In this paper the rate of accumulation was studied along four VO floodplain cross sections of the UpperTisza region between 1974 and 2014. VO floodplain cross sections are based on a mapping base-point grid (established in 1890), and they are located a few kilometers from each other. Furthermore, the roughness changes of different surface types, crossed by the VO floodplain cross-sections, were also determined between 1965 and 2015. The accumulation studies were extended to include the accumulation rates of the cut off meanders located along and/or close to the VO cross-sections. The roughness values increased in all four floodplain VO cross-sections since 1965; in two of them it reached or approximated 100 %. The average accumulation ...
During the Late Pelistocene-Holocene transition the fluvial landscape of the Great Hungarian Plain c...
To understand the hydro-morphological responses of a river to engineering works is a key to future s...
An attempt is presented at clearing the reasons of some uncommon flow phenomena observed over the Ti...
The area of floodplains in the Carpathian Basin was dramatically reduced as a result of river regula...
Land-use changes and their effect on overbank sediment accumulation were investigated on thefloodpla...
The aim of the present study is to analyse the morphology, sedi-mentary structure and age of flood-f...
The juxtaposition of natural levees results in alluvial ridges with a unique fluvial record. Our aim...
When examining the characteristics of individual floods Hungarian researchers primarily investigate ...
A dolgozatban a Felső-Tisza szabályozásokat követően elkülönült mentett ártéri, nyílt ártéri és hull...
The Tisza River experienced successive flood peaks between 1998 and 2010. The reasons of the increas...
During the past decade, a series of record flood stages have occurred along the Tisza River, resulti...
The 157 200 km2 large catchment of the River Tisa is situated in the eastern part of the Carpathian ...
Szeged situated at the confluence of the Tisza and the Maros Rivers has been exposed to significant ...
Szeged situated at the confluence of the Tisza and the Maros Rivers has been exposed to significant ...
Tisza is the largest water base in the eastern part of Szabolcs-Szatmár-Bereg County, in north-easte...
During the Late Pelistocene-Holocene transition the fluvial landscape of the Great Hungarian Plain c...
To understand the hydro-morphological responses of a river to engineering works is a key to future s...
An attempt is presented at clearing the reasons of some uncommon flow phenomena observed over the Ti...
The area of floodplains in the Carpathian Basin was dramatically reduced as a result of river regula...
Land-use changes and their effect on overbank sediment accumulation were investigated on thefloodpla...
The aim of the present study is to analyse the morphology, sedi-mentary structure and age of flood-f...
The juxtaposition of natural levees results in alluvial ridges with a unique fluvial record. Our aim...
When examining the characteristics of individual floods Hungarian researchers primarily investigate ...
A dolgozatban a Felső-Tisza szabályozásokat követően elkülönült mentett ártéri, nyílt ártéri és hull...
The Tisza River experienced successive flood peaks between 1998 and 2010. The reasons of the increas...
During the past decade, a series of record flood stages have occurred along the Tisza River, resulti...
The 157 200 km2 large catchment of the River Tisa is situated in the eastern part of the Carpathian ...
Szeged situated at the confluence of the Tisza and the Maros Rivers has been exposed to significant ...
Szeged situated at the confluence of the Tisza and the Maros Rivers has been exposed to significant ...
Tisza is the largest water base in the eastern part of Szabolcs-Szatmár-Bereg County, in north-easte...
During the Late Pelistocene-Holocene transition the fluvial landscape of the Great Hungarian Plain c...
To understand the hydro-morphological responses of a river to engineering works is a key to future s...
An attempt is presented at clearing the reasons of some uncommon flow phenomena observed over the Ti...