Abstract The River Tisza is one of Central Europe's most important rivers. In the last one and a half century numerous anthropogenic activities have influenced its watershed. As a result measures need to be taken to protect its water quality, necessitating a comprehensive picture of the spatial and temporal variability of its processes, which this study aims to extend further. In this study five sampling locations were analyzed in the upper section of the Tisza over the time interval 1974–2005, dealing with 24 parameters using multi-variate data analysis methods. Employing time series analysis and taking the river's tributaries into account, the strong influence of the River Szamos was pointed out, while stochastic connections indicated t...
In the last millennium one of the most important changes in the natural environment of the Great Hun...
An attempt is presented at clearing the reasons of some uncommon flow phenomena observed over the Ti...
The Tisza River experienced successive flood peaks between 1998 and 2010. The reasons of the increas...
Tisza is the largest water base in the eastern part of Szabolcs-Szatmár-Bereg County, in north-easte...
The research was done on the upper section of River Tisa from its two sources (rivers Bila Tisa and ...
The Tisza river plays an important role in the life of Eastern Hungary. Beside the river there are s...
This study investigates the potential of using principal component analysis and other multivariate a...
Doktori kutatásom során célul tűztem ki a Felső-Tisza vidékén Tokaj-Tiszabercel- Kótaj által közrezá...
The 157 200 km2 large catchment of the River Tisa is situated in the eastern part of the Carpathian ...
The aim of this article is to evaluate the quality of the Danube River in its course through Serbia ...
We have assembled and assessed the statistical procedure which is capable to objectively explore inf...
The research of the River Some? was accomplished during two field campaigns organised by the Tisza K...
In the Great Hungarian Plain (GHP), one of the most complex fluvial systems of Europe developed thr...
In this paper the rate of accumulation was studied along four VO floodplain cross sections of the Up...
In the section above Tiszaújlak, despite the presence of embankments, the River Tisza shows active ...
In the last millennium one of the most important changes in the natural environment of the Great Hun...
An attempt is presented at clearing the reasons of some uncommon flow phenomena observed over the Ti...
The Tisza River experienced successive flood peaks between 1998 and 2010. The reasons of the increas...
Tisza is the largest water base in the eastern part of Szabolcs-Szatmár-Bereg County, in north-easte...
The research was done on the upper section of River Tisa from its two sources (rivers Bila Tisa and ...
The Tisza river plays an important role in the life of Eastern Hungary. Beside the river there are s...
This study investigates the potential of using principal component analysis and other multivariate a...
Doktori kutatásom során célul tűztem ki a Felső-Tisza vidékén Tokaj-Tiszabercel- Kótaj által közrezá...
The 157 200 km2 large catchment of the River Tisa is situated in the eastern part of the Carpathian ...
The aim of this article is to evaluate the quality of the Danube River in its course through Serbia ...
We have assembled and assessed the statistical procedure which is capable to objectively explore inf...
The research of the River Some? was accomplished during two field campaigns organised by the Tisza K...
In the Great Hungarian Plain (GHP), one of the most complex fluvial systems of Europe developed thr...
In this paper the rate of accumulation was studied along four VO floodplain cross sections of the Up...
In the section above Tiszaújlak, despite the presence of embankments, the River Tisza shows active ...
In the last millennium one of the most important changes in the natural environment of the Great Hun...
An attempt is presented at clearing the reasons of some uncommon flow phenomena observed over the Ti...
The Tisza River experienced successive flood peaks between 1998 and 2010. The reasons of the increas...