Fig. 1From: The CHAOS-7 geomagnetic field model and observed changes in the South Atlantic AnomalyHistograms showing number of selected satellite data (combination of all the scalar, scalar gradient, vector and vector gradient data) distributed according to IMF \(B_z\) (top left), IMF \(B_y\) (top right) and the merging electric field at the magnetopause \(E_\text{m}\), as estimated by coupling function \(0.33 v^{4/3} B_t^{2/3} \sin ^{8/3} \left( | \Theta | / 2 \right) \) mV/m with v the solar wind speed in km/s, \(B_t=\sqrt{B_y^2 + B_z^2}\) the Interplanetary Magnetic Field magnitude in the \(y-z\) plane in GSM coordinates in nT, and \(\Theta = \arctan (B_y/B_z)\). IMF and Em values are averages of 1-min values for 2 h prior to the time of the observation. y-axis shows the number of observations per binBack to article page