Observations of Asymmetries in Ionospheric Return Flow During Different Levels of Geomagnetic Activity

It is known that the magnetic field of the Earth's closed magnetosphere can be highly displaced from the quiet‐day configuration when interacting with the interplanetary magnetic field (IMF), an asymmetry largely controlled by the dawn‐dusk component of the IMF. The corresponding ionospheric co...

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Bibliographic Details
Published in:Journal of Geophysical Research: Space Physics
Main Authors: Reistad, JP, Ostgaard, N, Laundal, KM, Ohma, A, Snekvik, K, Tenfjord, P, Grocott, A, Oksavik, K, Milan, SE, Haaland, S
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU), Wiley 2019
Subjects:
Science & Technology
Physical Sciences
Astronomy & Astrophysics
IMF B-Y
HIGH-LATITUDE CONVECTION
NON-SUBSTORM INTERVALS
MAGNETIC-FIELD
COMPONENT
MAGNETOTAIL
MAGNETOSPHERE
PLASMA
WIND
RECONNECTION
Arctic
Canada
Norway
Omni
Online Access:https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2017JA025051
http://hdl.handle.net/2381/44976
https://doi.org/10.1029/2017JA025051

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