Calculation of stable normal modes, on the other hand, would require analytic continuation of M(ω) into the lower half-plane, Im(s) ≤ 0, by deformation of the contour in velocity space, or perhaps by numerical analytic continuation. The numerical implementation of the eigenvalue solver, ...
3.2. Error Coefficient Calculation The geomagnetic field is stable. It can hardly change within days and is assumed to be constant in the calibration process. The geomagnetic field component perpendicular to the table is denoted as h ⊥ . When side 1 faces upwards, m ~ z 1 is equal to h...