The possibility of using all-sky meteor radar to observe ionospheric E-region field-aligned irregularities
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  • 英文篇名:The possibility of using all-sky meteor radar to observe ionospheric E-region field-aligned irregularities
  • 作者:XIE ; HaiYong ; LI ; GuoZhu ; NING ; BaiQi ; REID ; Iain ; HU ; LianHuan ; WU ; BaoYuan ; YU ; You ; YANG ; SiPeng
  • 英文作者:XIE HaiYong;LI GuoZhu;NING BaiQi;REID Iain;HU LianHuan;WU BaoYuan;YU You;YANG SiPeng;Key Laboratory of Earth and Planetary Physics,Institute of Geology and Geophysics,Chinese Academy of Sciences;Beijing National Observatory of Space Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences;College of Earth and Planetary Sciences,University of Chinese Academy of Science;ATmospheric RADar (ATRAD) Pty Ltd;School of Physical Sciences,University of Adelaide;
  • 英文关键词:meteor radar;;ionospheric irregularities;;sporadic E layer
  • 中文刊名:JEXG
  • 英文刊名:中国科学:技术科学(英文版)
  • 机构:Key Laboratory of Earth and Planetary Physics,Institute of Geology and Geophysics,Chinese Academy of Sciences;Beijing National Observatory of Space Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences;College of Earth and Planetary Sciences,University of Chinese Academy of Science;ATmospheric RADar (ATRAD) Pty Ltd;School of Physical Sciences,University of Adelaide;
  • 出版日期:2019-07-11 13:49
  • 出版单位:Science China(Technological Sciences)
  • 年:2019
  • 期:v.62
  • 基金:supported by the National Natural Science Foundation of China(Grant Nos.41727803,41574149,41621063)
  • 语种:英文;
  • 页:JEXG201908018
  • 页数:7
  • CN:08
  • ISSN:11-5845/TH
  • 分类号:191-197
摘要
All-sky meteor radars are primarily used for meteor observations. This paper reports the first observations of ionospheric Eregion field-aligned irregularities(FAIs) from a conventional all-sky meteor radar located at Wuhan(31°N, 114°E) for the period of March–June 2018. E-region FAI echoes evident in range-time intensity(RTI) maps show quasiperiodic striations with positive and negative slopes, which are consistent with multiple FAI structures moving across the wide beam of the meteor radar. A statistical analysis shows that out of a total of 111 d, there are 73 d with E-region FAI echoes detected by the meteor radar. The FAI events correspond well with the presence of sporadic-E layers which provide the necessary plasma density gradient for the development of gradient drift instability producing FAIs. The results demonstrate the capability of conventional meteor radars to make simultaneous routine observations of meteors and ionospheric E-region FAIs through incorporating RTI and spectral analysis into the online realtime data processing. Meteor radar observations could potentially address the limitations of ionospheric radars, which cannot provide simultaneous measurements of neutral winds and irregularity structures, and thereby contribute to better understanding of the dynamical processes producing E-region irregularities.
        All-sky meteor radars are primarily used for meteor observations. This paper reports the first observations of ionospheric Eregion field-aligned irregularities(FAIs) from a conventional all-sky meteor radar located at Wuhan(31°N, 114°E) for the period of March–June 2018. E-region FAI echoes evident in range-time intensity(RTI) maps show quasiperiodic striations with positive and negative slopes, which are consistent with multiple FAI structures moving across the wide beam of the meteor radar. A statistical analysis shows that out of a total of 111 d, there are 73 d with E-region FAI echoes detected by the meteor radar. The FAI events correspond well with the presence of sporadic-E layers which provide the necessary plasma density gradient for the development of gradient drift instability producing FAIs. The results demonstrate the capability of conventional meteor radars to make simultaneous routine observations of meteors and ionospheric E-region FAIs through incorporating RTI and spectral analysis into the online realtime data processing. Meteor radar observations could potentially address the limitations of ionospheric radars, which cannot provide simultaneous measurements of neutral winds and irregularity structures, and thereby contribute to better understanding of the dynamical processes producing E-region irregularities.
引文
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