2.3. Geographical location of single informations by means of orthophotos
Aerial photographs and film strips from scanners of high mountain ter
rain are subject to rather substantial geometrical distortions. To compare
different information in different data-sets of the same areal unit with
each other their exact location within a coordinate system is absolutely
necessary. This is achieved by a gridcell sampling technique. The construc
tion of such a systemic grid on the very heterogeneous photographic material
regarding scale and distortions would be most unpractical. Therefore the
different interpretation results first had to be transferred onto a uniform
data-base (Lit. 8). The most convenient form for such a data-base for high
mountain terrain presents the orthonhot ography (Lit. 9). Almost all impor
tant surface features and their boundaries recognizable on aerial photographs
are visible on the orthophoto, too. This allows a relatively simple, fast and
accurate transference of the interpreted data onto the general data-base.
On the other hand the number of identification points in maps of high moun
tain terrain is limited and insufficient, and the transference with instru
ments in extreme relief not precise enough and uneconomical. In addition
the oblique photographs could be oriented easily with the aid of the ortho
photos.
2.4. Quantification of data and storage in a data-bank
Besides the qualitative results an addition of quantitative informa
tion and the organization of the data for geoecological applications is
essential. The arrangement of the data in matrix form and the compilation
of a data-bank allows an easy further processing and outputs in various
ways, such as:
- printer maps of whatever element(s) and changes are desired,
- statistics, tabulations, areal measurements,
- graphical presentations,
- calculation of ecological correlations,
- print-outs of an element (or combinations of elements and changes) in cor
relation to another element (or elements) (e.g. the distribution of a
specific plant in relation to various features such as soil moisture etc.).
The interpreted data is transferred onto the orthophoto and then
sampled for each gridcell, coded and stored in matrix form. The quantitative
information and the coding of the qualitative information in alphanumerical
form has to be considered carefully, and individually for each feature. The
number of categories into which each feature is divided has not to be equal,
but for the different data-sets of a single feature (e.g. the different
situations of the snowcover) the same categories should be used.
For the Grevasalvas test site the grid was placed over an orthophoto
1 : 5'000, and oriented in accordance to the national coordinate system,
allowing an integration of the local information system into the existing
national data-bank. The grid width depends on the size of the area under