Magnetosheath

The regularly organized magnetic field generated by the planet becomes weak and irregular in the magnetosheath due to interaction with the incoming solar wind, and is incapable of fully deflecting the highly charged particles.

The density of the particles in this region is considerably lower than what is found beyond the bow shock, but greater than within the magnetopause, and can be considered a transitory state.

[1][2] Scientific research into the exact nature of the magnetosheath has been limited due to a longstanding misconception that it was a byproduct of the bow shock/magnetopause interaction and had no inherently important properties of its own.

Recent studies indicate, however, that the magnetosheath is a dynamic region of turbulent plasma flow which may play an important role in the structure of the bow shock and the magnetopause, and might help to dictate the flow of energetic particles across those boundaries.

[5] The Earth's magnetosheath typically occupies the region of space approximately 10 Earth radii on the upwind (Sun-facing) side of the planet, extending significantly further out on the downwind side due to the pressure of the solar wind.