2000
DOI: 10.1109/27.902224
|View full text |Cite
|
Sign up to set email alerts
|

An adaptive MHD method for global space weather simulations

Abstract: A 3-D parallel adaptive mesh refinement (AMR) scheme is described for solving the partial-differential equations governing ideal magnetohydrodynamic (MHD) flows. This new algorithm adopts a cell-centered upwind finite-volume discretization procedure and uses limited solution reconstruction, approximate Riemann solvers, and explicit multi-stage time stepping to solve the MHD equations in divergence form, providing a combination of high solution accuracy and computational robustness across a large range in the p… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

1
83
0

Year Published

2000
2000
2017
2017

Publication Types

Select...
9

Relationship

1
8

Authors

Journals

citations
Cited by 91 publications
(84 citation statements)
references
References 57 publications
1
83
0
Order By: Relevance
“…The model inputs are the solar wind driven outputs of the global MHD modeling provided in near real time by the Space Weather Modeling Framework (Tóth et al 2005(Tóth et al , 2012. 3D magnetic fields, as well as equatorial plasma density and temperature are obtained from the global magnetosphere SWMF GM/BATSRUS model (Powell et al 1999;De Zeeuw et al 2000) and 2D ionospheric height-integrated potentials are given by the ionospheric electrodynamics SWMF IE/RIM model (Ridley et al 2001. Equatorial plasma density and temperature are used to set the boundary conditions in the plasma sheet for electrons, which move inward in the provided magnetic and computed from the ionospheric potentials electric fields.…”
Section: Ring Current Electrons and Effects On Satellitesmentioning
confidence: 99%
“…The model inputs are the solar wind driven outputs of the global MHD modeling provided in near real time by the Space Weather Modeling Framework (Tóth et al 2005(Tóth et al , 2012. 3D magnetic fields, as well as equatorial plasma density and temperature are obtained from the global magnetosphere SWMF GM/BATSRUS model (Powell et al 1999;De Zeeuw et al 2000) and 2D ionospheric height-integrated potentials are given by the ionospheric electrodynamics SWMF IE/RIM model (Ridley et al 2001. Equatorial plasma density and temperature are used to set the boundary conditions in the plasma sheet for electrons, which move inward in the provided magnetic and computed from the ionospheric potentials electric fields.…”
Section: Ring Current Electrons and Effects On Satellitesmentioning
confidence: 99%
“…[11] Simulations of the solar wind -driven magnetosphere-ionosphere system are run at the Community Coordinated Modeling Center (CCMC) [Bellaire, 2004] at NASA/Goddard Space Flight Center using the Block-Adaptive-Tree Solarwind Roe Upwind Scheme (BATSRUS) 3-D MHD code [Powell et al, 1999;De Zeeuw et al, 2000;Gombosi et al, 2000;Ridley et al, 2004;A. J. Ridley and G. Toth, unpublished data, 2008].…”
Section: Mhd Simulationsmentioning
confidence: 99%
“…This property is often preferred in applications where shocks are present as one can easily take advantage of special algorithms defined to deal with these issues (see e.g. [19,20,21,22,23]). …”
Section: Preliminariesmentioning
confidence: 99%