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The Simulation of Rainfall-runoff process for the Czech Elbe River Basin Using One Hundred Years Daily Series
Buchtele, Josef ; Buchtelová, Marie ; Fořtová, Magda
Water regime changes happen in consequence of human activity on streams and in landscape. The present article deals with runoff changes caused by channel adjustment and by historical and recent reservoirs influence and deforestation and water withdrawal effect. The changes are evaluated by water balance and by rainfall-runoff process simulations.
Analysis of water regimes in two experimental basins in Beskydy Hills
Buchtele, Josef ; Košková, Romana ; Jařabáč, M.
Rainfall-runoff simulations were carried out in two experimental catchments with the aim of evaluation of the outflow changes caused by the defforestation. Results showed apparent influence on outflow.
Comparison of measured and simulated soil waters
Buchtele, Josef ; Buchtelová, Marie ; Tesař, Miroslav ; Šír, Miloslav
Measured values of soil water in localities with different vegetation were compared with the simulations of components of soil water using two rainfall-runoff models, SAC-SMA and BROOK. Simulated and measured volumes are different, time courses are similar.
Changes of water regime due to land use change
Buchtele, Josef ; Buchtelová, Marie ; Košková, Romana
Tendencies in water regime resulting from land-use change represent an important and actual subject for research on global scale as well as urgent problem from the local viewpoint.The assessment of deforestation, urbanisation and intense farming effects on flood regime on local or regional scale represent an important and integral part of such intentions and projects. Gradual deforestation, then overgrowing of deforested areas with grass or reforestation of some parts of catchments indicate that the change of vegetation cover did not occur as an abrupt change, but often even random phenomena took place, such as damage in woods inflicted by bark beetle, etc. In order to compare consequences of all these phenomena in different natural conditions simulations in relatively undisturbed areas, i.e. in the Šumava Mts in southern Bohemia were incorporated into the studies. The Vltava catchment down the river to Lenora village and Otava catchment down to Modrava are used for such comparisons.
Results of a rainfall-runoff model used for simulations in selected sub-basins of the Czech par of the Elbe river
Buchtele, Josef ; Košková, Romana ; Fořtová, Magda
The simulations of rainfall-runoff processes were prepared for the selected sub-basins of the Czech Labe river. The tool used for simulations was rainfall-runoff model Sacramento developed by the National Weather Service River Forecast Center. The aim of the project was to ascertain the changes int the observed and simulated runoff series caused by the geomorphological and climate conditions, by the model sensitivity to input data and by the human activities as land cover and land-use changes.
Influence of land-use changes on flood regime - simulation using rainfall-runoff model
Buchtele, Josef ; Buchtelová, Marie ; Fořtová, Magda
Deforestation induced by acid rains causes also the changes of runoff process. Data of one experimental basin have been used for simulation which should reveal appearing runoff changes.
Comparision of water balance simulations in catchments with different geomorphological conditions and antropogeneous influence
Buchtele, Josef ; Buchtelová, Marie ; Tesař, Miroslav ; Kulasová, A.
Simulations of rainfall-runoff processes for several basins of different size and climatic conditions show that deterministic hydrological models can be useful tools for evaluation of influence of land-use changes on water balance. However for such evaluation using differences between simulated and observed runoff also other analyses (using different time scales and/or statistical methods) are needed, especially when the changes are successive.
Rainfall-runoff modelling in different hydrogeologic environments
Buchtele, Josef ; Buchtelová, Marie
Simulations of runoff components and sub-surface water storages, using SAC-SMA model, have been carried out for basins in two areas in the Bohemian massif with quite distinct hydrogeological conditions: one is the area with crystalline bedrocks in south Bohemia, the other one belongs to Cretaceous area in north-eastern part of Bohemia. Results show that hydrogeological conditions are important for variability of storage and consequently of outflows. Variability of simulated sub-surface water storages in one basin in Cretaceous also indicate that agrometeorogical and hydrological droughts do not need to appear simultaneously.

National Repository of Grey Literature : 32 records found   previous11 - 20nextend  jump to record:
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5 Buchtele, Jaroslav
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