The Influence of Ionospheric Neutral Wind Variations on the Morphology and Propagation of Medium Scale Traveling Ionospheric Disturbances on 8th August 2016

被引:10
作者
Luo, Ji [1 ,2 ]
Xu, Jiyao [1 ,2 ]
Wu, Kun [1 ,2 ]
Wang, Wenbin [3 ]
Xiong, Chao [4 ]
Yuan, Wei [1 ,2 ]
机构
[1] Chinese Acad Sci, Natl Space Sci Ctr, State Key Lab Space Weather, Beijing, Peoples R China
[2] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
[3] Natl Ctr Atmospher Res, High Altitude Observ, Pob 3000, Boulder, CO 80307 USA
[4] Wuhan Univ, Coll Elect Informat, Dept Space Phys, Wuhan, 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
All-sky imager; MSTIDs dissipation; Meridian wind influences on the MSTIDs dissipation; MSTIDs propagation direction change; Zonal wind influences on the MSTIDs propagation; ATMOSPHERIC GRAVITY-WAVES; MIDLATITUDE SPREAD-F; AIRGLOW OBSERVATIONS; IMAGES; ELECTRODYNAMICS; NETWORK; FIELDS;
D O I
10.1029/2020JA029037
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
This study reports a special case of the propagation and morphology of medium scale traveling ionospheric disturbances (MSTIDs) over middle-latitude China on the night of August 8, 2016. The MSTIDs were simultaneously observed by multi-instruments, including the all-sky imager, Swarm satellite, and global positioning system (GPS). The MSTIDs lasted for about 6 h in the field view of airglow imager, showing typical wavelength, phase velocity of 272-296 km and 67-250 m/s, respectively. In addition, the imagers show that the inclination angles of phase fronts for some MSTIDs were decreasing during their propagation, resulting in the propagation direction changed from southwestward to nearly westward. More interestingly, the MSTIDs began to dissipate in the airglow observation when they propagated to lower latitudes (below similar to 40 degrees N) whereas the MSTIDs at higher latitudes were still visible in the later local times. Simulation results from the Thermosphere-Ionosphere-Electrodynamics General Circulation Model are fairly consistent with the Fabry-Perot Interferometer (FPI) wind observations, which provide convincing explanation to show that the variations of ionospheric neutral winds might play important roles in the changes of propagation direction and the dissipation of MSTIDs.
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页数:12
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