From initial Pioneer Venus observations during the maximum of solar cycle 21 it was evident that the position of the Venus bow shock varies with solar activity. The bow shock radius in the terminator plane changed from 2.4 Rv to 2.1 Rv as solar activity went from maximum to minimum and, as activity has increased in cycle 22, it has increased again. Our recent studies of the subsolar region show that the altitude of the nose of the bow shock varies from 1600 km at solar minimum to 2200 km at intermediate solar activity in concert with the terminator altitude so that the shape remains constant and only the size varies during the solar cycle. Using a gas dynamic model and the observed bow shock location, we infer the variation in the size of the effective observable during the solar cycle. At solar maximum, the effective obstacle is larger than the ionopause as if a ''magnetic barrier'' exists in the inner magnetosheath. This magnetic barrier acts as the effective obstable deflecting the magnetosheath plasma about 500 km above the surface of Venus. However, at solar minimum the effective obstacle is well below the subsolar ionopause, and some absorption of the solar wind plasma by the Venus neutral atmosphere is suggested by these observations. The dependence of the solar cylce variation of the shock position on the orientation of the interplanetary magnetic field reinforces the idea that planetary ion pickup is important in the interaction of the solar wind with Venus. ¿ American Geophysical Union 1990