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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 22, issue 12
Ann. Geophys., 22, 4071-4076, 2004
https://doi.org/10.5194/angeo-22-4071-2004
© Author(s) 2004. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 22, 4071-4076, 2004
https://doi.org/10.5194/angeo-22-4071-2004
© Author(s) 2004. This work is distributed under
the Creative Commons Attribution 3.0 License.

  22 Dec 2004

22 Dec 2004

High altitude large-scale plasma waves in the equatorial electrojet at twilight

J. L. Chau1 and D. L. Hysell2 J. L. Chau and D. L. Hysell
  • 1Radio Observatorio de Jicamarca, Instituto Geofísico del Perú, Lima, Peru
  • 2Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York, USA

Abstract. Jicamarca radar observations of a new class of large-scale plasma waves in the equatorial electrojet (EEJ) are presented and characterized. The study is based on long-term (204 days), single-baseline interferometry observations made in 2003 using a low-power radar mode, also known as JULIA mode, along with a few hours of observations made in an aperture synthesis imaging mode. The large-scale waves are found to occur at high altitudes in the E-region, mainly between 120 and 140km, around twilight (between 18:30 and 20:00 LT), with durations of a few minutes to an hour. In our long-term observations, these large-scale waves occur very often (between 1 and 5 out 10 nights), drift westward (~70 ms–1), exhibit very narrow spectral widths, and have both positive and negative Doppler shifts. The imaging results show that the large-scale waves occur along tilted bands that sweep westward and downward (~30–60ms–1), with a horizontal separation between bands of about 10–15km. The cause of the waves remains unknown.

Key words. Ionosphere (ionospheric irregularities; equatorial ionosphere; instruments and techniques)

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