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Geomagnetic conjugate observations of medium-scale traveling ionospheric disturbances at midlatitude using all-sky airglow imagers

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TLDR
In this article, the first time simultaneous observations of medium-scale traveling ionospheric disturbances (MSTIDs) at geomagnetic conjugate points in both hemispheres, using two all-sky airglow imagers at midlatitudes, were reported.
Abstract
[1] We report for the first time simultaneous observations of medium-scale traveling ionospheric disturbances (MSTIDs) at geomagnetic conjugate points in both hemispheres, using two all-sky airglow imagers at midlatitudes. A 630-nm all-sky CCD imager at Sata, Japan, detected MSTIDs with a wavefront elongated from NW to SE on the night of August 9, 2002. During this event, MSTIDs with a wavefront elongated from SW to NE were observed at the geomagnetic conjugate point, Darwin, Australia. To investigate geomagnetic conjugacy of the MSTID structures, the Darwin images were mapped The MSTID structures mapped from Darwin to its magnetic conjugate points along the geomagnetic field lines (B) coincide closely with those in the Sata images. This result suggests that polarization electric field (Ep) plays an important role in the generation of MSTIDs. Ep maps along B and moves the F region plasma upward or downward by E × B drifts, causing plasma density perturbations with structures mirrored in the northern and southern hemispheres.

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Journal ArticleDOI

Medium‐scale traveling ionospheric disturbances detected with dense and wide TEC maps over North America

TL;DR: In this article, the TEC maps reveal that the nighttime MSTIDs propagate southwestward with 200-500 km wavelengths over North America and have wavefronts longer than ∼2,000 km.
Journal ArticleDOI

Three‐dimensional simulation of the coupled Perkins and Es‐layer instabilities in the nighttime midlatitude ionosphere

TL;DR: In this article, a three-dimensional numerical model was used to simulate two instability mechanisms: Perkins instability in the F-region and sporadic-E (Es)-layer instability in E-region.
Journal ArticleDOI

GPS observations of medium-scale traveling ionospheric disturbances over Europe

TL;DR: In this article, a two-dimensional structure of medium-scale traveling ionospheric disturbances (MSTIDs) over Europe has been revealed, for the first time, by using maps of the total electron content (TEC) obtained from more than 800 GPS receivers of the European GPS receiver networks.
Journal ArticleDOI

Climatological study of GPS total electron content variations caused by medium‐scale traveling ionospheric disturbances

TL;DR: In this article, the authors investigated total electron content (TEC) perturbations associated with medium-scale traveling ionospheric disturbances (MSTIDs) and found that MSTIDs activity during daytime is different from that during nighttime with respect to seasonal, solar activity, longitudinal, and latitudinal dependences.
Journal ArticleDOI

Propagation characteristics of nighttime mesospheric and thermospheric waves observed by optical mesosphere thermosphere imagers at middle and low latitudes

TL;DR: In this paper, the authors review measurements of nighttime atmospheric/ionospheric waves in the upper atmosphere in Japan, Indonesia, and Australia, using all-sky airglow imagers of optical mesosphere thermosphere imagers (OMTIs).
References
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Journal ArticleDOI

Internal atmospheric gravity waves at ionospheric heights

TL;DR: In this paper, the proper interpretation of irregular motions in the upper atmosphere has been investigated by a variety of techniques, but their proper interpretation has yet to be established. But their proper meaning has not yet been established.
Book ChapterDOI

Internal Atmospheric Gravity Waves at Ionospheric Heights

TL;DR: In this article, the proper interpretation of irregular motions in the upper atmosphere has been investigated by a variety of techniques, but their proper interpretation has yet to be established. But their proper meaning has not yet been established.
Journal ArticleDOI

Atmospheric gravity waves generated in the high‐latitude ionosphere: A review

TL;DR: A review of theoretical and observational results describing atmospheric gravity wave (AGW)/traveling ionospheric disturbance (TID) phenomena at high latitudes is presented in this paper.
Journal ArticleDOI

Polarization fields produced by winds in the equatorial F-region

TL;DR: In this article, the E-layer conductivity may be too small to close this circuit, so that polarization fields build up in the F-layer, causing the plasma to drift with the wind.
Journal ArticleDOI

Spread F and ionospheric currents

TL;DR: In this paper, it was shown that the widely used equilibrium in which the nighttime F region is supported by E×B drifts is unstable if, in addition to the supporting eastward field, a north-south electric field component exists.
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