Properties of Magnetic Reconnection and FTEs on the Dayside Magnetopause With and Without Positive IMF Bx Component During Southward IMF

Research output: Contribution to journalArticleScientificpeer-review

Researchers

  • Sanni Hoilijoki
  • Urs Ganse
  • David G. Sibeck
  • Paul A. Cassak
  • Lucile Turc
  • Markus Battarbee
  • Robert C. Fear
  • Xochitl Blanco-Cano
  • Andrew Dimmock
  • Emilia K.J. Kilpua
  • Riku Järvinen

  • Liisa Juusola
  • Yann Pfau-Kempf
  • Minna Palmroth

Research units

  • University of Helsinki
  • University of Colorado Boulder
  • NASA Goddard Space Flight Center
  • West Virginia University
  • University of Southampton
  • Universidad Nacional Autonoma de Mexico
  • Finnish Meteorological Institute
  • Swedish Institute of Space Physics

Abstract

This paper describes properties and behavior of magnetic reconnection and flux transfer events (FTEs) on the dayside magnetopause using the global hybrid-Vlasov code Vlasiator. We investigate two simulation runs with and without a sunward (positive) B x component of the interplanetary magnetic field (IMF) when the IMF is southward. The runs are two-dimensional in real space in the noon-midnight meridional (polar) plane and three-dimensional in velocity space. Solar wind input parameters are identical in the two simulations with the exception that the IMF is purely southward in one but tilted 45° toward the Sun in the other. In the purely southward case (i.e., without B x) the magnitude of the magnetosheath magnetic field component tangential to the magnetopause is larger than in the run with a sunward tilt. This is because the shock normal is perpendicular to the IMF at the equatorial plane, whereas in the other run the shock configuration is oblique and a smaller fraction of the total IMF strength is compressed at the shock crossing. Hence, the measured average and maximum reconnection rate are larger in the purely southward run. The run with tilted IMF also exhibits a north-south asymmetry in the tangential magnetic field caused by the different angle between the IMF and the bow shock normal north and south of the equator. Greater north-south asymmetries are seen in the FTE occurrence rate, size, and velocity as well; FTEs moving toward the Southern Hemisphere are larger in size and observed less frequently than FTEs in the Northern Hemisphere.

Details

Original languageEnglish
Pages (from-to)4037-4048
JournalJournal of geophysical research: Space physics
Volume124
Issue number6
Publication statusPublished - Jun 2019
MoE publication typeA1 Journal article-refereed

    Research areas

  • flux transfer event, hybrid-Vlasov, magnetic reconnection, magnetopause, numerical modeling

ID: 35591983