Magnetosphere Sawtooth Oscillations Induced by Ionospheric Outflow.

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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]
Copyright of Science (pre-March 2025) is the property of American Association for the Advancement of Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
Database: Psychology and Behavioral Sciences Collection
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  Data: Magnetosphere Sawtooth Oscillations Induced by Ionospheric Outflow.
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  Data: <searchLink fieldCode="AR" term="%22Brambles%2C+O%2E+J%2E%22">Brambles, O. J.</searchLink><br /><searchLink fieldCode="AR" term="%22Lotko%2C+W%2E%22">Lotko, W.</searchLink><br /><searchLink fieldCode="AR" term="%22Zhang%2C+B%2E%22">Zhang, B.</searchLink><br /><searchLink fieldCode="AR" term="%22Wiltberger%2C+M%2E%22">Wiltberger, M.</searchLink><br /><searchLink fieldCode="AR" term="%22Lyon%2C+J%2E%22">Lyon, J.</searchLink><br /><searchLink fieldCode="AR" term="%22Strangeway%2C+R%2E+J%2E%22">Strangeway, R. J.</searchLink>
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  Data: <searchLink fieldCode="JN" term="%22Science+%28pre-March+2025%29%22">Science (pre-March 2025)</searchLink>. 6/3/2011, Vol. 332 Issue 6034, p1183-1186. 4p.
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  Data: <searchLink fieldCode="DE" term="%22Magnetosphere%22">Magnetosphere</searchLink><br /><searchLink fieldCode="DE" term="%22Magnetospheric+physics%22">Magnetospheric physics</searchLink><br /><searchLink fieldCode="DE" term="%22Oscillations%22">Oscillations</searchLink><br /><searchLink fieldCode="DE" term="%22Ionospheric+research%22">Ionospheric research</searchLink><br /><searchLink fieldCode="DE" term="%22Solar+wind%22">Solar wind</searchLink><br /><searchLink fieldCode="DE" term="%22Magnetic+fields%22">Magnetic fields</searchLink><br /><searchLink fieldCode="DE" term="%22Convection+%28Astrophysics%29%22">Convection (Astrophysics)</searchLink>
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  Data: 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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  Data: <i>Copyright of Science (pre-March 2025) is the property of American Association for the Advancement of Science and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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        Value: 10.1126/science.1202869
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      – Code: eng
        Text: English
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        PageCount: 4
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      – SubjectFull: Magnetosphere
        Type: general
      – SubjectFull: Magnetospheric physics
        Type: general
      – SubjectFull: Oscillations
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      – SubjectFull: Ionospheric research
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      – SubjectFull: Solar wind
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      – SubjectFull: Magnetic fields
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      – SubjectFull: Convection (Astrophysics)
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              Text: 6/3/2011
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