Investigation of Nighttime MSTIDS Observed by Optical Thermosphere Imagers at Low Latitudes: Morphology, Propagation Direction, and Wind Filtering

被引:28
作者
Figueiredo, C. A. O. B. [1 ]
Takahashi, H. [1 ]
Wrasse, C. M. [1 ]
Otsuka, Y. [2 ]
Shiokawa, K. [2 ]
Barros, D. [1 ]
机构
[1] Inst Nacl Pesquisas Espaciais, Sao Jose Dos Campos, Brazil
[2] Nagoya Univ, Inst Space Earth Environm Res, Nagoya, Aichi, Japan
关键词
Gravity waves; TIDs; MSTIDs; Ionoshere; Thermosphere; Airglow images; TRAVELING IONOSPHERIC DISTURBANCES; ATMOSPHERIC GRAVITY-WAVES; MIDNIGHT TEMPERATURE MAXIMUM; QUASI-PERIODIC ECHOES; SPORADIC-E; MIDLATITUDE IONOSPHERE; F-REGION; AIRGLOW OBSERVATIONS; MU RADAR; LAYER;
D O I
10.1029/2018JA025438
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Different types of medium-scale traveling ionospheric disturbances (MSTIDs) have been observed at Cachoeira Paulista (22.4 degrees S; 45.0 degrees W), Brazil, from June 2013 to December 2015, using airglow OI 630.0-nm images. During the period, 58 MSTIDs were identified and classified as follows: dark band MSTIDs (around 10 events) and periodic MSTIDs (48 events). Dark band MSTIDs present phase velocity between 50 and 200m/s and propagation direction to northwestward. On the other hand, periodic MSTIDs have phase velocity of 50 to 200 m/s, horizontal wavelengths from 80 to 160 km, periods ranging between 5 and 45 min, and propagation directions are mainly north-northeastward. The wave parameters indicate that periodic MSTIDs have different characteristics when compared to dark band MSTIDs, suggesting that periodic MSTIDs are not generated through the well-known Perkins and E-F coupling instability. In addition to it, the present study indicates that the spectral characteristics found in Brazil are different from other regions such as Japan and Indonesia. Therefore, we intend to do the statistics of the wave parameters (wavelength, phase velocity, period, propagation direction, and time occurrence) and investigate the generation mechanisms of periodic MSTIDs at low to middle latitude for the first time. Furthermore, the anisotropy observed in periodic MSTID propagation direction can be explained by different mechanisms.
引用
收藏
页码:7843 / 7857
页数:15
相关论文
共 72 条
  • [1] ON THE FRACTAL STRUCTURE OF SMALL-SCALE TRAVELING IONOSPHERIC DISTURBANCES
    Alimov, V. A.
    Vybornov, F. I.
    Rakhlin, A. V.
    [J]. RADIOPHYSICS AND QUANTUM ELECTRONICS, 2008, 51 (01) : 20 - 27
  • [2] Amorim DCM, 2011, J GEOPHYS RES-SPACE, V116, DOI [10.1029/2010JA016090, 10.1029/2010JA016091]
  • [3] [Anonymous], 2010, INFR MON ATM STUD, DOI DOI 10.1007/978-1-4020-9508-5_1
  • [4] Observation of a mesospheric front in a thermal-doppler duct over King George Island, Antarctica
    Bageston, J. V.
    Wrasse, C. M.
    Batista, P. P.
    Hibbins, R. E.
    Fritts, D. C.
    Gobbi, D.
    Andrioli, V. F.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2011, 11 (23) : 12137 - 12147
  • [5] F-LAYER HEIGHT BANDS IN THE NOCTURNAL IONOSPHERE OVER ARECIBO
    BEHNKE, R
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1979, 84 (NA3): : 974 - 978
  • [6] BOWMAN GG, 1989, ANN GEOPHYS, V7, P259
  • [7] SOME ASPECTS OF MID-LATITUDE SPREAD-ES AND ITS RELATIONSHIP WITH SPREAD-F
    BOWMAN, GG
    [J]. PLANETARY AND SPACE SCIENCE, 1985, 33 (09) : 1081 - &
  • [8] Campos J. A. V., 2016, BRAZILIAN J GEOPHYSI, V34, P10, DOI DOI 10.22564/RBGF.V34I4.876
  • [9] Statistical analysis of the occurrence of medium-scale traveling ionospheric disturbances over Brazilian low latitudes using OI 630.0 nm emission all-sky images
    Candido, C. M. N.
    Pimenta, A. A.
    Bittencourt, J. A.
    Becker-Guedes, F.
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (17)
  • [10] Generation of mesoscale F layer structure and electric fields by the combined Perkins and ES layer instabilities, in simulations
    Cosgrove, R. B.
    [J]. ANNALES GEOPHYSICAE, 2007, 25 (07) : 1579 - 1601