Skip to main content
Earth, Planets and Space
Fig. 10 | Earth, Planets and Space

Fig. 10

From: On the detectability of the magnetic fields induced by ocean circulation in geomagnetic satellite observations

Fig. 10

The assimilation results using various from the imposed field differing true OIMFs. The shown NRMSD expresses how well the rescaled OIMF anomalies reflects the true OIMF anomalies. The left side shows the result for spatial deviations using a true OIMF with SH resolution of degrees 45 and 60. On the right side, temporal deviations in the form of low-frequency (LF) and high-frequency (HF) noise are considered. Dark red indicates areas with large NRMSD and, therefore, a large discrepancy between rescaled and true OIMF; respectively, lighter colors point out areas of good agreement

Back to article page