A numerical study of solar wind—magnetosphere interaction for northward interplanetary magnetic field

The solar wind-magnetosphere interaction for northward interplanetary magnetic field (IMF) is studied using a newly developed three-dimensional adaptive mesh refinement (AMR) global MHD simulation model. The simulations show that for north-ward IMF the magnetosphere is essentially closed. Reconnection between the IMF and magnetospheric field is limited to finite regions near the cusps. When the reconnection process forms newly closed magnetic field lines on the day side, the solar wind plasma trapped on these reconnected magnetic field lines becomes part of the low-latitude boundary layer (LLBL) plasma and it convects to the nightside along the magnetopause. The last closed magnetic field line marks the topological boundary of the magnetospheric domain. When the last closed magnetic field line disconnects at the cusps and reconnects to the IMF, its plasma content becomes part of the solar wind. Plasma convection in the outer magnetosphere does not directly contribute to the reconnection process. On the dayside the topological boundary between the solar wind and the magnetosphere is located at the inner edge of the magnetopause current layer. At the same time, multiple current layers are observed in the high-altitude cusp region. Our convergence study and diagnostic analysis indicate that the details of the diffusion and the viscous interaction do not play a significant role in controlling the large-scale configuration of the simulated magnetosphere. It is sufficient that these dissipation mechanisms exist in the simulations. In our series of simulations the length of the magnetotail is primarily determined by the balance between the boundary layer driving forces and the drag forces. With a parametric study, we find that the tail length is proportional to the magnetosheath plasma beta near the magnetopause at local noon. A higher solar wind density, weaker IMF, and larger solar wind Mach number results in a longer tail. On the nightside downstream of the last closed magnetic field line the plasma characteristics are similar to that in the magnetotail, posing an observational challenge for identification of the topological status of the corresponding field lines.

[1]  M. Kivelson,et al.  Dynamical polar cap: A unifying approach , 1997 .

[2]  Christopher T. Russell,et al.  Initial ISEE magnetometer results - Magnetopause observations , 1978 .

[3]  C. Clauer,et al.  High‐latitude dayside electric fields and currents during strong northward interplanetary magnetic field: Observations and model simulation , 1988 .

[4]  Joachim Raeder,et al.  The structure of the distant geomagnetic tail during long periods of northward IMF , 1995 .

[5]  G. Paschmann,et al.  ISEE plasma observations near the subsolar magnetopause , 1978 .

[6]  C. Russell,et al.  Model of the formation of the low-latitude boundary layer for strongly northward interplanetary magnetic field , 1992 .

[7]  Kenneth G. Powell,et al.  Three‐dimensional multiscale MHD model of cometary plasma environments , 1996 .

[8]  M. L. Goodman,et al.  Comment on : A three-dimensional, iterative mapping procedure for the implementation of an ionosphere-magnetosphere anisotropic Ohm's law boundary condition in global magnetohydrodynamic simulations. Author's reply , 1996 .

[9]  Kenneth G. Powell,et al.  AN APPROXIMATE RIEMANN SOLVER FOR MAGNETOHYDRODYNAMICS (That Works in More than One Dimension) , 1994 .

[10]  Philip L. Roe,et al.  An upwind scheme for magnetohydrodynamics , 1995 .

[11]  K. Powell,et al.  A model of solar wind–magnetosphere–ionosphere coupling for due northward IMF , 2000 .

[12]  R. Walker,et al.  A magnetohydrodynamic simulation of the bifurcation of tail lobes during intervals with a northward interplanetary magnetic field , 1984 .

[13]  J. Choe,et al.  The Magnetospheric Boundary , 1974 .

[14]  C. T. Russell,et al.  Initial ISEE magnetometer results: magnetopause observations , 1978 .

[15]  L. Zanetti,et al.  Large-scale Birkeland currents in the dayside polar region during strongly northward IMF: A new Birkeland current system , 1984 .

[16]  Wolfgang Baumjohann,et al.  Ionospheric and Birkeland current distributions for northward interplanetary magnetic field: Inferred polar convection , 1984 .

[17]  Michael L. Goodman,et al.  A three-dimensional, iterative mapping procedure for the implementation of an ionosphere-magnetosphere anisotropic Ohm’s law boundary condition in global magnetohydrodynamic simulations , 1995 .

