Comparison of the CHAMP radio occultation data with the Canadian advanced digital ionosonde in the Polar Regions

被引:11
|
作者
Sadighi, Samaneh [1 ]
Jayachandran, P. T. [1 ]
Jakowski, N. [2 ]
MacDougall, J. W. [3 ]
机构
[1] Univ New Brunswick, Dept Phys, Fredericton, NB E3B 5A3, Canada
[2] DLR, German Aerosp Ctr, Inst Commun & Nav, Neustrelitz, Germany
[3] Univ Western Ontario, Dept Elect Engn, London, ON N6A 5B9, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Polar ionosphere; Ionospheric Radio Occultation; Electron density profiles; LEO satellites; GLOBAL POSITIONING SYSTEM;
D O I
10.1016/j.asr.2009.07.016
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
In this paper we present the results of the comparison of the retrieved electron density profiles of the Ionospheric Radio Occultation (IRO) experiment on board CHAMP (CHAllenging Minisatellite Payload), with the ground ionosonde profiles for the Polar Regions. IRO retrieved electron density profiles from CHAMP are compared with Canadian Advanced Digital Ionosonde (CADI) measurements at two vertical sounding stations well within the Polar Cap, Eureka (geog. 80 degrees 13' N; 86 degrees 11' W) and Resolute Bay (geog. 74 degrees 41' N; 94 degrees 54' W). We compared the ionospheric parameters such as the peak electron density of the F-layer (NmF(2)) and the peak height of the F-layer (h(m)F(2)) for a 3-year period, 2004-2006. CHAMP derived NmF(2) shows reasonable agreement with the ionosonde retrieved NmF(2) for both the stations (0.76 and 0.71 correlation coefficient, for Eureka and Resolute Bay, respectively) whereas the h(m)F(2) agreement is not that acceptable (0.25 and 0.37 correlation coefficient, respectively). The h(m)F(2) from vertical sounding showed less spread than the CHAMP h(m)F(2) (C) 2009 COSPAR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:1304 / 1308
页数:5
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