Physics
Scientific paper
Sep 1986
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986jgr....9110029o&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 91, Sept. 1, 1986, p. 10029-10045.
Physics
56
Earth Magnetosphere, Interplanetary Magnetic Fields, Solar Terrestrial Interactions, Solar Wind, Space Environment Simulation, Cross Sections, Field Aligned Currents, Lines Of Force, Magnetic Field Configurations, Plasma Layers, Three Dimensional Models, Vorticity
Scientific paper
The interaction between the solar wind and the earth's magnetosphere has been studied by using a time-dependent three-dimensional MHD model in which the IMF pointed in several directions between dawnward and southward. When the IMF is dawnward, the dayside cusp and the tail lobes shift toward the morningside in the northern magnetosphere. The plasma sheet rotates toward the north on the dawnside of the tail and toward the south on the duskside. For an increasing southward IMF component, the plasma sheet becomes thinner and subsequently wavy because of patchy or localized tail reconnection. At the same time, the tail field-aligned currents have a filamentary layered structure. When projected onto the northern polar cap, the filamentary field-aligned currents are located in the same area as the region 1 currents, with a pattern similar to that associated with auroral surges. Magnetic reconnection also occurs on the dayside magnetopause for southward IMF.
Ashour-Abdalla Maha
Dawson John M.
Ogino Takeshi
Walker Ray J.
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