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SCOP AS AN ALL-PURPOSED TOOL FOR ELABORATION OF DIGITAL TERRAIN MODEL
- THE USER'S COMMENTS
Marta Borowiec, Krystian Pyka
The Department of Photogrammetry and Remote Sensing Informatics
St.Staszic University of Minig and Metallurgy, Krakow, Poland
Commission IV, Working group 4
KEY WORDS : DEM/DTM, GIS, Digitization, Orthoimage, Acqiusition, Modeling
ABSTRACT
Depending on the scale, scope and kind of problems solved by the spatial information system (GIS,LIS) they need to
be supported by DTM with different degree of accuracy and minuteness of detail.
The quality and accuracy of DTM depend on the data-acquisition and the mathematical technique of interpolation. In
this paper, the acquirements with different projects, which purpose was a description of the surface of the earth as well
as another objects, will be presented. These experiences were carried out in 1993-96, thanks to supplying us with the
SCOP package within the framework of Central European Initiative (CEI).
1. INTRODUCTION
Since mid 1993 the Department of Photogrammetry and
Remote Sensing Informatics at AGH has got the
specialistic SCOP (Stuttgart COntour Programme)
package. The package is a result of many years long
experiments carried out by researchers at Stuttgart and
Vienna Universities. It has been continuously modernised
and developed.
It is indispensable in GIS systems to have information
about the surface relief. The most popular forms of
representation of the terrain topography are isolines or
regular grids. The grid form, is more applicable because
it gives possibilities for 3-D space analyses and is
necessary for ortho-rectification of aerial or satellite
images.
The source of data for DTM creation can be different, but
most often the data are collected from topographic maps
or aerial photographs. The choose of data source and the
method of their digitization depends on many factors as:
- data accessibility;
- required accuracy;
- time and costs of production.
In the last 2 years the Department of Photogrammetry
and Remote Sensing Informatics accomplished several
projects related to creation of a DTM. In each of the
projects the SCOP was used to create DTM
independently from data acquirement method.
In the paper, the authors present the way of
such data preparation for reliable SCOP interpolation
avoiding impact of big differences in data density.
2. DATA ACQUISITION
The accuracy of DTM is strongly related to the method of
data acquisition. Direct geodetic survey is the source of
the most accurate hights information. A competitive
method, especially from the viewpoint of economy, is
photogrammetric survey.
When accuracy requirements are low then digitization of
the existing cartographic maps is a relatively cheap and
fast method for data acquisition. The latter method is
661
widely used in data collecting for Geographical
Information Systems ( GIS).
In our projects we have applied various methods of data
acquisition: direct digitization of topographic maps,
digitization of scanned maps, stereo-digitization of aerial
photographs, and direct field measurements with use of a
total station. The variety of these methods is presented in
Table 1, which contain short characteristic of some
projects.
3. MATHEMATICAL MODEL OF INTERPOLATION
In each projects shown in Table 1, the SCOP was used
to create DTM. In comparison with other programs in the
field of DTM, the SCOP has some particular features,
among others:
- four categories of points are taken into consideration
in the interpolation process: dispersed points, spot
heights, sequences of points that create the form
lines, and break lines,
- the possibility to assign different accuracy to data
allows for interpolation with filtration.
The SCOP reliably models the terrain relief in those
cases where the data are obtained along profile lines
supplemented with the structural lines. It is interesting
that the SCOP program is easier to use for mountainous
and wavy terrains than for the plane ones. In the latter
case it requires a significantly higher density of data than
it can be obtained from contour line digitization.
The effects of SCOP interpolation are not stable in
areas of different density of data. This occurs especially
in places where the flat terrain transits into elevated
surface.
The linear prediction method was used to interpolate the
DTM points. This method is reliable to cope even with the
most complicated surfaces including the elements of
their discontinuity. However, the calculation parameters
should be choosen with caution and data have to be
properly prepared. For proper interpolation program
requires similar data density for the whole area, what in
many cases is difficult to achieve.
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B4. Vienna 1996