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Mass-loading and the formation of the Venus tail
Authors:CT Russell  MA Saunders  JG Luhmann
Institution:1. Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90024, U.S.A.;2. Blackett Laboratory, Imperial College, London SW7 2BZ, England
Abstract:Despite its lack of an intrinsic magnetic field Venus has a well defined magnetotail, containing about 3 megawebers of magnetic flux in a tail about 4 RV across with perhaps a slightly elliptical cross section. This tail arises through the mass-loading of magnetic flux tubes passing by the planet. Mass-loading can occur due to charge exchange and photo-ionization as well as from the diffusion of magnetic field into the ionosphere. Various evidence exists for the mass-loading process, including the direct observation of the picked up ions with both the Venera and Pioneer Venus plasma analyzers.
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