[18]  P. Roe Approximate Riemann Solvers, Parameter Vectors, and Difference Schemes , 1997 .

[19]  L. Mcginnis,et al.  Regional free air gravity anomalies and tectonic observations in the United States , 1979 .

[20]  T. Sanderson,et al.  Low-latitude dusk flank magnetosheath, magnetopause, and boundary layer for low magnetic shear: Wind observations , 1997 .

[21]  W. J. Burke,et al.  Polar cap electric field structures with a northward interplanetary magnetic field , 1979 .

[22]  T. Linde,et al.  A three-dimensional adaptive multifluid MHD model of the heliosphere. , 1998 .

[23]  B. Sonnerup Transport Mechanisms at the Magnetopause , 1980 .

[24]  G. Paschmann,et al.  ISEE plasma observations near the subsolar magnetopause , 1978 .

[25]  A. Nishida,et al.  Pattern of electron and ion precipitation in northern and southern polar regions for northward interplanetary magnetic field conditions , 1992 .

[26]  N. A. Saflekos,et al.  The quiet time polar cap: DE 1 observations and conceptual model , 1992 .

[27]  C. Kennel,et al.  Can the ionosphere regulate magnetospheric convection , 1973 .

[28]  Christopher T. Russell,et al.  The thickness of the magnetosheath: Constraints on the polytropic index , 1991 .

[29]  T. Hill,et al.  Mapping of the solar wind electric field to the Earth's polar caps , 1989 .

[30]  R. Hoffman,et al.  Control parameters for polar ionospheric convection patterns during northward interplanetary magnetic field , 1996 .

[31]  R. Lepping,et al.  Geotail Observations of an Unusual Magnetotail under Very Northward IMF Conditions , 1996 .

[32]  D. Fairfield Solar wind control of the distant magnetotail: ISEE 3 , 1993 .

[33]  E. W. Hones,et al.  Possible conjugate reconnection at the high-latitude magnetopause , 1995 .

[34]  B. Sonnerup Theory of the low-latitude boundary layer , 1980 .

[35]  C. Russell,et al.  Structure and properties of the subsolar magnetopause for northward interplanetary magnetic field - Multiple-instrument particle observations , 1993 .

[36]  R. Spiro,et al.  Generation of region 1 current by magnetospheric pressure gradients , 1994 .

[37]  W. J. Burke,et al.  A theoretical model of polar cap auroral arcs , 1985 .

[38]  P. Roe,et al.  A Solution-Adaptive Upwind Scheme for Ideal Magnetohydrodynamics , 1999 .

[39]  C. Mobarry,et al.  Equatorial plasma convection from global simulations of the Earth's magnetosphere , 1996 .

[40]  C. Wu The effects of northward IMF on the structure of the magnetosphere , 1985 .

[41]  Akira Kageyama,et al.  A global simulation of the magnetosphere with a long tail: Southward and northward interplanetary magnetic field , 1993 .

[42]  J. L. Green,et al.  Evidence of high‐latitude reconnecting during northward IMF: Hawkeye observations , 1996 .

[43]  C. Russell,et al.  Modelling the low‐latitude boundary layer with reconnection entry , 1994 .

[44]  P. Reiff,et al.  IMF By-dependent plasma flow and Birkeland currents in the dayside magnetosphere: 2. A global model for northward and southward IMF , 1985 .

[45]  Harry E. Petschek,et al.  Magnetic Field Annihilation , 1963 .

[46]  J. Dungey Interplanetary Magnetic Field and the Auroral Zones , 1961 .

[47]  Nancy U. Crooker,et al.  Dayside merging and cusp geometry , 1979 .

[48]  M. Kivelson,et al.  Anomalous aspects of magnetosheath flow and of the shape and oscillations of the magnetopause during an interval of strongly northward interplanetary magnetic field , 1993 .

[49]  Hideaki Kawano,et al.  Magnetopause location under extreme solar wind conditions , 1998 .

[50]  J. Lyon,et al.  The Earth's magnetosphere is 165 RE long: Self‐consistent currents, convection, magnetospheric structure, and processes for northward interplanetary magnetic field , 1995 .

[51]  C. Russell,et al.  Statistical characteristics of bursty bulk flow events , 1994 .

[52]  Christopher T. Russell,et al.  The Configuration of the Magnetosphere , 1972 .