Model simulation of the large-scale high-latitude F-layer modification by powerful HF waves with different modulation

被引:4
|
作者
Mingaleva, G. I. [1 ]
Mingalev, V. S. [1 ]
Mingalev, I. V. [1 ]
机构
[1] Russian Acad Sci, Kola Sci Ctr, Polar Geophys Inst, Apatity 184209, Murmansk Region, Russia
关键词
High-latitude ionosphere; Active experiments; Modeling and forecasting; Plasma temperature and density; RADIO-WAVES; OPTICAL-EMISSIONS; IONOSPHERIC MODIFICATION; HEATING EXPERIMENTS; EISCAT OBSERVATIONS; MAGNETIC ZENITH; INDUCED AIRGLOW; REGION; ENHANCEMENTS; FREQUENCIES;
D O I
10.1016/j.jastp.2008.11.007
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 mathematical model of the high-latitude ionosphere, developed earlier, is applied to investigate how the modulation regime of the ionospheric HF heating facility near Tromso, Scandinavia, affects the large-scale high-latitude F-layer modification. Simulations are made for distinct cases, in which high-power waves have different modulations, namely, for continuous wave transmission and for pulse operation, with the amplitude of the HF wave being square wave-modulated. The calculations are performed for different lengths of pulses and various time intervals between successive pulses. The frequency of HF waves is chosen to be close to the most effective frequency for the large-scale F2-layer modification. Simulations are made for autumn and low geomagnetic activity conditions both for nocturnal and for daytime conditions. The results of modeling indicate that the most considerable decrease in the F-region electron concentration may be achieved when the heater is operated continuously. Moreover, the perceptible decrease in the F-region electron concentration may take place when the heating facility is operated pulsatily. For the pulse operation, the amplitude of the electron concentration variations depends on the ratio of the length of pulses to the time interval between successive pulses. The higher the latter ratio is, the more the electron concentration variation amplitude ought to be. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:559 / 568
页数:10
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