The coherent shifts in inclinations among the Okhotsk Sea, western equatorial Pacific, and North Atlantic may also be explained by hypothetical dipole wobbles.
As the apex dentis takes its final position as early as the age of 7 years [ 22], the inclination shift is possibly related to the caudal displacement of the lower frontal point of the axis (C2a) that falls exactly on the reference line used for the projection assessment of the apex dentis.
All its members could muster was a shift from an inclination to raise rates to a neutral monetary policy stance.
Postoperative 3D evaluation revealed improved positioning parameters for most patients in dorsopalmar tilt, axial rotation (pronation and supination), radial inclination, proximodistal shift and volodorsal shift.
However, the correspondence of the inclination shifts to paleointensity lows prefers the SCOR field model.
We show that synchronous inclination shifts occur in the Okhotsk Sea and western equatorial Pacific and that the inclination variations may correlate with paleointensity.
These are synchronous to inclination shifts toward negative reported in the western equatorial Pacific and coincide in general with paleointensity lows.
These are synchronous with inclination shifts toward negative previously reported in the western equatorial Pacific, and temporally coincide with paleointensity lows in general.
Thus, the observed inclination shifts around excursions, shallower in the Okhotsk Sea and deeper toward negative in the western equatorial Pacific, may be explained by a larger contribution of the SCOR field when the GAD was weak.
These inclination shifts are synchronous with relative paleointensity lows in general (Fig. 5), as pointed out in the West Caroline Basin by Yamazaki and Oda (2002) and Yamazaki et al. (2008), although a period of paleointensity low around 100 ka contradictorily has steeper, but not shallower, inclinations in the Okhotsk Sea.
