VHF radar observations of the dip equatorial E-region during sunset in the Brazilian sector

• Main Authors: C. M. Denardini, M. A. Abdu, E. R. de Paula, C. M. Wrasse, J. H. A. Sobral
• Format: Article
• Language: English
• Published: Copernicus Publications 2006-07-01
• Series: Annales Geophysicae
• Online Access: https://www.ann-geophys.net/24/1617/2006/angeo-24-1617-2006.pdf

Using the RESCO 50 MHz backscatter radar (2.33&deg; S, 44.2&deg; W, DIP: &ndash;0.5), at S&#227;o Lu&#237;s, Brazil, we obtained Range Time Intensity (RTI) maps covering the equatorial electrojet heights during daytime and evening. These maps revealed a scattering region at an altitude of about 108 km during the sunset period. The type of 3-m irregularity region we present here has not been reported before in the literature, to our knowledge. It was mainly observed around the Southern Hemisphere summer-solstice period, under quiet magnetic activity condition. The occurrence of this echo region coincides in local time with the maximum intensity of an evening pre-reversal eastward electric field of the ionospheric <i>F</i>-region. A tentative explanation is proposed here in terms of the theory of the divergence of the equatorial electrojet (EEJ) current in the evening ionosphere presented by Haerendel and Eccles (1992), to explain the partial contribution of the divergence to the development of the pre-reversal electric field. The theory predicts an enhanced zonal electric field and hence a vertical electric field below 300 km as a consequence of the EEJ divergence in the evening. The experimental results of the enhanced echoes from the higher heights of the EEJ region seem to provide evidence that the divergence of the EEJ current can indeed be the driver of the observed scattering region.