A similar effect, known as the magnetic draping effect, occurs when a super-Alfvénic plasma flow impacts an unmagnetized object such as what happens when the solar wind reaches the ionosphere of Venus: the flow deflects around the object draping the
magnetic field along the wake flow. The condition for the flow to be super-Alfvénic means that the relative velocity between the flow and object, v, is larger than the local
Alfvén velocity V_A which means a large
Alfvénic Mach number: M_A \gg 1. For unmagnetized and
electrically conductive objects, the ambient field creates
electric currents inside the object, and into the surrounding plasma, such that the flow is deflected and slowed as the time scale of magnetic
dissipation is much longer than the time scale of magnetic field
advection. The induced currents in turn generate magnetic fields that deflect the flow creating a bow shock. For example, the
ionospheres of Mars and Venus provide the conductive environments for the interaction with the solar wind. Without an ionosphere, the flowing magnetized plasma is absorbed by the non-conductive body. The latter occurs, for example, when the solar wind interacts with the
Moon which has no ionosphere. In magnetic draping, the field lines are wrapped and draped around the leading side of the object creating a narrow sheath which is similar to the bow shocks in the planetary magnetospheres. The concentrated magnetic field increases until the
ram pressure becomes comparable to the
magnetic pressure in the sheath: :\rho_0 v^2 = \frac{B_0^2}{2\mu_0}, where \rho_0 is the density of the plasma, B_0 is the draped magnetic field near the object, and v is the relative speed between the plasma and the object. Magnetic draping has been detected around planets, moons, solar coronal mass ejections, and galaxies. ==See also==