Abstract

We report on nighttime airglow imaging observations of the low latitude ionosphere by means of a 630-m all-sky imager installed in March 2006 at Yonaguni, Japan (24.5°N, 123.0°E; 14.6°N geomagnetic), about 100 km east of Taiwan. The imager detected medium-scale traveling ionospheric disturbances (MSTIDs) for about 7 hours on the night of 26 May 2006. A dense GPS network in Japan also observed the same MSTID event on this night. The imager and GEONET data indicate that most of the MSTIDs propagated southwestward from the north of Japan to the south of Yonaguni and Taiwan over 4000 km, with a southern limit of 19°N (geomagnetic latitude 9°N) or lower On the night of 10 November 2006, the imager observed two weak emission bands that were embedded on the F-region anomaly crest to the south of Yonaguni. The simultaneous electron density profiles from the FORMOSAT-3/COSMIC mission demonstrate that the weak emission bands are due to density depletions in equatorial plasma bubbles. These case studies suggest that the Yonaguni imager in collaboration with other instruments is very suitable for the study of ionospheric disturbances in and around the northern F-region anomaly crest.

Highlights

  • Traveling ionospheric disturbances (TIDs) with horizontal scales of > 100 km in the F-region ionosphere have been extensively studied by means of radio techniques (Hunsucker 1982; Hocke and Schlegel 1996)

  • Recent new observation techniques using all-sky CCD imagers and Global Positioning System (GPS) satellites have brought about a new era of TID studies

  • The observational results are summarized as follows: (1) medium-scale traveling ionospheric disturbances (MSTIDs) were observed for about 7 hours on the night of 26 May 2006 by the imager at Yonaguni

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Summary

INTRODUCTION

Traveling ionospheric disturbances (TIDs) with horizontal scales of > 100 km in the F-region ionosphere have been extensively studied by means of radio techniques (Hunsucker 1982; Hocke and Schlegel 1996). These techniques have clarified various characteristics of TIDs most of the observations have been made at a fixed location with a single method. To monitor ionospheric disturbances routinely at low latitude in East Asia, we installed an all-sky airglow imager on Yonaguni Island, Japan (24.5°N, 123.0°E; 14.6°N geomagnetic), about 100 km east of Taiwan, in March 2006. This paper gives the first results from this imager to demonstrate capability for monitoring MSTIDs and plasma bubbles in a wide area over Yonaguni and Taiwan, and shows an example of a bubble simultaneously observed by the imager and the FORMOSAT-3/COSMIC mission

OBSERVATIONS
Medium-Scale Traveling Ionospheric Disturbances
Plasma Bubbles
DISCUSSION AND CONCLUDING
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