Fig. 14From: On the detectability of the magnetic fields induced by ocean circulation in geomagnetic satellite observationsComparison of the selected (nighttime and geomagnetic low activity) vector field magnetic satellite measurements. The residuals from the core and lithosphere component are shown. The artificial data used in the presented OSSE are marked in red; the real Swarm observational data are marked in black. All three vector field components (\(B_r\), \(B_\theta\), \(B_\phi\)) are shown for each 100th satellite measurement of year 2014 in dependence on the satellite latitude positionBack to article page