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Figure 13a illustrates directional change of the HTC1s with time as the reversal angle (Valet et al. 2012) which denotes the angle between the local magnetic vector and the GAD-expected direction at the GSDS site (D = 0°, I = 53°).
a The GSDS1-AF-derived HFC and the GSDS2-TH-derived HTC1 directional changes, expressed as the reversal angle (the angle between the paleomagnetic direction and the direction of today's axial dipole field at the GSDS site) through time with our inferred age-depth model.
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Only one bank angle reversal is needed for a no-fly zone or waypoint, so the reversal times are few.
For each reference point, one bank angle reversal is designed.
During this kind of reversal the tilt angle grows and the magnetospheric configuration passes the pole-on configuration.
Moreover, as no reversal of bank angle exists in the whole flight, the control command is easier to follow.
Because the orientations were sampled in 1°-steps, the number of reversals represents the angle between the 2 tonotopic gradients adjoining at a given edge location.
Since the children in our study showed valgus angulation, the reversal of knee angles from physiological varus to valgus occurs before two years of age and therefore outside the boundaries of this study.
In addition, the lateral error is removed by regulating the reversal time of bank angle.
However, both polar angle retinotopy (reversal at an upper visual field vertical meridian) and the posterior bound of ipsilateral responses were situated near the middle of the oval.
However, complex reversal modes appear when the angle at which the external field is applied is varied, leading to a non-monotonic behavior of the coercivity and remanence.
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