The possibility of using all-sky meteor radar to observe ionospheric E-region field-aligned irregularities

被引:13
|
作者
Xie HaiYong [1 ,2 ]
Li GuoZhu [1 ,2 ,3 ]
Ning BaiQi [1 ,2 ]
Red, Iain [4 ,5 ]
Hu LianHuan [1 ,2 ]
Wu BaoYuan [2 ]
Yu You [1 ,3 ]
Yang SiPeng [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Inst Geol & Geophys, Beifing Natl Observ Space Environm, Beijing 100029, Peoples R China
[3] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100029, Peoples R China
[4] ATmospher RADar ATRAD Pty Ltd, Thebarton 5031, Australia
[5] Univ Adelaide, Sch Phys Sci, Adelaide, SA 5005, Australia
基金
中国国家自然科学基金;
关键词
meteor radar; ionospheric irregularities; sporadic E layer; QUASI-PERIODIC ECHOES; SPORADIC-E LAYER; LOW-LATITUDE; VHF RADAR; BACKSCATTER; MECHANISM; MIDDLE;
D O I
10.1007/s11431-018-9418-5
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
All-sky meteor radars are primarily used for meteor observations. This paper reports the first observations of ionospheric E-region field-aligned irregularities (FAIs) from a conventional all-sky meteor radar located at Wuhan (31 degrees N, 114 degrees 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.
引用
收藏
页码:1431 / 1437
页数:7
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