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A Korosok arvizeinek néhany hidrologiai sajatossagai és az 1980. évi arviz. (Hydrology of floods on the Koros rivers with a special regard to events of the flood in 1980)
The author gives an overview of floods and flood control measures on the Koros rivers, East-Hungary. The study is concerned with the laws of occurrence, monthly and annual distribution of floods, the sudden fluctuations in water regime, the mean
and peak discharges of rivers and the duration of floods on various stretches.

The five distinct topographic units of the vicinity of the town (alluvial plain covered with wind-blown sand, Upper Pleistocene residual levels, high flood-plain, low flood-plain and the active flood-plain) are described and mapped by the author.

Ovatko Pohjanmaan jokien tulvat kasvaneet ? (Have the floods in Ostrobothnia increased ?)
It has often been claimed in Finland during the 1980's that flooding in Ostrobothnia has increased as the result of ditching and other regulation measures. In order to gain additional information about the subject a study is made of a number
of rivers known to flod regularly over two twenty year periods. During the first period, 1940-1959, there was still little regulation of the rivers and ditching of the forests and bogs| during the second period, 1964-1983, the changes wrought by man were

The upper Pite River valley. A study of large boulder deposits and catastrophic floods.

Die Uberschwemmungen der Elbe bei Wittenberg und ihre Auswirkungen auf den Boden und die Grasbestände im Deichvorland. (Floods of the river Elbe near Wittenberg and effects on the soil and grasslands of foreshore)
Between 1974 and 1978, the time, intensity and frequency of floods of the river Elbe near Wittenberg were recorded and the effects on soil and grassland investigated. On the foreshore, sedimentation prevailed over erosion. The deposits were unevenly
spread (between 4 to 20 and 30 to 50 ha) depending on the relief and the flow conditions. They were rich in humus and nutrients. Permanent grassland showed great tolerance of flooding. Reseeded grassland was strongly affected by excessive alluvial mud (2
-3 cm). Flooding tolerance was high in Phalaris arundinacia, Alepecurus pratensis, Phlenum pratense, Proa pratensis| moderate in Festuca pratensis| and low in Lolium perenne.

Hydrometeorologicky rozbor povodni na Vltave v Praze za obdobi 1873 az 1982. (Hydrometeorological analysis of floods on Vltava in Prague in period 1873-1982)
There are followed the whole 36 cases of flood discharges in 1873-1982. Maximum crest discharge exceeded 1 490 m/sec. On the basis of analysis of meteorological situations and deviations of average daily air temperatures from long-term standards

Vyskyt povodni na Vltave v Praze vevztahuk prazskym meteorologickym pozorovanim v Klementinu. (Floods occurrence on the Vltava river in relation to meteorological observations of Prague Clementinum)
It was stated the connection between flood peak-discharge in Prague and some meteorological elements based on the long series observations performed in Clementinum Prague station, 1771-1954. (MS).

Példak a folyoszabalyozasok utani arvizek településhalozatformalo hatasara az Alfoldon. (Examples for the influence of floods after river regulations on the formation of the settlement network in the Great Plain)
Physical geographical factors have always affected the spatial pattern of settlement network. The effects of water should be counted with even today. The study exemplifies the role of floods in the development of settlements with two older (1879

The basin of the Ecsed Swamp was formed in the Holocene but intensive swamping occured only in the Beech Phase. Village people on the swamp were occupied in flood-plain agriculture. This flood-plain agriculture was based on artificial channels

The governing role of topography is stressed in the spatial distribution of salt-affected soils and in the constellation of conditions inducing solonchak formation. Flood-plain geomorphological patterns (natural levees and enclosed depressions
) control surficial and groundwater movements and flood-plain deposition and eventually soil fertility. (DLO).

Floods on modified floodplains in Man's impact on the hydrological cycle in the United Kingdom.

Extreme rainfall and its implications for flood frequency : a case study of the middle river Tweed basin, Scotland

The building of mill races was an important factor in the geomorphological development of river valleys and flood-plains in the Bohemian and Moravian landscape through the Middle Ages. This activity was connected not only with early channeling works
but it affected the development of flood-plains as well as the accumulation of fine-grained overbank deposits. - (MS)

Sédimentation and water quality in the flood basin of the river Kyronjoki in Finland

Flooding (acqua alta) in Venice (Italy): a worsening phenomenon in Coastal problems, in the mediterranean sea.

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