A comparison of numerical simulation and measurements during ionospheric heating

High power radio wave heating of the ionospheric plasma can induce disturbances of electron temperature and density, and modify the ionosphere. The numerical model can be presented from a series of continuity equation, momentum equation and energy equation. The heating disturbances of the electron d...

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Bibliographic Details
Main Authors: Wang Zhan-Ge, Xu Bin, Xu Zheng-Wen, Wu Jian, Wu Jun, Zhao Hai-Sheng, 北京8701信箱
Format: Report
Language:Chinese
Published: 2012
Subjects:
Online Access:http://ir.nssc.ac.cn/handle/122/3143
id ftchinacadscnssc:oai:ir.nssc.ac.cn:122/3143
record_format openpolar
spelling ftchinacadscnssc:oai:ir.nssc.ac.cn:122/3143 2023-05-15T18:33:50+02:00 A comparison of numerical simulation and measurements during ionospheric heating Wang Zhan-Ge Xu Bin Xu Zheng-Wen Wu Jian Wu Jun Zhao Hai-Sheng 北京8701信箱 2012 http://ir.nssc.ac.cn/handle/122/3143 中文 chi CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION Wang Zhan-Ge; Xu Bin; Xu Zheng-Wen; Wu Jian; Wu Jun; Zhao Hai-Sheng.A comparison of numerical simulation and measurements during ionospheric heating,CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2012,55(3):751-759 http://ir.nssc.ac.cn/handle/122/3143 8 Ionospheric Heating Numerical Simulation Electron Temperature And Density Incoherent Scatter Radar 空间物理 期刊论文 2012 ftchinacadscnssc 2019-09-21T06:43:15Z High power radio wave heating of the ionospheric plasma can induce disturbances of electron temperature and density, and modify the ionosphere. The numerical model can be presented from a series of continuity equation, momentum equation and energy equation. The heating disturbances of the electron density and temperature in polar ionosphere are presented and the effects of the pump parameters are discussed. It shows that electron temperature almost increases in all altitude, however,the peak at the reflection altitude is not clear. Electron density vale is formed at the altitude above peak, and density peaks appear around both sides of it. The heating characteristic increases with the increment of the heating power and the decrement of the pump frequency. Using the parameters of the ionospheric modification experiments carried out in January 2008 at Tromso, Norway as initialization, the six 0 mode heating cases are simulated, and the results are consistent with the observation very well. Report Tromso Tromso National Space Science Center: NSSC OpenIR (Chinese Academy of Sciences) Norway Tromso ENVELOPE(16.546,16.546,68.801,68.801)
institution Open Polar
collection National Space Science Center: NSSC OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacadscnssc
language Chinese
topic Ionospheric Heating
Numerical Simulation
Electron Temperature And Density
Incoherent Scatter Radar
空间物理
spellingShingle Ionospheric Heating
Numerical Simulation
Electron Temperature And Density
Incoherent Scatter Radar
空间物理
Wang Zhan-Ge
Xu Bin
Xu Zheng-Wen
Wu Jian
Wu Jun
Zhao Hai-Sheng
北京8701信箱
A comparison of numerical simulation and measurements during ionospheric heating
topic_facet Ionospheric Heating
Numerical Simulation
Electron Temperature And Density
Incoherent Scatter Radar
空间物理
description High power radio wave heating of the ionospheric plasma can induce disturbances of electron temperature and density, and modify the ionosphere. The numerical model can be presented from a series of continuity equation, momentum equation and energy equation. The heating disturbances of the electron density and temperature in polar ionosphere are presented and the effects of the pump parameters are discussed. It shows that electron temperature almost increases in all altitude, however,the peak at the reflection altitude is not clear. Electron density vale is formed at the altitude above peak, and density peaks appear around both sides of it. The heating characteristic increases with the increment of the heating power and the decrement of the pump frequency. Using the parameters of the ionospheric modification experiments carried out in January 2008 at Tromso, Norway as initialization, the six 0 mode heating cases are simulated, and the results are consistent with the observation very well.
format Report
author Wang Zhan-Ge
Xu Bin
Xu Zheng-Wen
Wu Jian
Wu Jun
Zhao Hai-Sheng
北京8701信箱
author_facet Wang Zhan-Ge
Xu Bin
Xu Zheng-Wen
Wu Jian
Wu Jun
Zhao Hai-Sheng
北京8701信箱
author_sort Wang Zhan-Ge
title A comparison of numerical simulation and measurements during ionospheric heating
title_short A comparison of numerical simulation and measurements during ionospheric heating
title_full A comparison of numerical simulation and measurements during ionospheric heating
title_fullStr A comparison of numerical simulation and measurements during ionospheric heating
title_full_unstemmed A comparison of numerical simulation and measurements during ionospheric heating
title_sort comparison of numerical simulation and measurements during ionospheric heating
publishDate 2012
url http://ir.nssc.ac.cn/handle/122/3143
long_lat ENVELOPE(16.546,16.546,68.801,68.801)
geographic Norway
Tromso
geographic_facet Norway
Tromso
genre Tromso
Tromso
genre_facet Tromso
Tromso
op_relation CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
Wang Zhan-Ge; Xu Bin; Xu Zheng-Wen; Wu Jian; Wu Jun; Zhao Hai-Sheng.A comparison of numerical simulation and measurements during ionospheric heating,CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2012,55(3):751-759
http://ir.nssc.ac.cn/handle/122/3143
op_rights 8
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