We describe the "magnetic string" approach to integrating the dissipationle
ss magnetohydrodynamic (MHD) equations for flow around planetary obstacles
and apply it to some aspects of the flow in the magnetosheath of Venus. Our
method has both analytical and numerical components and is particularly su
ited to study the structure of the magnetic barrier (depletion layer). We d
o not include ion pickup processes and thus discuss only the contribution t
o the structure of the Venus magnetosheath made by the flow of the shocked
solar wind. We work with an interplanetary magnetic field which is directed
orthogonal to the solar wind bulk velocity. Magnetic forces on the flow ar
e strongly dependent on the Alfven Mach number upstream of the bow shock, a
nd one aim of this work is to study the dependence of field and flow quanti
ties in the Venus magnetosheath on this parameter, thus allowing further fu
ture comparisons with data under a variety of interplanetary conditions. A
second aim is to compare our MHD model results to a? synopsis of observatio
ns made by the Pioneer Venus Orbiter. As one main conclusion, we show that
this method leads, in principle, to a standoff bow shock position in good a
greement with observations. We find, namely, that for a low but reasonable
Alfven Mach number, our MHD-modeled magnetosheath is only similar to 3.6% t
hinner in the Sun-Venus direction than that given by observations. Our meth
od is complementary to three-dimensional, global MHD simulations of the sol
ar wind-Venus interaction and offers versatility to modeling other aspects
of the complicated interaction of the solar wind with Venus.