991, 27 (06) :931-938
[7]   More total electron content climatology from TOPEX/Poseidon measurements [J].
Codrescu, MV ;
Beierle, KL ;
Fuller-Rowell, TJ ;
Palo, SE ;
Zhang, XL .
RADIO SCIENCE, 2001, 36 (02) :325-333
[8]   DETECTION OF AURORAL ACTIVITY USING GPS SATELLITES [J].
COKER, C ;
HUNSUCKER, R ;
LOTT, G .
GEOPHYSICAL RESEARCH LETTERS, 1995, 22 (23) :3259-3262
[9]  
Coster A. J., 1992, Navigation. Journal of the Institute of Navigation, V39, P191
[10]   Studying the ionosphere with the Global Positioning System [J].
Davies, K ;
Hartmann, GK .
RADIO SCIENCE, 1997, 32 (04) :1695-1703