Modeling of equatorial plasma bubbles triggered by non-equatorial traveling ionospheric disturbances
Article first published online: 19 APR 2011
Copyright 2011 by the American Geophysical Union.
Geophysical Research Letters
Volume 38, Issue 8, 28 April 2011
How to Cite
2011), Modeling of equatorial plasma bubbles triggered by non-equatorial traveling ionospheric disturbances, Geophys. Res. Lett., 38, L08103, doi:10.1029/2011GL046890., , , , , , and (
- Issue published online: 19 APR 2011
- Article first published online: 19 APR 2011
- Manuscript Accepted: 10 FEB 2011
- Manuscript Revised: 7 FEB 2011
- Manuscript Received: 24 JAN 2011
- equatorial spread-F
 The Naval Research Laboratory three-dimensional simulation code SAMI3/ESF is used to study the response of the post-sunset ionosphere to electrified mesoscale traveling ionospheric disturbances (MSTIDs). An MSTID is modeled as an externally-imposed traveling-wave E field with wavelength 250 km and period 1 h that drives vertical E × B drifts of up to ±50 m/s. We find that the coupling between the MSTID at low- to mid-latitudes and the equatorial F layer leads to growth of equatorial plasma bubbles (EPBs). This coupling is strongest when the wave vector is perpendicular to the geomagnetic field. Model results reproduce key features of observed nighttime MSTIDs and associated EPBs.