Computer Science
Scientific paper
May 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993p%26ss...41..395m&link_type=abstract
Planetary and Space Science (ISSN 0032-0633), vol. 41, no. 5, p. 395-399.
Computer Science
4
Boundary Layer Plasmas, Gas Dynamics, Solar Terrestrial Interactions, Solar Wind, Two Dimensional Models, Venus Atmosphere, Pioneer Venus Spacecraft, Planetary Ionospheres, Venus, Gasdynamics, Simulation, Model, Solar Wind, Interaction, Flow, Boundaries, Origin, Formation, Dayside, Ionopause, Mass Loading, Ions, Pickup, Oxygen, Thickness, Layers, Parameters, Temperature, Density, Mass, Velocity, Comparison, Numerical Methods, Production Rate, Calculations, Magnetosheath, Magnetosphere, Photoionization
Scientific paper
A 2D gasdynamic simulation of the mass-loaded solar wind flow around the dayside of Venus is presented. For average ionopause conditions near 300 km, the simulations show that mass loading from the pickup of oxygen ions produces a boundary layer of finite thickness along the ionopause. Within this layer and toward the ionopause, the temperature decreases and the total mass density increases significantly. Furthermore, there is a shear in the bulk flow velocity across the boundary layer, such that the tangential flow decreases in speed as the ionopause is approached and remains low along the ionopause which is consistent with Pioneer Venus observations. Numerical simulations are carried out for various mass addition rates and demonstrate that the boundary layer develops when oxygen ion production exceeds approximately 2 x 10 exp 5/cu m per s.
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