On the evolution of a magnetic flux rope: Two‐dimensional MHD simulation results. Issue 10 (24th October 2015)
- Record Type:
- Journal Article
- Title:
- On the evolution of a magnetic flux rope: Two‐dimensional MHD simulation results. Issue 10 (24th October 2015)
- Main Title:
- On the evolution of a magnetic flux rope: Two‐dimensional MHD simulation results
- Authors:
- Teh, W.‐L.
Nakamura, T. K. M.
Nakamura, R.
Baumjohann, W.
Abdullah, M. - Abstract:
- Abstract: We use the time‐dependent, two‐dimensional (2‐D), ideal MHD equations to simulate and investigate the evolution of magnetic field and plasma profiles of the typical (T) and crater (C) magnetic flux ropes (FRs). The T‐FR has a magnetic pressure peak at the center of the flux rope, while the C‐FR has a local dip instead. The simulation starts with a 2‐D magnetic flux rope in magnetohydrostatic equilibrium, where pressure gradient forces are balanced by Lorentz forces. The magnetic field and plasma pressure profiles for the initial flux rope are derived from the analytical solutions by Zhang et al. (2010). The initial flux rope starts to evolve when the force balance is broken by imposing pressure or magnetic field perturbations onto the equilibrium system. The pressure perturbations are produced by increasing/decreasing the internal plasma pressure of the flux rope, while the magnetic field perturbations are produced by increasing/decreasing the transverse magnetic fields across the flux rope. We conclude that a T‐FR can be evolved into a C‐FR and vice versa, if the perturbation strength is sufficient, and that the plasma pressure and density in the new equilibrium state could be either increased or decreased for the evolution of C‐FR to T‐FR and also for the evolution of T‐FR to C‐FR. Key Points: T‐FR can be evolved into C‐FR and vice versa Initial stage of both T‐FR and C‐FR can be either a T‐like or C‐like FR Pressure and density could be increased/decreasedAbstract: We use the time‐dependent, two‐dimensional (2‐D), ideal MHD equations to simulate and investigate the evolution of magnetic field and plasma profiles of the typical (T) and crater (C) magnetic flux ropes (FRs). The T‐FR has a magnetic pressure peak at the center of the flux rope, while the C‐FR has a local dip instead. The simulation starts with a 2‐D magnetic flux rope in magnetohydrostatic equilibrium, where pressure gradient forces are balanced by Lorentz forces. The magnetic field and plasma pressure profiles for the initial flux rope are derived from the analytical solutions by Zhang et al. (2010). The initial flux rope starts to evolve when the force balance is broken by imposing pressure or magnetic field perturbations onto the equilibrium system. The pressure perturbations are produced by increasing/decreasing the internal plasma pressure of the flux rope, while the magnetic field perturbations are produced by increasing/decreasing the transverse magnetic fields across the flux rope. We conclude that a T‐FR can be evolved into a C‐FR and vice versa, if the perturbation strength is sufficient, and that the plasma pressure and density in the new equilibrium state could be either increased or decreased for the evolution of C‐FR to T‐FR and also for the evolution of T‐FR to C‐FR. Key Points: T‐FR can be evolved into C‐FR and vice versa Initial stage of both T‐FR and C‐FR can be either a T‐like or C‐like FR Pressure and density could be increased/decreased during C‐to‐T and during T‐to‐C … (more)
- Is Part Of:
- Journal of geophysical research. Volume 120:Issue 10(2015:Oct.)
- Journal:
- Journal of geophysical research
- Issue:
- Volume 120:Issue 10(2015:Oct.)
- Issue Display:
- Volume 120, Issue 10 (2015)
- Year:
- 2015
- Volume:
- 120
- Issue:
- 10
- Issue Sort Value:
- 2015-0120-0010-0000
- Page Start:
- 8547
- Page End:
- 8558
- Publication Date:
- 2015-10-24
- Subjects:
- magnetic flux ropes -- magnetohydrodynamics
Magnetospheric physics -- Periodicals
Space environment -- Periodicals
Cosmic physics -- Periodicals
Planets -- Atmospheres -- Periodicals
Heliosphere (Astrophysics) -- Periodicals
Geophysics -- Periodicals
523.01 - Journal URLs:
- http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)2169-9402 ↗
http://onlinelibrary.wiley.com/ ↗ - DOI:
- 10.1002/2015JA021619 ↗
- Languages:
- English
- ISSNs:
- 2169-9380
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 4995.010000
British Library DSC - BLDSS-3PM
British Library HMNTS - ELD Digital store - Ingest File:
- 2221.xml