Physics
Scientific paper
May 1991
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991jgr....96.7779m&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 96, May 1, 1991, p. 7779-7791. DOE-sponsored research.
Physics
41
Computerized Simulation, Planetary Ionospheres, Solar Planetary Interactions, Solar Wind, Venus Atmosphere, Ionopause, Planetary Magnetic Fields, Three Dimensional Models
Scientific paper
A three-dimensional global hybrid simulation of the interaction of the solar wind with the entire dayside of Venus is presented. The model obstacle is half the size of Venus, and planetary ion mass loading is included self-consistently. Results are compared to observations as well as to results from gasdynamic convected field modeling. Magnetic field magnitudes and bulk flow speeds along the planet-sun line are comparable in both models, but only the hybrid model reproduces the experimentally observed magnetic barrier proton density depletions. The finite gyroradius of the planetary pickup ions causes a number density asymmetry in the direction of the convective (-V x B) electric field, as predicted and observed. Mass addition consistent with photoionization of the planetary neutral hot oxygen corona has little effect on the geometry of the shock, including the subsolar and terminator shock altitudes. Mass addition rates well in excess of likely values are required to significantly affect the model shock geometry. The hybrid model results imply that oxygen ions originating deep within the dayside Venus magnetic barrier are nearly fluidlike, while oxygen ions produced higher on the dayside, at much lower densities, behave more as test particles.
McComas David John
Moore Kurt R.
Thomas Anne V.
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