Adalékok a tiszantuli szikes területek mikroklimajahoz. (Some remarks about the microclimate of alkali areas in the region east of the Tisza river)
Climat ; Géographie de l'Europe ; Hongrie ; Microclimat ; Sol ; Sol salin ; Tisza
Many scientific disciplines have paid particular attention to the problem of alkali soils covering extensive areas in the region east of the Tisza river. In order to assess the results of the measurements both analytical and graphic methods were
A Tiszantul kozépso részének kozpontjai, területi elrendezodésük, potencialjuk. (Centres, regional pattern and potentials of the central part of Trans-Tisza region)
(1978) ; Fonction centrale ; Géographie de l'Europe ; Hiérarchie ; Hongrie ; Peuplement ; Réseau urbain ; Tisza
On this part of the Trans-Tisza region, due to the changing possibilities, the differences of historical development and changes in politico-geographical situation, an unsettledness and an image with full of contradiction can be found
Géomorphologie ; Hongrie ; Hydrologie fluviale ; Lutte contre les inondations ; Régime fluvial ; Tisza
These studies are realized in the Tisza river basin (E Hungary). Extremely high water levels of the Tisza river over the last few years drew the attention of scientists and the public to the question of efficiency of flood prevention in Hungary
. After a brief overwiev of the history of flood control in the Tisza basin the most important tasks of research and the possible adequate methods of flood control are discussed. - (JS)
Water temperatures of the Danube and Tisza Rivers in Hungary
Années 1951-2010 ; Bassin-versant ; Changement climatique ; Corrélation ; Cours d'eau ; Danube ; Hongrie ; Hydrologie fluviale ; Série chronologique ; Température de l'eau ; Tisza
Based on a 60-year long hydrological observation series from the Hungarian Hydrological Service (between 1951 and 2010), the monthly mean water temperatures of both largest rivers in the Carpathian Basin, the Danube and the Tisza were studied
in the paper. The monthly extremes in water temperatures were explained by the different climatic conditions in the drainage basins of the rivers : the Danube basin upstream its entrance to Hungarian territory with a marked Atlantic and the Tisza basin
The development and relationship between an alluvial plain and a neighboring alluvial fan was evaluated in the paper on the case of the Lower Tisza Region and the Maros alluvial fan. The paleo-channels on the surface differ in their size and channel
The Lower Tisza floodplain can be divided based on height conditions. The lower floodplain was probably the result of tectonic movement and river incision during the Late Pleistocene or the Holocene. However, the exact date and circumstances of its
A folyópartok alakjánk szerepe a hullámtereken kiülepedö üledékek szemcse- és nehézfém frakcionációjában, a Duna és Tisza példáján
Caractérisation physique des sédiments associés à des métaux lourds dans les plaines d'inondation actives des fleuves Danube et Tisza, Hongrie
Charge en suspension ; Cours d'eau ; Danube ; Hongrie ; Métaux lourds ; Plaine d'inondation ; Tisza ; Végétation ripicole
This paper focuses on the filtration and physical speciation of suspended load by riparian belts, which is a form of appearance of this buffer function. Five transects were traversed along the Danube and Tisza rivers. Samples were taken from river
Az árvízek település - és településhálózat formáló hatása Felsö-Tisza-vidéken
Impact des crues sur les habitats et le réseau d'habitat de la région de la Tisza supérieure
Cours d'eau ; Crue ; Habitat ; Habitat rural ; Hongrie ; Impact ; Logement ; Tisza ; Village
the individual settlements. A common feature of the five sample villages selected is that they had been damaged considerably during some of the great floods of the past decades. The conclusion of the investigation is that the safety of the Upper Tisza Region from
This paper is a contribution to the investigation of point bar and natural levee formation in the middle section of Tisza River (E-Hungary). Point bars and natural levees increase the size of mean-stage channel as well as its water transport
Két hatranyos helyzetü terület az Alfoldon: A Kozép-Tiszavidék és a Berettyo-Korosvidék. (Two backward areas in the Great Hungarian Plain: Mid-Tisza and Berettyo-Koros regions)
(1981) ; Alfold ; Berettyo-Koros ; Croissance ; Développement rural ; Géographie de l'Europe ; Hongrie ; Mid-Tisza ; Modernisation ; Peuplement ; Production agricole ; Réseau de peuplement
Action anthropique ; Aménagement hydraulique ; Cours d'eau ; Danube ; Géographie de l'Europe ; Hongrie ; Régularisation de l'écoulement ; Tisza
construction of the Bos-Nagymaros barrage system very important. Prospectively this will be connected with the Danube-Tisza canal, which is important not only for transport but also in respect to the long-range water-supply of the Tisza Valley. (C. Kiriczi).
Strategy or disaster. Flood prevention related issues and actions in the Tisza River basin
Accumulation fluviatile ; Crue ; Hongrie ; Lutte contre les inondations ; Tisza
Changes in land use of the lowland landscape along the Tisza River have largely been shaped by processes that took place after flood control and regulation measures of that river. As a result fluvial accumulation has either been eliminated
Danube ; Domaine aride ; Domaine semi-aride ; Dégradation des sols ; Désertification ; Hongrie ; Tisza
is a real national danger, especially on the Danube-Tisza interfluve. There are areas in Hungary corresponding to desertification definitions. Thus, desertification research is an important challenge for Hungarian geography. - (AM)
Bassin-versant ; Classification hiérarchique ; Géomorphométrie ; Roumanie ; Réseau de drainage ; Tisza
This paper describes the main characteristics of the catchment area of Upper Tisza, the hierarchical system of the network of waterways and the quantitative relations between the parameters through examining a representative sample area. - (JS)
Aménagement hydraulique ; Gestion de l'eau ; Hongrie ; Paysage aménagé ; Plaine d'inondation ; Risque naturel ; Tisza
This study presents a solution for the increasing challenges and danger caused by floods of the Tisza river. According to the concept presented here the probability of floods can drop to 1 in 8 as a result of the further development
A new lithological evaluation and typology of loess exposures in Transdanubia and on the Danube-Tisza Interfluve in Loess and the Quaternary: Chinese and Hungarian case studies.
Bassin-versant ; Décision ; Economie de l'eau ; Gestion ; Géographie physique ; Hongrie ; Programmation à buts multiples ; Recherche opérationnelle ; Ressource en eau ; Système ; Tisza, fl.
Analyse des techniques d'optimisation dans le cadre d'une programmation à buts multiples appliquée au développement d'un système de ressources en eau d'un bassin-versant... Application au bassin de la Tisza, Hongrie.
Agriculture ; Géographie de l'Europe ; Géographie historique ; Histoire rurale ; Hongrie ; Siècle XVIII-XIX ; Tisza ; Village
The fok agriculture of villages along the Tisza river is described. (Fok is a gap breaking trough natural level). The physical and economic geographical picture is shown in the 18th-19th century by the example of the village Tiszatarjan. (DLO).