4.7 Article

THREE-DIMENSIONAL SOLAR WIND MODELING FROM THE SUN TO EARTH BY A SIP-CESE MHD MODEL WITH A SIX-COMPONENT GRID

Journal

ASTROPHYSICAL JOURNAL
Volume 723, Issue 1, Pages 300-319

Publisher

IOP PUBLISHING LTD
DOI: 10.1088/0004-637X/723/1/300

Keywords

magnetohydrodynamics (MHD); methods: numerical; solar wind; Sun: heliosphere

Funding

  1. National Natural Science Foundation of China [41031066, 40921063, 40874091, 40890162, 40904050, 40874077, 40536029]
  2. 973 project [2006CB806304]
  3. Specialized Research Fund for State Key Laboratories
  4. AFOSR [FA9550-07-1-0468]
  5. NSO [C10569A, AST 0132798]
  6. NSF [ATM-0754378]
  7. NASA

Ask authors/readers for more resources

The objective of this paper is to explore the application of a six-component overset grid to solar wind simulation with a three-dimensional (3D) Solar-InterPlanetary Conservation Element/Solution Element MHD model. The essential focus of our numerical model is devoted to dealing with: (1) the singularity and mesh convergence near the poles via the use of the six-component grid system, (2) the del . B constraint error via an easy-to-use cleaning procedure by a fast multigrid Poisson solver, (3) the Courant-Friedrichs-Levy number disparity via the Courant-number insensitive method, (4) the time integration by multiple time stepping, and (5) the time-dependent boundary condition at the subsonic region by limiting the mass flux escaping through the solar surface. In order to produce fast and slow plasma streams of the solar wind, we include the volumetric heating source terms and momentum addition by involving the topological effect of the magnetic field expansion factor f(S) and the minimum angular distance theta(b) (at the photosphere) between an open field foot point and its nearest coronal hole boundary. These considerations can help us easily code the existing program, conveniently carry out the parallel implementation, efficiently shorten the computation time, greatly enhance the accuracy of the numerical solution, and reasonably produce the structured solar wind. The numerical study for the 3D steady-state background solar wind during Carrington rotation 1911 from the Sun to Earth is chosen to show the above-mentioned merits. Our numerical results have demonstrated overall good agreements in the solar corona with the Large Angle and Spectrometric Coronagraph on board the Solar and Heliospheric Observatory satellite and at 1 AU with WIND observations.

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