Physics
Scientific paper
Oct 1979
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979ge%26ae..19..865k&link_type=abstract
Geomagnetizm i Aeronomiia, vol. 19, Sept.-Oct. 1979, p. 865-870. In Russian.
Physics
Atmospheric Boundary Layer, Earth Magnetosphere, Equatorial Atmosphere, Solar Wind Velocity, Boundary Value Problems, Daytime, Geomagnetism, Magnetohydrodynamic Flow, Solar Magnetic Field, Unsteady Flow
Scientific paper
The successive-approximation method is used to solve a time-dependent system of equations for the magnetic boundary layer that occurs at the outer boundary of the dayside magnetosphere. The solar-wind plasma dynamics is investigated, along with the magnetic- and electric-field distributions with the magnetopause. A wedge-shaped abstraction of the frontal point of the magnetosphere is employed for this purpose. The results obtained indicate that the thickness of the magnetopause decreases, and the electric-field strength within the magnetopause increases nearly linearly, as solar-wind speed increases.
Kereselidze Z. A.
Kiriia D. K.
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