Satellite model of foF2 in winter high-latitude ionosphere describing the trough structure

被引:5
作者
Karpachev, Alexander T. [1 ]
Klimenko, Maksim, V [2 ]
Klimenko, Vladimir V. [2 ]
Chirik, Nikolay, V [2 ]
Zhbankov, Gennadiy A. [3 ]
Pustovalova, Lubov, V [1 ]
机构
[1] Russian Acad Sci, Pushkov Inst Terr Magnetism Ionosphere & Radio Wa, Moscow, Troitsk Region, Russia
[2] St Petersburg Univ, West Dept, Pushkov Inst Terr Magnetism Ionosphere & Radio Wa, Russian Acad Sci, Kaliningrad, Russia
[3] Southern Fed Univ, Rostov Na Donu, Russia
关键词
Ionosphere; foF2; Main ionospheric trough; Empirical model; LOCAL TIME; F-REGION; MAIN TROUGH; DEPENDENCE; LONGITUDE; MIDLATITUDE; COSMOS-900; ALTITUDE; SEASON; LAYER;
D O I
10.1016/j.asr.2021.07.014
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
An empirical foF2 model was constructed for the winter high-latitude ionosphere taking into account the structure of the ionization trough. This model describes the trough position and its shape in terms of longitudinal-latitudinal variations in foF2 in geographic latitude intervals of 40-85 degrees N and 40-85 degrees S. The model is valid for November to February in the Northern hemisphere and May-August in the Southern hemisphere. The simulation describes quiet geomagnetic conditions (Kp from 0 to 3+ for all local time (LT) and universal time (UT) hours at any solar activity level in the interval F10.7 = 70-200 s.f.u. The model is based on the Cosmos-900, Interkosmos-19 and CHAMP satellite data. The radio occultation observation data obtained from the GRACE, CHAMP and COSMIC/FORMOSAT experiments were partially used. The International Reference Ionosphere (IRI) was also used; thus, the ground-based station data were indirectly considered. Within the model framework, the variations in the trough minimum position with longitude and local time were identified and studied in detail. The latitudinal and longitudinal variations in foF2 were also revealed and investigated. The constructed model more adequately reproduces variations in foF2 than the IRI-2016 model. The new model is available on the IZMIRAN website: http://www.izmiran.ru/ionosphere/sm-mit/. (c) 2021 COSPAR. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:2 / 15
页数:14
相关论文
共 33 条
[1]   TOPSIDE IONOSPHERIC TROUGH MORPHOLOGY - OCCURRENCE FREQUENCY AND DIURNAL, SEASONAL, AND ALTITUDE VARIATIONS [J].
AHMED, M ;
SAGALYN, RC ;
WILDMAN, PJL ;
BURKE, WJ .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1979, 84 (NA2) :489-498
[2]  
Annakuliev S.K., 1997, Geomag. Aeron., V37, P83
[3]   Principles of Processing and Selection of Radio Occultation Observation Data for Investigating the Ionospheric F2-Layer [J].
Chirik, N. V. ;
Klimenko, M. V. ;
Klimenko, V. V. ;
Karpachev, A. T. ;
Ratovskii, K. G. ;
Koren'kova, N. A. .
RUSSIAN JOURNAL OF PHYSICAL CHEMISTRY B, 2017, 11 (06) :1038-1046
[4]   ON THE FORMATION OF DAYTIME TROUGHS IN THE F-REGION WITHIN THE PLASMASPHERE [J].
EVANS, JV ;
HOLT, JM ;
WAND, RH .
GEOPHYSICAL RESEARCH LETTERS, 1983, 10 (05) :405-408
[5]  
Feichter E, 2002, ANN GEOPHYS-ITALY, V45, P117
[6]   LOCATION AND SOURCE OF IONOSPHERIC HIGH-LATITUDE TROUGHS [J].
GREBOWSKY, JM ;
TAYLOR, HA ;
LINDSAY, JM .
PLANETARY AND SPACE SCIENCE, 1983, 31 (01) :99-105
[7]   MODEL OF F2 PEAK ELECTRON-DENSITIES IN MAIN TROUGH REGION OF IONOSPHERE [J].
HALCROW, BW ;
NISBET, JS .
RADIO SCIENCE, 1977, 12 (05) :815-820
[8]   Dynamics of Main and Ring Ionospheric Troughs at the Recovery Phase of Storms/Substorms [J].
Karpachev, A. T. .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2021, 126 (01)
[9]   Variations in the Winter Troughs' Position With Local Time, Longitude, and Solar Activity in the Northern and Southern Hemispheres [J].
Karpachev, A. T. .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2019, 124 (10) :8039-8055
[10]   Model of the Ionospheric Trough for Daytime Winter Conditions Based on Data from Interkosmos-19 and Champ Satellites [J].
Karpachev, A. T. .
GEOMAGNETISM AND AERONOMY, 2019, 59 (04) :383-397