The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B5. Beijing 2008
improves the navigation for flight lines where a constant
height over the topography is required.
D. Flight Plan management: Different flight plans and flight
lines can be loaded and activated. The line attributes (such
as height, required speed over ground or sensor head
attitude) can be displayed for each line.
E. Laver control: GIS-like control to display or deactivate
different data layers.
F. Online/offline button: Control button to switch between
online mode (RT georeferencing, display of RT swath
boundary) and offline mode (data coverage analysis,
transmission of data extend and data gaps to HELIPOS
(see section 5).
7. DISCUSSION OF RESULTS
The described software modules have been tested on several
flights in the period of January to April 2008. In this section we
will discuss some of the results comparing the real-time
solutions (trajectory and raw point-cloud) and indicators to that
of post-processing.
7.1 Trajectory
Differvnc* in Tra|«ctory determination (RT - Postprocessing)
01 Poll l Pitch
8«!
Yaw
oaf
PXcrt mean 0 00". stt) 0 0T
■> 0X»'}rn 0M‘
1755 3 7« 3 795
Figure 9: Difference in the computed position, attitude and
velocity between the RT solution using point
positioning and post-processed solution using CP-
DGPS.
Figure 9 shows the difference in trajectory estimation (position,
attitude and velocity) between the RT solution using point
positioning (computed by GIINAV) and the post-processed
results based on differential carrier-phase (computed by
GrafNav/PosProc) for a flight by helicopter in the region of
Lausanne (Switzerland). The plot depicts that the difference in
attitude is low (roll /pitch: RMS < 0.05°, yaw: RMS <0.1°) and
close to the noise of the used IMU (Litton LN-200), whereas
the difference in absolute position is more important (RMS
planimetry > 1.5m, RMS altimetry > 4m). These results are not
surprising, considering that neither DGPS nor RTK (Real-time
Kinematics) were used for the RT solution. The correspondence
in velocities is much better due to the influence of the IMU
data.
7.2 Laser point-cloud
For the in-flight quality assessment of the ALS data mainly the
accuracy and the completeness of the georeferenced point-cloud
is of interest. The histograms in Figure 10 depict the
distribution of the point-cloud coordinate differences (RT point
positioning GPS/INS versus reference trajectory). As proven by
forward covariance propagation (Glennie, 2006; Landtwing,
2005), the errors in position propagate directly into the
georeferenced point. Accordingly, the east and north
components are similar (RMS « 1.5 m) to the position errors in
the trajectory (Figure 9). The RMS of the height component is
about 2-3 times worse. But again, corresponds well to that of
point-positioning accuracy in the vertical channel. In this
particular flight the height over ground was approximately
250m. Thus, the angular discrepancies had a minor impact on
the final georeferencing quality (roll/pitch: 0.05° at 250m « 0.2
m). Hence, up to 1000 meters flying height a 2D point-cloud
accuracy below 3m can be achieved without differential
techniques. For the purposes of in-flight monitoring displaying
the swath and the computation of data coverage, this accuracy
is largely sufficient.
Difference in pointcloud coordinates (RT - Postprocessing)
met®«
t«»t: m*an 0.9m aid 0.9m Nortti: mean 0.8m atd 1.0m Op: mean -2.0m aid 2.3m
Figure 10: Histograms of difference in point-cloud coordinates
computed in real-time and in post-processing (based
on 3.7 Mio samples)
As the relative accuracy of the laser point-cloud is not affected
by the positioning accuracy, the integrity of the results of LI AN
can be guaranteed even in point-positioning mode. Comparing
the data extends and data gaps computed using the RT and the
post-processed point-cloud indicated no substantial differences.
All data gaps were identified correctly, and the identified
boundaries (in 2D) corresponded to the accuracy for the single
laser point (i.e. RMS «1.5 m).
7.3 System Performances
The testing in several survey missions was also very
informative about the achievable system performances in terms
of manageable data rates and CPU load. To separate the vital
and extended elements physically from each other, the
computing was divided on two field laptops:
• LOG-PC: linked to hardware (GPS/IMU/LiDAR) through
Ethernet and running the GPS Datalogger, ALS
Datalogger and IMU Datalogger modules.
• NAV-PC: Linked to LOG-PC through Ethernet and
running the LIEOS, GIINAV and HELIPOS modules.
On the LOG-PC the CPU consumption was very low with peaks
not passing 10%. Even tough data thinning of the raw ALS data
can be enabled, we tested LIEOS at the full data rate of the
employed laser (lO’OOO points/second). Trajectory computation
by GIINAV was performed at 400 Hz, whereas trajectory
information (position, attitude and velocity) was transmitted at
1Hz to HELIPOS. The swath boundaries were also updated at
1Hz. Running only the georeferencing and naviagtion modules
occupied the CPU of the NAV-PC with less than 5%. The most