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Calibration of a Terrestrial Laser Scanner - Institute of Geodesy and ...

Calibration of a Terrestrial Laser Scanner - Institute of Geodesy and ...

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56 3. <strong>Calibration</strong> <strong>of</strong> <strong>Terrestrial</strong> <strong>Laser</strong> <strong>Scanner</strong>X-Direction0 100 200 300 400 500 600 700 800 900azimuth [°]Y-Direction0 100 200 300 400 500 600 700 800 900azimuth [°]Figure 3.29:Inclination values <strong>of</strong> three data series acquired by identical setups <strong>and</strong> reduced by the levelling error;x-direction (top) <strong>and</strong> y-direction (bottom).the phase angle derived by the y-direction, but there is an angle difference <strong>of</strong> approximately 120 ° betweenthe x-direction <strong>and</strong> the y-direction instead <strong>of</strong> 90 °. In addition, [Gerstbach, 1976] investigated the theodoliteKern DKM2-A <strong>and</strong> found a phase shift in the wobble <strong>of</strong> the vertical axis between the x-direction <strong>and</strong> they-direction <strong>of</strong> 30°.The results show a significant wobble <strong>of</strong> the vertical axis exists <strong>and</strong> the wobble is repeatable.The nextquestion raised is if these results can be reproduced by independent setups.This means the wobble <strong>of</strong> thevertical axis should also be reproducible concerning the frequency, or period, the amplitude <strong>and</strong> the phaseangle, including the difference <strong>of</strong> the phase angles between the x-direction <strong>and</strong> the y-direction.ResultsThe wobble <strong>of</strong> the vertical axis was investigated with several different <strong>and</strong> independent setups.series were analyzed in the way shown so that the results concerningAll datathe harmonic oscillations describedby the parameters frequency, or period, amplitude <strong>and</strong> phase angle can be compared.following:The results are the

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