TY - JOUR
T1 - Space-based imaging of nighttime medium-scale traveling ionospheric disturbances using FORMOSAT-2/ISUAL 630.0 nm airglow observations
AU - Rajesh, P. K.
AU - Liu, J. Y.
AU - Lin, C. H.
AU - Chen, A. B.
AU - Hsu, R. R.
AU - Chen, C. H.
AU - Huba, J. D.
N1 - Funding Information:
FORMOSAT-2/ISUAL data used in this study are obtained with the permission of ISUAL science group at National Cheng Kung University, Taiwan (http://sprite.phys.ncku.edu.tw/En/Eindex.html). SAMI2 is an open source model developed at the Naval Research Laboratory and is available at http://www.nrl.navy.mil/ppd/branches/6790/sami2. This work is supported by the Ministry of Science and Technology grants MOST 104-2119-M-006-019, 103-2923-M-006-002-MY3, and 103-2111-M-006-003-MY3 to National Cheng Kung University, Taiwan and MOST 104-2628-M-008-001 to National Central University, Taiwan.
Publisher Copyright:
©2016. American Geophysical Union. All Rights Reserved.
PY - 2016/5/1
Y1 - 2016/5/1
N2 - This paper reports the results of space-based imaging of nighttime medium-scale traveling ionospheric disturbances (MSTIDs) in 630.0 nm emission by Imager of Sprites and Upper Atmospheric Lightnings (ISUAL), on board FORMOSAT-2 satellite. The limb integrated measurements, after removing background, reveal multiple bands of intensity perturbation when projected to a horizontal plane corresponding to the altitude of peak emission, with distinct southwest to northeast orientation in the Southern Hemisphere. Simulations are carried out by artificially introducing MSTID fluctuations in model electron density to confirm if the MSTID could be identified in the ISUAL-viewing geometry. The ISUAL observations in year 2007 are further used to investigate the MSTID features as well as occurrence characteristics in the Southern Hemisphere, most of which are over the ocean where no ground-based observations are available. The preliminary statistics shows more MSTID occurrence in solstices with peak in June–July months. Majority of the MSTID perturbations have wavelength in the range 150–300 km, and the wavefronts are aligned at about 30°–50° from the east-west plane. The statistic results of the orientation of wavefronts indicate that Es layer instability might be important in the MSTID generation.
AB - This paper reports the results of space-based imaging of nighttime medium-scale traveling ionospheric disturbances (MSTIDs) in 630.0 nm emission by Imager of Sprites and Upper Atmospheric Lightnings (ISUAL), on board FORMOSAT-2 satellite. The limb integrated measurements, after removing background, reveal multiple bands of intensity perturbation when projected to a horizontal plane corresponding to the altitude of peak emission, with distinct southwest to northeast orientation in the Southern Hemisphere. Simulations are carried out by artificially introducing MSTID fluctuations in model electron density to confirm if the MSTID could be identified in the ISUAL-viewing geometry. The ISUAL observations in year 2007 are further used to investigate the MSTID features as well as occurrence characteristics in the Southern Hemisphere, most of which are over the ocean where no ground-based observations are available. The preliminary statistics shows more MSTID occurrence in solstices with peak in June–July months. Majority of the MSTID perturbations have wavelength in the range 150–300 km, and the wavefronts are aligned at about 30°–50° from the east-west plane. The statistic results of the orientation of wavefronts indicate that Es layer instability might be important in the MSTID generation.
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U2 - 10.1002/2015JA022334
DO - 10.1002/2015JA022334
M3 - Article
AN - SCOPUS:84971242696
SN - 2169-9402
VL - 121
SP - 4769
EP - 4781
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 5
ER -