FLOODS AND FLOOD RISK MAPPING IN THE
I. Kovalchuk, A. Mykhnovych
admin@ukrmap.com.ua
In the
last decades the human activity in the mountain part of the Dnister river basin
causes activization of extreme floods development. Traditionally the main
measures of flood protection in the
The
problems of flood development, flood protection management and hydrological
regime analysis of the Upper Dnister have been investigated within the joint
German-Ukrainian research project “Transformation processes in the Dnister
region (
▪
hydrological
data base (daily discharge and water levels, precipitation) was
elaborated;
▪
the
data bases containing morphometric parameters of river valley and river bed,
morphometry and present state of embankments have been created;
▪
the
present technical state of embankments as well as risk of their breaking and
overflooding was evaluated;
▪
flood
modelling applying GIS technologies is carried out;
▪
GIS-models
were verified by comparing them with maps showed real flooded areas created in
the upper Dnister river valley.
The floods
and flood risk mapping were realized applying ArcView and ARC/INFO GIS software
and also GIS-integrated software for hydrological modelling like HEC-RAS.
As the
result of investigations the large-scale GIS-model of flooded zones has been
created. The dynamic GIS-model of flood development for different probability
has been created. Overlaying of created models on the map of land use the risk
of economical damages has been evaluated.
Other
part of our investigations in the Dnister catchment is assessment of riverbed
processes and their impact on a flood risk due to threat of embankments
destroying by erosion processes as well as of sediments accumulation.
Assessment
of scales, intensity and trends of river beds vertical deformations was based
on the set of cross-sections and longitudinal profiles as well as water
level–discharges relation curves created for different periods of time.
For
investigated catchments trends, scale and average intensity of deformation for
period 8 – 32 years have been calculated. Obtained results have shown that
mountain and pre-mountain catchments are characterized by highest potential of
hydro-geomorphologic processes and intensity of their development. Erosion
dominates within the larger part of Dnister catchment.