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Hydrological processes of the Danube River Basin : perspectives from the Danubian countries

Mitja Brilly
TLDR
The Danube River and its Basin Physical Characteristics, Water Regime and Water Balance are discussed in this article, along with the role of runoff regime and its stability in the Danube Catchment.
Abstract
History and Results of the Hydrological Co-operation of the Countries Sharing the Danube Catchment (1971-2008).- The Danube River and its Basin Physical Characteristics, Water Regime and Water Balance.- Palaeogeography of the Danube and Its Catchment.- Danube River Basin Coding.- Characterization of the Runoff Regime and Its Stability in the Danube Catchment.- Coincidence of Flood Flow of the Danube River and Its Tributaries.- Basin-Wide Water Balance in the Danube River Basin.- Thermal and Ice Regimes of the Danube River and Its Tributaries.- Sediment Regime of the River Danube (1956-1985).- Training of the Danube River Channel.- The Fords of the Danube.- Forecast Uncertainties in the Operational Flood Forecasting of the Bavarian Danube Catchment.- Sarib.

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Review Article: Structural flood-protection measures referring to several European case studies

TL;DR: In this article, a review of structural measures that were taken to cope with floods in some cities along the Danube River, such as Vienna, Bratislava, and Belgrade, is presented.
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The use of fluvial archives in reconstructing landscape evolution: the value of sedimentary and morphostratigraphical evidence

TL;DR: In this article, the concept of headward-migrating knickpoints implies a mechanism for incision that is difficult to reconcile with the formation of the broadly parallel river terraces that are observed in many systems.
Journal ArticleDOI

The hillslope length impact on SWAT streamflow prediction in large basins

TL;DR: In this paper, the impact of hillslope length on Soil and Water Assessment Tool (SWAT) streamflow predictions in large basins was assessed using three methods for hill-slope length calculation (the SWAT method, L1; a 3D analysis method L2; a constant value, L3).