Postmidnight equatorial plasma irregularities on the June solstice during low solar activity - a case study

被引:4
|
作者
Candido, Claudia M. N. [1 ,2 ]
Shi, Jiankui [1 ]
Batista, Inez S. [2 ]
Becker-Guedes, Fabio [2 ]
Correia, Emilia [2 ,6 ]
Abdu, Mangalathayil A. [2 ,4 ]
Makela, Jonathan [3 ]
Balan, Nanan [7 ]
Chapagain, Narayan [5 ]
Wang, Chi [1 ]
Liu, Zhengkuan [1 ]
机构
[1] Chinese Acad Sci, Natl Space Sci Ctr, State Key Lab, China Brazil Joint Lab Space Weather, Beijing, Peoples R China
[2] Natl Inst Space Res INPE, Sao Jose Dos Campos, SP, Brazil
[3] Univ Illinois, Dept Elect & Comp Engn, 1406 W Green St, Urbana, IL 61801 USA
[4] Inst Tecnol Aeronaut ITA, Sao Jose Dos Campos, Brazil
[5] Tribhuvan Univ, Dept Phys, Patan Multiple Campus, Latitpur, Nepal
[6] Univ Presbiteriana Mackenzie, Ctr Radio Astron & Astrofis Mackenzie, Sao Paulo, Brazil
[7] Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
FIELD-ALIGNED IRREGULARITIES; SPREAD-F; REGION; BUBBLES; RADAR;
D O I
10.5194/angeo-37-657-2019
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We present a case study of unusual spread-F structures observed by ionosondes at two equatorial and low-latitude Brazilian stations - Sao Luis (SL: 44.2 degrees W, 2.33 degrees S; dip angle: -6.9 degrees) and Fortaleza (FZ: 38.45 degrees W, 3.9 degrees S; dip angle: -16 degrees). The irregularity structures observed from midnight to postmidnight hours of moderate solar activity (F10.7 < 97 sfu, where 1 sfu = 10(-22) W m(-2) s(-1)) have characteristics different from typical post-sunset equatorial spread F. The spread-F traces first appeared at or above the F-layer peak and gradually became well-formed mixed spread F. They also appeared as plasma depletions in the 630.0 nm airglow emissions made by a wide-angle imager located at the nearby low-latitude station Cajazeiras (CZ: 38.56 degrees W, 6.87 degrees S; dip angle: -21.4 degrees). The irregularities appeared first over FZ and later over SL, giving evidence of an unusual westward propagation or a horizontal plasma advection. The drift-mode operation available in one of the ionosondes (a digital portable sounder, DPS-4) has enabled us to analyze the horizontal drift velocities and directions of the irregularity movement. We also analyzed the neutral wind velocity measured by a Fabry-Perot interferometer (FPI) installed at CZ and discuss its possible role in the development of the irregularities.
引用
收藏
页码:657 / 672
页数:16
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