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I use the rotation between each pair of consecutive postmainshock time periods to characterize the postseismic rotation.
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In the implementation of the edge-map based method, note that phase correlation [ 26] was used to determine the rotation between images rather than using the cross correlation recommended in the original paper due to the fact that phase correlation can generate the same results as cross correlation but is more robust than cross correlation with respect to partial occlusion [ 27].
As stated above, the rotor can be used to realize the rotation between the two coordinate systems.
For interpretation, principal components were rotated using the varimax rotation method, an orthogonal rotation procedure.
Due to the large angle between the magnetic moment and the rotation axis for Uranus and Neptune we use the average field between the poles and the equator.
The solution was rotated using the varimax rotation.
Factors were rotated using the oblique rotation method (promax).
Using the factor rotation technique, the varimax rotated component matrix [ 18] revealed that after rotation, thirty items loaded strongly (>0.40) (Table 6) on one of the four components, indicating a strong correlation between the item and the corresponding components.
Eight analyses were conducted; four using the Geomin rotation and four using the Oblimin rotation.
The correlation between factors was low (r = 0.06), suggesting a Varimax rotation would be more suitable, but the results of this rotation did not differ from the loading pattern obtained using the oblique rotation.
Independent factors were obtained using the Varimax rotation method.
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