The Milibach River between Hasliberg-Reuti and Meiringen agglomerations in Switzerland has a limited hydraulic capacity leading to frequent flooding. During the 2005 flood event, large populated areas were inundated and damages exceeding many millions of Swiss francs occurred (Fig. 1). The deficit of the river flow capacity is essentially caused by a reduction of river cross sections due to local sediment deposits which lead to the overtopping of the lateral embankment
Flood risk (defined as a result of flood probability and potential damage) along Rhine and Meuse riv...
River reaches downstream dams where a constant residual flow discharge is imposed, often lack sedime...
Many multipurpose reservoirs are situated in the low mountain range of Germany. Most of them are nec...
As revitalization and protection against floods are essential in our time, the town of Delémont in S...
The Gebidem Dam located on the Massa River intercepts annually around 400’000 m3 of solid material. ...
The consideration of recent extreme events in flood statistics implies an increase of design flood p...
The regulation of the Upper Rhine between the cities Basel and Mannheim, further its subsequent deve...
In August 2005 a very severe fl ood hit large parts of Switzerland. Strong erosion occurred in sever...
During floods, the bedload transport of steep headwaters can exceed the hydraulic transport capacity...
This paper analyses the flood protection history of the Gürbe River (Switzerland), a 29-km-long trib...
Climate change is expected to cause higher discharge levels in the river Rhine at the Dutch-German b...
As one speciality of the Swiss hydraulic engineering tradition, several torrent diversion schemes we...
The Gürbe Valley, located south of Bern, is very prone to floods due to the hydrological and geologi...
The State Reservoir Administration of Saxony is planning to expand the spillway discharge capacity o...
The river Lutz as many other rivers in Austria was forced into a straight and narrow river bed. Seve...
Flood risk (defined as a result of flood probability and potential damage) along Rhine and Meuse riv...
River reaches downstream dams where a constant residual flow discharge is imposed, often lack sedime...
Many multipurpose reservoirs are situated in the low mountain range of Germany. Most of them are nec...
As revitalization and protection against floods are essential in our time, the town of Delémont in S...
The Gebidem Dam located on the Massa River intercepts annually around 400’000 m3 of solid material. ...
The consideration of recent extreme events in flood statistics implies an increase of design flood p...
The regulation of the Upper Rhine between the cities Basel and Mannheim, further its subsequent deve...
In August 2005 a very severe fl ood hit large parts of Switzerland. Strong erosion occurred in sever...
During floods, the bedload transport of steep headwaters can exceed the hydraulic transport capacity...
This paper analyses the flood protection history of the Gürbe River (Switzerland), a 29-km-long trib...
Climate change is expected to cause higher discharge levels in the river Rhine at the Dutch-German b...
As one speciality of the Swiss hydraulic engineering tradition, several torrent diversion schemes we...
The Gürbe Valley, located south of Bern, is very prone to floods due to the hydrological and geologi...
The State Reservoir Administration of Saxony is planning to expand the spillway discharge capacity o...
The river Lutz as many other rivers in Austria was forced into a straight and narrow river bed. Seve...
Flood risk (defined as a result of flood probability and potential damage) along Rhine and Meuse riv...
River reaches downstream dams where a constant residual flow discharge is imposed, often lack sedime...
Many multipurpose reservoirs are situated in the low mountain range of Germany. Most of them are nec...