Time scales of expansion and contraction of the auroral oval
- 1 April 1986
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 91 (A4) , 4437-4450
- https://doi.org/10.1029/ja091ia04p04437
Abstract
The auroral boundary index calculated by Gussenhoven et al. [1983] on the basis of Defense Meteorological Satellite Program precipitating electron data is used to examine the dynamics of the auroral oval in the midnight sector. The equatorward boundary of the oval expands equatorward and contracts poleward corresponding to southward and northward turnings, respectively, of the interplanetary magnetic field (IMF). The time scales are found to be, on the average, 45 min for the expansion and 8 hours for the contraction. A general empirical formula to predict the oval location for any IMF variation is devised. Physical processes in the magnetosphere consistent with the “rapid” expansion and “slow” contraction of the auroral oval are discussed.Keywords
This publication has 40 references indexed in Scilit:
- Ring current simulation in connection with interplanetary space conditionsPlanetary and Space Science, 1984
- The inner edge of the plasma sheet and the diffuse auroraJournal of Geophysical Research, 1984
- A theoretical approach to the morphology and the dynamics of diffuse auroral zonesJournal of Geophysical Research, 1983
- Theoretical magnetograms based on quantitative simulation of a magnetospheric substormJournal of Geophysical Research, 1982
- Plasma and electric field boundaries at high and low altitudes on July 29, 1977Journal of Geophysical Research, 1982
- DMSP/F2 electron observations of equatorward auroral boundaries and their relationship to magnetospheric electric fieldsJournal of Geophysical Research, 1981
- Trajectory traces of charged particles in the magnetosphereJournal of Geophysical Research, 1978
- An empirical relationship between interplanetary conditions andDstJournal of Geophysical Research, 1975
- Dynamics of auroral belt and polar geomagnetic disturbancesPlanetary and Space Science, 1967
- The main phase of great magnetic stormsJournal of Geophysical Research, 1963