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CONTRIBUTION TO THE DTMs STUDY
(DTM ON DRAINAGE STUDIES)
Patmios E., Professor
Laboratory of Photogrammetry-Remote Sensing
Dept. of Civil Engineers
Polytechnic School
Aristotle University of Thessaloniki GREECE
Commission IV
ABSTRACT
In this paper the subject of DTM is dealt with, on the base of a triangle net of sampling points.
The basic principles of digital model are presented as well some products (indicatively contours, secti-
ons, etc.).
The example concerns an area of Athos peninsula, which is especially important as historic (monastic)
center.
The digital model was chosen at first as suitable for the mountaineous relief, but it can also be used
for general applications.
Many cartographic facilitations can be achieved based on this DTM.
Furthermore, requirements of geoinformation systems and aspects of correlation with sattellite data can
be facilitated.
1. INTRODUCTION
Several internal and external factors in combina-
tion with human action, have formed and continue
to form the shape of the surface of the earth.
Sciences as geomorphology, geology, geodesy, pho-
togrammetry, Remote Sensing etc, study among othe-
rs the surface and generally the crust of the
earth from various aspects. The study concerns the
qualitative and quantitative research in correla-
tion, or not, with the relevant dynamic causes.
In this research the presentation of the forms
oontinues to be the basic pursuit. Several methods
have relatively developed at times, with advanta-
ges and disadvantages correspondingly. The con-
tour curves constitute a specially useful way of
presentation, with which the scientists and te-
chnologists are particularly familiar. Scientific
and technological progress, automatisms etc.,
contineously improve the considerations about the
methods of presentation of landforms.
On this base the considerations on DTM present
particular advantages and for this reason their
study has multiple interest, theoritical and pra-
ctical, not only for the presentation of the
landform but for every other form (architectural
elements, etc.).
For a totality of points for which we know with
some method (topographic, photogrammetric etc.)
the altitude (sampling points), the mathematical
Structure and the calculation procedure for find-
ing, basing on the above, the altitude of other
point in the consideration area, in generally the
content of a DTM (4).
For all the cases, except the others, the choice
of the sampling points is basic stage, determinal
for the quality of all the work. The sampling
points may form nets of various kinds (orthogonal,
Square, triangular etc.) regular or irregular.
They also may be taken along different lines (co-
ntours, morphological etc.) or at various combi-
nations of the above with the correspondent ad-
vantages and disadvantages. The choice of the
sampling points may be determined from the begin-
ning or during the measurements. Method of the
sampling procedure which allows the progressive in-
crease of the density of sampling points, based on
some criteria, where the landform demands (1) or
compound works of additional taking of lonely and
characteristic sampling points (2), especially
surve the whole problem of DTM. The method of
sampling that is being used, in combination with
the landform (categories of terrain) constitute
determinal factors for the general quality of all
the works, as accuracy benefit, etc.
The above concern only some characteristic points
from the research relatively to DTMs. Therefore it
is obvious that the general study of DTMs is a
multiple and compound work which continues to be
systematically faced (isolated researchers, Insti-
tutes, work groups of International Commissions
eto.
At some cases it is useful and realistic local par-
ticularities and factors to be seriously taken up
in mind (weakness in substructure of DTMs, various
necessities in applications, general developing
plans, particularities of the relief etc.).
Of this point of view, and to continue our previous
study (3), we developed a DTM basing on a triangu-
lar net of sampling points.
The basic principles of the mathematical model, of
the sampling procedure and the calculation of sec-
tions and contour curves are shortly presented in
this paper. An example for the case of study of a
drainage net is also presented (area of Agio Oros,
Athos Peninsula, Greece).
2. BASIC PRICIPLES OF THE DTM
At the presented DTM the surface of the land is at-
tached by a polyhedral surface which has triangles
as faces, with apexes the sampling points.
Basing on this surface, for every other point P
with horizontal coordinates Xp, Yo; which belongs
in the limits of the surface determined by the sa-
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