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The vertical accuracy of all three data sets in the very shallow water zone shows a relatively small amount of small
difference between the laser grid and echo sounding points, which may be due to the poor echo sounding data. The first
campaign does not satisfy the confidence level of TVU niax . but the percentage of differences came close to 95% between
4-6 m depth. The second and third campaigns fulfill the requirement of TVU max up to 11 m and 8 m depth, respectively.
5. CONCLUSION
In this paper, we present some results of the project ‘Investigation on the use of airborne laser bathymetry in
hydrographic surveying’, in which the applicability of the ALB for monitoring the German Baltic Sea Coast is being
analyzed in cooperation with the German Federal Maritime and Hydrographic Agency. The goal is to investigate the
ALB technique and to determine areas for which ALB is potentially more economical than ship-based echo sounding.
For the first campaign a Riegl VQ-820-G sensor was used, which is designed up to one Secchi depth under certain
conditions, but in the tests about 97.7% of the observed points classified as seabed have a depth of less than 0.7 x Secchi
depth. High point densities are observed in very shallow water regions. For the second and third campaign a Chiroptera
sensor with a nominal penetration depth of 1.5/ Secchi depth was used. The pulses reached up to 1.3 x Secchi depth. On
the one hand, the maximum point density is lower than the results obtained by the Riegl sensor, probably due to the
lower pulse rate and the smaller strip overlap. On the other hand, the point density of the Chiroptera sensor decreases
only slowly with depth. We also show that the shallow areas are well covered up to 0.7* Secchi depth by a Riegl sensor
and up to 1.0x Secchi depth by a Chiroptera sensor. The vertical accuracy of ALB was investigated in a comparison to
echo sounding and was compared to the IHO Standards for Hydrographic Surveys (S-44). In order to fulfill the
requirements, 95% of the differences must be less or equal ±0.5 m. The results of the first campaign do not meet the
demanded vertical accuracy standards, but for approx. 94% of the seabed points of a depth of 3-6 m the differences were
within ±TVU max . The second and third campaign satisfied the requirement in 4-11 and 3-8 m depth, respectively. Overall,
over 92.5% of the seabed points of the three campaigns showed depth differences of less than 0.5 m compared to the
echo sounding data.
In future work the full waveform information will be used for a classification of the points into several seabed substrates
and underwater vegetation.
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Proc. of SPIE Voi. 9638 96380Z-8