The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-2, 2018
ISPRS TC II Mid-term Symposium “Towards Photogrammetry 2020”, 4-7 June 2018, Riva del Garda, Italy
This contribution has been peer-reviewed.
https://doi.org/10.5194/isprs-archives-XLII-2-961-2018 | ©Authors 2018. CC BY4.0 License.
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5.3 Comparison
Overall, the effects predicted in the numerical simulation are confirmed
by the experimental validation. Compared to the experimental
results the simulation tends to be too optimistic. The wave
induced height and planimetry coordinate errors obtained from
the experimental validation are 10 times larger than the values
predicted in the simulation. The main reason is the limitation
of the simulations to identical forward and backward laser pulse
paths here. Effects of dispersion and diffuse reflections at the
water bottom are neglected.
Another reason is the difference between real and simulated water
surface. The simulated wave pattern is characterized by smoother
wave crests as shown in figure 4. Furthermore, the artificial character
of the machine-made waves is not optimally reproduced
with the oceanographic statistics based surface wave model for
ocean waves, especially reflections of waves at the pool wall.
Moreover, the distribution of the water surface points differs in
simulation and experiment. The simulation is based on a homogeneous
distribution with 1 respectively 10 points per square meter.
In contrast, the water surface representation used for the experimental
validation is characterized by an inhomogeneous distribution
of water surface points. Figure 8 shows an example for
a typical point distribution present in the data sets. The point density
varies from 0 to 8 points per square meter. The results of the
experimental validation remain mean values for the whole investigation
area averaging zones with high and low point density.
Assessing the results of numerical simulation and experimental
validation, furthermore, the different level of detail used for the
ray path modeling has to be considered. In contrast to the simulation,
the refraction correction of the measurement data does not
take into account the beam divergence, instead the laser pulse is
treated as infinitesimal small line.
6. CONCLUSION
This contribution investigates the effect of wave patterns on coordinate
accuracy in airborne LiDAR bathymetry. For this purpose,
a numerical simulation as well as an experimental validation was
carried out for a real world scenario. The comparison of the errors
predicted in the simulation and the errors derived from real
measurement data show a consistent tendency. However, the experimental
validation reveals significantly larger errors than predicted
in simulation.
Furthermore, the results indicate that the effect of wave patterns
is not sufficiently considered in common refraction correction
methods. Therefore, a next step could be to model local wave
patterns on the basis of real LiDAR bathymetry water surface reflections.
As a final result, point-wise strict coordinate correction
terms can then be applied in order to increase the accuracy potential
of airborne LiDAR bathymetry.
ACKNOWLEDGEMENTS
The research work presented in this paper has been funded by
the German Research Foundation (DFG). We would also like to
thank Milan Geoservices for acquiring the LiDAR bathymetry
data used in this study. Finally, our thanks goes to the operator of
the swimming pool, sbf GmbH Radebeul, providing access to the
swimming pool facility and controlling the wave machine.
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