How the IMF B y induces a B y component in the closed magnetosphere and how it leads to asymmetric currents and convection patterns in the two hemispheres-Reference-Cited by-同舟云学术

How the IMF B y induces a B y component in the closed magnetosphere and how it leads to asymmetric currents and convection patterns in the two hemispheres

Published:2015-11 Issue:11 Volume:120 Page:9368-9384
ISSN:2169-9380
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:J. Geophys. Res. Space Physics

Author:

Tenfjord P.¹,Østgaard N.¹,Snekvik K.¹,Laundal K. M.¹,Reistad J. P.¹,Haaland S.¹²,Milan S. E.¹³

Affiliation:

1. Birkeland Centre for Space Science, Department of Physics and Technology University of Bergen Bergen Norway

2. Max Planck Institute for Solar System Research Göttingen Germany

3. Department of Physics and Astronomy University of Leicester Leicester UK

Funder

Research Council of Norway/CoE

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA021579

Reference66 articles.

1. Sensing global Birkeland currents with iridium® engineering magnetometer data

2. Statistical Birkeland current distributions from magnetic field observations by the Iridium constellation

3. IMFBy-dependent plasma flow and Birkeland currents in the dayside magnetosphere: 1. Dynamics Explorer observations

4. Dependence of IMFBypenetration into the neutral sheet on IMFBzand geomagnetic activity

5. Magnetospheric asymmetries associated with the y-component of the IMF

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