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电离层加热实验中反射高度下降特征的数值模拟

程木松 徐彬 吴振森 李海英 许正文 吴军 吴健

电波科学学报2016,Vol.31Issue(5):834-842,9.
电波科学学报2016,Vol.31Issue(5):834-842,9.DOI:10.13443/j.cjors.2015041101

电离层加热实验中反射高度下降特征的数值模拟

A simulation of the descending reflection height in ionospheric heating experiment

程木松 1徐彬 2吴振森 3李海英 4许正文 5吴军 5吴健4

作者信息

  • 1. 中国电子科技集团公司第三十八研究所,合肥 230088
  • 2. 西安电子科技大学 物理与光电工程学院,西安 710071
  • 3. 中国电波传播研究所 电波环境特性及模化技术重点实验室,青岛 266107
  • 4. 中国电波传播研究所 电波环境特性及模化技术重点实验室,青岛 266107
  • 5. 西安电子科技大学 物理与光电工程学院,西安 710071
  • 折叠

摘要

Abstract

Enhanced ion and plasma lines can be observed by the ground-based incoherent radar when high power HF waves were transmited into ionosphere.An ionospheric heating experiment was carried out in the fall of 2010,Norway.The long-lived enhanced ion and plasma lines were first observed in this ex-periment,and this may be caused by the Parametric Decay Instability (PDI).In addition,the VHF data show that the enhanced lines are descending in altitude with time during the heater-on period.The possible cause for the descending altitude may be the enhanced electron diffusion.In this paper,the reflection height is simulated based on the parameters of modified IRI and MSISE models,and results show that the reflection height can be descent with time due to the enhanced diffusion.A good agreement is obtained be-tween the simulation and experiment,thus the hypothesis is proved to be reliable.

关键词

电离层加热/离子线/等离子体线/反射高度

Key words

ionospheric heating/ion lines/plasma lines/reflection height

分类

天文与地球科学

引用本文复制引用

程木松,徐彬,吴振森,李海英,许正文,吴军,吴健..电离层加热实验中反射高度下降特征的数值模拟[J].电波科学学报,2016,31(5):834-842,9.

基金项目

国家自然科学基金(40831062,41004065,41104108) (40831062,41004065,41104108)

中央高校基本科研基金(K5051207003) (K5051207003)

空间天气学国家重点实验室(08262DAA4S) (08262DAA4S)

电波环境特性及模化技术国防重点实验室基金 ()

电波科学学报

OA北大核心CSCDCSTPCD

1005-0388

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