Steady state slow shock inside the Earth's magnetosheath: To be or not to be? 2. Numerical three-dimensional MHD modeling

Details Steady state slow shock inside the Earth's magnetosheath: To be or not to be? 2. Numerical three-dimensional MHD modeling Steady state slow shock inside the Earth's magnetosheath: To be or not to be? 2. Numerical three-dimensional MHD modeling

Jan 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004jgra..10901218s&link_type=abstract

Journal of Geophysical Research, Volume 109, Issue A1, CiteID A01218

Physics

7

Magnetospheric Physics: Magnetosheath, Magnetospheric Physics: Numerical Modeling, Magnetospheric Physics: Solar Wind/Magnetosphere Interactions, Magnetospheric Physics: Mhd Waves And Instabilities

Scientific paper

Large-scale structures in the dayside terrestrial magnetosheath are studied in this paper. The question about existence of the steady state slow MHD shock in the inner magnetosheath is one of the principal theoretical and experimental problems which has not been solved yet. In part 1, the original observations have been revisited. In this part, the numerical results of the three-dimensional MHD model are presented and discussed. It is shown that for the given observations the density enhancement identified previously as a slow mode transition region is explained by temporal variations of the magnetic field and density observed in the supersonic solar wind. There are three factors resulting in the density increase in the slow mode transition region: A density increase in the upstreamflow, a decrease of the IMF modulus, and a new IMF orientation which forms a quasi-parallel bow shock in the subsolar region. We show that numerical solutions obtained by non-stationary and stationary MHD models are significantly different for the same solar wind conditions. We discuss how the magnetopause motion may enlarge the observed variations of the magnetosheath density. Also we answer the question why the existed numerical MHD models do not predict the slow shock in the steady state solution and show how the magnetosheath flow may be organized without such shock.

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