The Lower Zambezi River is influenced by the presence of two very large hydropower impoundments which have modified the natural seasonal flows, the sediment balance, the morphology of the river and the pattern of the riparian vegetation. Downstream of these large impoundments, appreciable local effects are reported to take place, such as scour, bank collapse and shoreline degradation. In order to quantify the sediment transport along the Lower Zambezi River and to predict the effects of the dams on morphology we have developed a simplified 1-D hydro-morphodynamic model capable to deal with the scarcity of available data. Besides the systematic flow records at the dam gauging station and few occasional measurements of turbidity and grain siz...
The Middle Zambezi, host to a rich biodiversity, is located in the central part of the Zambezi River...
The meandering Ribb River flows in northwest Ethiopia to Lake Tana, the source of the Blue Nile Rive...
The Ayeyarwady River is a river with large hydrological variations and an abundance of relatively fi...
The Lower Zambezi River is influenced by the presence of two very large hydropower impoundments whic...
The Zambezi River is the fourth largest river in Africa (after the Congo, Nile, and Niger), and it i...
none3River morphodynamics are the result of a variety of processes, ranging from the typical small-s...
In terms of changing flow and sediment regimes of rivers, dams are often regarded as the most domina...
The Zambezi Basin, a semi-arid 1.4 Mio km2 catchment area spreading across eight countries, constitu...
ABSTRACT: The Zambezi Basin, a semi-arid 1.4Mio km2 catchment area spreading across eight countries,...
The meandering Ribb River flows in northwest Ethiopia to Lake Tana, the source of the Blue Nile Rive...
This work investigates the applicability of an analytical method for quick assessments of the long-t...
Natural damming of upland river systems, such as landslide or lava damming, occurs worldwide. Many d...
Gully erosion is a significant and widespread feature of southern African wetlands, including the we...
The establishment of stability in rivers is dependent on a variety of factors, and yet the establish...
The Pongola Floodplain in the Makhathini Flats is an area of low topographic relief between the 1973...
The Middle Zambezi, host to a rich biodiversity, is located in the central part of the Zambezi River...
The meandering Ribb River flows in northwest Ethiopia to Lake Tana, the source of the Blue Nile Rive...
The Ayeyarwady River is a river with large hydrological variations and an abundance of relatively fi...
The Lower Zambezi River is influenced by the presence of two very large hydropower impoundments whic...
The Zambezi River is the fourth largest river in Africa (after the Congo, Nile, and Niger), and it i...
none3River morphodynamics are the result of a variety of processes, ranging from the typical small-s...
In terms of changing flow and sediment regimes of rivers, dams are often regarded as the most domina...
The Zambezi Basin, a semi-arid 1.4 Mio km2 catchment area spreading across eight countries, constitu...
ABSTRACT: The Zambezi Basin, a semi-arid 1.4Mio km2 catchment area spreading across eight countries,...
The meandering Ribb River flows in northwest Ethiopia to Lake Tana, the source of the Blue Nile Rive...
This work investigates the applicability of an analytical method for quick assessments of the long-t...
Natural damming of upland river systems, such as landslide or lava damming, occurs worldwide. Many d...
Gully erosion is a significant and widespread feature of southern African wetlands, including the we...
The establishment of stability in rivers is dependent on a variety of factors, and yet the establish...
The Pongola Floodplain in the Makhathini Flats is an area of low topographic relief between the 1973...
The Middle Zambezi, host to a rich biodiversity, is located in the central part of the Zambezi River...
The meandering Ribb River flows in northwest Ethiopia to Lake Tana, the source of the Blue Nile Rive...
The Ayeyarwady River is a river with large hydrological variations and an abundance of relatively fi...