The structure of the dayside boundary layer between the Venus ionosphere and the shocked solar wind

Physics

Scientific paper

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Atmospheric Models, Magnetosheath, Particle Interactions, Planetary Boundary Layer, Planetary Ionospheres, Beam Interactions, Solar Wind, Venus Atmosphere

Scientific paper

A physical mechanism that may explain the observations at the boundary layer between the magnetosheath and the dayside ionosphere of nonmagnetic planets was investigated. The mechanism is based on a beam particle type interaction between the shocked solar wind and cold planetary ions. Some of the consequences of these interaction processes were established using Pioneer-Venus Orbiter and Phobos-2 observations. However, the identification of the accelerated electrons in the case of Venus eluded detection.

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