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AGU: Journal of Geophysical Research, Space Physics

 

Keywords

  • gravity waves
  • ionosphere
  • E region

Index Terms

  • Ionosphere: Equatorial ionosphere
  • Ionosphere: Electric fields
  • Radio Science: Ionospheric physics
  • Atmospheric Composition and Structure: Middle atmosphere: energy deposition
  • Radio Science: Radar atmospheric physics
Abstract
Cited By (2)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, A11308, 8 PP., 2009
doi:10.1029/2009JA014177

Climatology of gravity waves–induced electric fields in the equatorial E region

H. C. Aveiro

Divisao de Aeronomia, Instituto Nacional de Pesquisas Espaciais, Sao Paulo, Brazil

C. M. Denardini

Divisao de Aeronomia, Instituto Nacional de Pesquisas Espaciais, Sao Paulo, Brazil

M. A. Abdu

Divisao de Aeronomia, Instituto Nacional de Pesquisas Espaciais, Sao Paulo, Brazil

Equatorial electrojet (EEJ) observations using VHF radars show backscattered echoes from two types of electron density irregularities explained by the modified two-stream (Type I) and the gradient drift (Type II) instabilities. From the Type II irregularity velocities obtained by a radar installed at São Luiz Space Observatory (2.58°S, 44.23°W, magnetic latitude 0.23°S) we have inferred the vertical electric fields (Ez). The Ez inference was based on geomagnetic field and atmospheric models. A harmonic analysis of these electric fields shows the presence of gravity waves (GW) induced oscillations in the EEJ. We calculated the ratio between GW-related electric fields and the total Ez, which is an indicator of the efficiency in the production of an additional electric field due to a gravity wave neutral wind. In the present paper we describe the methodology of analysis and discuss some characteristics of the gravity waves that could modify the equatorial ionospheric electric fields.

Received 25 February 2009; accepted 17 July 2009; published 14 November 2009.

Citation: Aveiro, H. C., C. M. Denardini, and M. A. Abdu (2009), Climatology of gravity waves–induced electric fields in the equatorial E region, J. Geophys. Res., 114, A11308, doi:10.1029/2009JA014177.

Cited By

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