Relative Timing of Nightside and Dayside Plasmapause Motion: Two Events in June 2001
Affiliation
Univ Arizona, Lunar & Planetary LabIssue Date
2019-12-22
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AMER GEOPHYSICAL UNIONCitation
Goldstein, J., & Sandel, B. R. (2020). Relative timing of nightside and dayside plasmapause motion: Two events in June 2001. Journal of Geophysical Research: Space Physics, 125(1), e2019JA027153.Rights
© 2019. American Geophysical Union. All Rights Reserved.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
We examine the relative timing of dayside and nightside plasmapause motion following southward interplanetary magnetic field turnings on 2 and 9 June 2001. For both events the delay between the dayside and nightside plasmapause response is less than the temporal resolution of Imager for Magnetopause-to-Aurora Global Exploration extreme ultraviolet observations (10 min). Our result thus establishes a possible upper limit (<= 10 min) on the day-to-night onset delay. From analysis of the extreme ultraviolet-observed plasmapause motion we find on 2 June the time-averaged plasmapause E field was (in mV/m) 0.61 near noon magnetic local time, 0.35 near midnight magnetic local time, and 0.44 overall. The normalized plasmapause speed data (both dayside and nightside) are fitted to the curve (0.09 +/- 0.05)L-3, consistent with a spatially uniform and time-constant dawn-dusk penetration E field that is 9% of the solar wind field. On 9 June the time-averaged E field values (mV/m) were 0.24 (dayside), 0.28 (nightside), and 0.26 (overall); the plasmapause motion was consistent with a penetration E field 10% of the solar wind field. Plasmasphere erosion is a fundamental element of the dynamic magnetospheric response to solar wind driving. This study yields an important observational constraint on the day-to-night timing of the plasmapause response. The result also has implications for the two main models for the cause of erosion (convection and interchange).Note
6 month embargo; first published online 22 December 2019ISSN
2169-9380EISSN
2169-9402Version
Final published versionSponsors
National Aeronautics and Space Administrationae974a485f413a2113503eed53cd6c53
10.1029/2019ja027153