Principles of Processing and Selection of Radio Occultation Observation Data for Investigating the Ionospheric F2-Layer

被引:5
作者
Chirik, N. V. [1 ]
Klimenko, M. V. [1 ,2 ]
Klimenko, V. V. [1 ]
Karpachev, A. T. [3 ]
Ratovskii, K. G. [4 ]
Koren'kova, N. A. [1 ]
机构
[1] Russian Acad Sci, Pushkov Inst Terr Magnetism Ionosphere & Radio Wa, West Branch, Kaliningrad, Russia
[2] Russian Acad Sci, Immanuel Kant Balt Fed Univ, Kaliningrad, Russia
[3] Russian Acad Sci, Pushkov Inst Terr Magnetism Ionosphere & Radio Wa, Moscow, Russia
[4] Russian Acad Sci, Inst Solar Terr Phys, Siberian Branch, Irkutsk, Russia
基金
俄罗斯科学基金会;
关键词
ionosphere; longitudinal variations; Weddell Sea anomaly; equatorial anomaly; electron density; numerical simulation; ionosonde; radio occultation observations; MODEL; GPS; PROTONOSPHERE; THERMOSPHERE; PARAMETERS; SYSTEM; CHAMP;
D O I
10.1134/S1990793117060197
中图分类号
O64 [物理化学(理论化学)、化学物理学]; O56 [分子物理学、原子物理学];
学科分类号
070203 ; 070304 ; 081704 ; 1406 ;
摘要
Programs designed for automatic collection and processing of data on the ionospheric F2-layer parameters obtained by the radio occultation method are described. The programs developed make it possible to analyze the dependence of the parameters h (m) F2, foF2, and N (m) F2 on the level of solar activity with a given temporal and spatial resolution, which is important in solving scientific and applied problems. Global maps of the distribution of the maximum electron density of the F2-layer are presented for different seasons and times (UT and LT). The diurnal and seasonal variations of the normalized parameter N (m) F2 are compared with data calculated by empirical and numerical ionospheric models and with ionosonde data. The results calculated in this study reproduce all existing ionospheric anomalies and demonstrate a qualitative agreement with the data obtained by different methods. This indicates that radio occultation observation data can be efficiently used in theoretical research and empirical modeling of the ionosphere.
引用
收藏
页码:1038 / 1046
页数:9
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