Geometric Transformation Models (Helmert, Bursa-Wolf,
Moledenski-Bedakes etc.), Two-parameter Polynomials, Finite
Elements, Interpolation Methods (LSQ, Least Curvature,
Triangulation etc.) (TKGM Turkish National Transformation
Project Report 2008).
2. GEODETIC INFRASTRUCTURE IN TURKEY
After the adjustment of the National Fundamental Triangulation
Network in 1954, the fact remains that some parts were revised,
but there are errors in adjustment modeling related to the
reduction of measurements; various plates move with different
velocities because of tectonic properties in and around Turkey
and these movements were not monitored systematically;
because ED-50 coordinates were not renewed in accordance,
points were displaced in different velocities and because the
studies carried out before 1988 Regulation were in local
coordinate systems, many engineering works including cadastre
were done at local coordinate systems.
Since inner accuracy or local accuracy criteria were minded in
densification works, information about network accuracies was
not required. Therefore, detailed examination cannot be done.
Moreover, the networks, formed according to 1988 Regulation,
provide inner integrity. However, problems arise in larger
scales. First and second order points were calculated with
respect to adjustment, whereas lower degree points were
calculated by inter/re-section methods.
Distortions resulting from crustal movements, landslides etc. in
networks generated by conventional methods are an inevitable
fact Every single point group of these networks forms a
separate datum. Up to a recent history in Turkey, ED-50 was
used and all geodetic networks, maps and measures were
generated at this datum. The National Geodetic Network studies
in question were began in 1950-1954 by the General Command
of Mapping (HGK) and 449,215 points were established with
the subsequent densifications done by the cooperation of the
General Directorate of Land Registry and Cadastre (TKGM)
and HGK. These networks have an accuracy of 10-20 ppm.
Third and fourth order 285,000 triangulation points were
established, measured and calculated for the purpose of
producing 1/5,000 scaled standard topographic maps. These
points, whose 71,000 were produced by HGK and rest 215,000
by TKGM, are present within the archive of TKGM. The
accuracy of the National Geodetic Network fell behind the
accuracy that the modern technology has reached. In order to
fulfil this need, the Turkish National Fundamental GPS
Network (TUTGA), consisting of 594 points, was established
between 1997-2001 by TKGM and HGK. The coordinates and
velocities of TUTGA points were determined in ITRF. Relative
accuracy of the network is 0.1-0.01 ppm, whereas point position
accuracy is about 1-3 cm (TKGM Turkish National
Transformation Project Report 2008).
2.1 Some of the Results obtained between TUTGA and ED-
50
a) +3-5 m transformation match was obtained for whole Turkey
with 3D similarity transformation between TUTGA99A and
ED-50 using 220 points.
b) +1.5-2 m transformation match was obtained for every single
Zone with separate similarity transformations.
c) Similar results were obtained through modeling latitude and
longitude differences.
d) For Izmir and Istanbul, transformation accuracies of +8 cm
and +10 cm were obtained, respectively.
According to the 82™ article of the Large Scale Map and Map
Information Production Regulation, minimum transformation
accuracy was taken as 49 cm. According to the 100^ article,
transformation enhancement and update tasks were given to
TKGM, HGK and universities. However, increasingly growing
municipality borders, Metropolitan municipalities and
countrywide projects like TUSAGA-Aktif require horizontal
and vertical parameters persistent for whole area with high
network accuracy or transformation grid data. Using this data
has to be juristically guaranteed. For example, technical and
juridical guarantee has to be provided for transferring
information produced at ED-50 or ITRF derived from legal
cadastre information without accuracy loss. This requirement
constitutes the primary concern of datum transformation.
All maps and coordinates produced countrywide until 2001 are
on ED-50. There are around 283,000 map sheets on ED-50
within the body of TKGM. Transformation into ITRF datum of
these map sheets is an inevitable fact. However, most of these
map sheets are not digital and errors coming from production
(erroneous measurement, drawing, edging etc.) exist. Bringing
these maps into digital form with digitizing and absolute
transformation will transfer the existing errors to digital map
and result in legal consequences.
Transformation accuracy of ED-50 data and map sheet scale are
desired to be concordant. Accuracy on 1/1,000 scaled map
sheets is around 0.2-0.3 m and taking relative accuracy into
consideration with respect to National Geodetic Networks, it is
required to have common points at 10-30 km intervals whose
coordinates are determined on ED-50 and ITRF. Thus, GNSS
measurements will be required for a reasonable transformation
at geodetic points that map sheets depend on and at produced
details. This will be possible by loss in transformation accuracy
(TKGM Turkish National Transformation Project Report 2008).
3. COMMONLY USED DATUMS IN TURKEY
3.1 European Datum 1950 (ED-50)
All maps and coordinates produced countrywide until 2001 are
on ED-50. There are around 283,000 map sheets on ED-50
within the body of TKGM.
Up to a recent history in Turkey, ED-50 was used and all
geodetic networks, maps and measures were generated at this
datum. The National Geodetic Network studies in question were
began in 1950-1954 by HGK and 449,215 points were
established with the subsequent densifications done by the
cooperation of TKGM and HGK. These networks have an
accuracy of 10-20 ppm. ED-50 represents International 1924
Ellipsoid which was defined locally for Europe (TKGM Turkish
National Transformation Project Report 2008).
ED-50 takes International 1924 Ellipsoid (a-6378388 m;
b=6356911.9461; f=1/297; e=0.08199188998) as reference
ellipsoid, and Greenwich Meridian as prime meridian. In this
system, Helmertturm point (®=52° 22" 51”.446 N; A=13° 03’
58".741 E; Geoid height (N) = 0 m; north-south component of
deflection of the vertical ({)=3".36, east-west component of
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