Two possible consequences of magnetic merging are studied: first, the presence of ionospheric-magnetospheric currents in the outer magnetosphere, as consequence of magnetospheric convection; second, the presence of magnetosheath-like plasma, possibly penetrating through the magnetopause. The field aligned currents were studied through the effect they have on the field direction projected in the
... [Show full abstract] equatorial plane. In 25% of the magnetopause crossings the magnetospheric lines of force show an anomalous distortion (sunward instead of tailward of the meridian planes) related, most likely, to the field aligned currents. This anomalous distortion is preferentially present at middle latitudes in the day side region. Another important feature of the outer magnetosphere was found in the magnetic field intensity as an abrupt increase of B (going earthward it appears as an abrupt decrease) usually located 1 to 2 earth radii from the magnetopause. This feature was observed 40% of the time at any latitude or local time. Magnetospheric plasma was observed in at least 8 magnetopause crossings. Bulk speed and density appear to be lower in the magnetosphere, the temperature being higher there than in the magnetosheath.