Abstract:
Abstract: The use of GNSS technologies for precise point
positioning enabled the calculations for single-point observations
or relative positioning of long baselines. The GNSS absolute and
relative positioning techniques can be implemented between
points within different tectonic plates, while the classical
surveying methods start from local reference/triangulation points
to near points within a few kilometers. The definition of the
kinematic models of the earth has become an important role in
GNSS measurements techniques and networks adjustment
methods based on international terrestrial reference frames
(ITRF), where the reference points can be located in different
continents and tectonic plates. Thus, the position calculations in
the ITRF systems are time-dependent. To satisfy the requirements
of land and cadastral surveying, the bidirectional transformation
between classical geodetic networks and GNSS global, regional
and local networks is nowadays a primary requirement in modern
geodesy. While the classical networks were defined locally
assuming a static earth system, the ITRF coordinates by GNSS
techniques are defined globally and directly affected by earth
kinematics including plate tectonics and local crustal movements.
However, Palestine has a special kinematic situation because it is
located at the border between two plates; Nubia/Sinai plate and
the Arabia plate along the Jordan valley line. Thus, the result is
unsteady surface kinematics all over the country, which has a
longitudinal shape parallel to the Jordan valley rift. Using the
IGS/EUREF stations and GNSS stations data that are freely
available on the internet, varying positional velocities were
calculated in both magnitude and direction using years of daily
available GNSS raw observations. The GNSS precise observation
techniques have proven that the points of the classical networks
were subjected to a kinematic situation over the years. Therefore,
the Palestinian geodetic network has to be revised for kinematic
effects for the integration with the modern GNSS positioning. In
this work, the effect of surface movements is included in the
calculations between the different ITRF coordinate systems and
the classical geodetic network of Palestine. To achieve the
required transformations between ITRF and the classical
network, a velocities model was established and tested utilizing
GIS raster interpolation. The accuracy of the modeled velocities
could support 1cm in static or real-time GNSS positioning. This
made it possible for the integration between geodetic
measurements between different time epochs.