Magnetosphere Sawtooth Oscillations Induced by Ionospheric Outflow.

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Bibliographic Details
Title: Magnetosphere Sawtooth Oscillations Induced by Ionospheric Outflow.
Authors: Brambles, O. J., Lotko, W., Zhang, B., Wiltberger, M., Lyon, J., Strangeway, R. J.
Source: Science (pre-March 2025). 6/3/2011, Vol. 332 Issue 6034, p1183-1186. 4p.
Subjects: Magnetosphere, Magnetospheric physics, Oscillations, Ionospheric research, Solar wind, Magnetic fields, Convection (Astrophysics)
Abstract: The sawtooth mode of convection of Earth's magnetosphere is a 2- to 4-hour planetary-scale oscillation powered by the solar wind-magnetosphere-ionosphere (SW-M-I) interaction. Using global simulations of geospace, we have shown that ionospheric O+ outflows can generate sawtooth oscillations. As the outflowing ions fill the inner magnetosphere, their pressure distends the nightside magnetic field. When the outflow fluence exceeds a threshold, magnetic field tension cannot confine the accumulating fluid; an O+-rich plasmoid is ejected, and the field dipolarizes. Below the threshold, the magnetosphere undergoes quasi-steady convection. Repetition and the sawtooth period are controlled by the strength of the SW-M-I interaction, which regulates the outflow fluence. [ABSTRACT FROM AUTHOR]
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Database: Psychology and Behavioral Sciences Collection
Description
Abstract:The sawtooth mode of convection of Earth's magnetosphere is a 2- to 4-hour planetary-scale oscillation powered by the solar wind-magnetosphere-ionosphere (SW-M-I) interaction. Using global simulations of geospace, we have shown that ionospheric O+ outflows can generate sawtooth oscillations. As the outflowing ions fill the inner magnetosphere, their pressure distends the nightside magnetic field. When the outflow fluence exceeds a threshold, magnetic field tension cannot confine the accumulating fluid; an O+-rich plasmoid is ejected, and the field dipolarizes. Below the threshold, the magnetosphere undergoes quasi-steady convection. Repetition and the sawtooth period are controlled by the strength of the SW-M-I interaction, which regulates the outflow fluence. [ABSTRACT FROM AUTHOR]
ISSN:00368075
DOI:10.1126/science.1202869