International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B4. Istanbul 2004
.A.- The need for up-to-date topographical information
showing the situation just before the emergency situation;
B.- The need to acquire as quickly as possible heterogeneous
geospatial data from the disaster area after the emergency
situation in order to understand and monitor the situation, to
evaluate the damages and the risk for additional damages and
injuries, to plan and monitor the rescue/recovery operations.
Same data (as high resolution imagery) should be recorded
repeatedly over the same area for monitoring needs. In
addition, the team has to address the problem of integrating
these layers of data from divers origins, not necessary
homogenous, having different resolutions and precision.
In a real life situation, the separation between these two main
cartographic problems is not so clear. In many areas the existing
topographic information is not updated on a regular basis and
some important changes for examples for the local road network
(such as access roads to industrial facilities) are not included in
the last version of the topographic database. The Emergency
Mapping Group will face the challenge for example to use the
new imagery layers recorded after the disaster for 'situation
understanding’ purposes and in the same time for the updating
of the old topographic information. Same confusions and errors
could happen.
Another possible issue is the delivery of geomatics outputs to
the main group of users, the emergency services, in order to
help the understanding of the ongoing changes. This issue is not
discussed in the present paper.
4. OUR TESTS IN OTTAWA SOUTH
4.1 Description of the test
The Centre of Topographic Information (CTI) began to
investigate in 2001 the development of rapid mapping and rapid
change detection systems for current mapping operations and
for emergency situations. A contract was granted in 2002 to
Mosaic Mapping Systems Inc. of Ottawa for an airborne survey
of a test area of about 5 square kilometres (1.5 km x 3.5 km).
The contractor had to provide a turnkey airborne survey,
complete with data acquisition of LIDAR and digital camera
data, and GPS field control.
The overall objective of this project was to test and evaluate the
acquisition, processing and handling of LIDAR DEM data
collected simultaneously with optical data and their contribution
to a rapid change detection system.
Flight and LIDAR Parameters:
Flight Altitude: apprx. 300 m AGL (Above Ground Level)
Swath Width: apprx. 300 m
Laser Wavelength: 0.9 um
Scan Angle: up to +/- 30 degrees
Flight Overlap: 40 percent
Flight line Spacing:apprx. 140 m
Point Density: 0.4 m x 1.0 m (approximate and adjustable)
Scan Rate: 34 hz (approximate and adjustable)
Data rate: 10 MHz
Beam Divergence: 3.0 mrads (90 cm spot size at 300 m)
Collection Mode: Last Pulse and Intensity
Digital Camera Data:
[mage size: 2300 x 3500 pixels,
Resolution: about 8 cm, at 300 m
Image Swath Size: apprx 400 m x 260 m, at 300 m
A second flight (recording optical images only) was flown at
900m above ground.
The test area was chosen in the South of the City of Ottawa
along the Rideau River, close to the Ottawa Airport. One of the
selection criteria was to have a variety of topographic features
and land use categories: roads, railways, two important bridges
over the Rideau river, residential and industrial areas with
buildings of different sizes, lakes, some vegetation spread
across the residential area, a more dense forest area along the
river and some terrain height variation.
4.2 Reference data
Landscape change detection analysis involves the comparison
of two or more spatio-temporal datasets and the identification
and location of differences in the patterns of two spatio-
temporal datasets. For change detection operations it is
important the have a good spatial registration between the two
data sets. In order to test the change detection operations and
other mapping operations needed for emergency mapping as
merging/fusion of heterogeneous geospatial data sets, more
imagery and digital topographic data were acquired for the tes
area:
- National Topographic Data Base (NTDB) data set 31G05;
- Colour aerial photography from 1999 at 1:15 000 scale.
In addition, for the evaluation of the LIDAR data and the
associated digital camera, a data set of over 230 check points
have been measured by the Mapping Services Branch personnel
using the GPS kinematic technique. This data set was used only
as independent checkpoints and was not communicated to the
contracting company. A number of 6 points were signalized.
Part of the GPS check points were recorded as profiles over
different slope shapes: across and along a railway track, alonga
country road with moderate, constant slope, across a 5 levels
building and its attached flat parking lot, etc.
4.3 Results of Ottawa tests
4.3.1 A priori accuracy estimation:
The expected accuracy was estimated a priori using the
manufacturer specifications of all the components of the Mosaic
Mapping LIDAR system and taking in account the company’s
experience in operating the system in standard terrain
conditions and in processing the data.
Considering a confidence level of 95% (2 sigma), the expected
accuracy of the LIDAR data was as following:
a.- For the absolute Vertical Accuracy: +/- 0.15 to 0.25
meters on Hard Surfaces; +/- 0.25 to 0.40 meters on
Soft/Vegetated Surfaces (flat to rolling terrain); +/- 0.40 to 0.75
metres on Soft/Vegetated Surfaces (hilly terrain).
b.- For the absolute Horizontal Accuracy: +/- 0.75 to 1.0
meter on all but extremely hilly terrain.
4.3.2 Evaluation of the LIDAR DSM and DEM:
The LIDAR data was delivered in two versions:
- The ‘original’ data set containing all the laser signal returns
called ‘all-returns’ was used to produce the digital surface
model (DSM),
- The filtered data set produced using 2 automatic filtering
processes and an interactive editing, intended to eliminate all
the noise, the buildings, the trees an all objects above the
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