Fig. 2From: Sunlight effects on the 3D polar current system determined from low Earth orbit measurementsAMPERE and SuperMAG currents. AMPERE (left) radial currents and SuperMAG (right) equivalent currents in the Northern hemisphere for periods when IMF \(B_z < -2\) nT. The format and scales are the same as in Fig. 1, except that AMPERE uses altitude-adjusted corrected geomagnetic (AACGM) coordinates, which is very similar to modified apex coordinates at high latitudes (e.g., Laundal and Gjerloev 2014)Back to article page