Integrated dynamic water and chloride balance models with a catchment-scale hydrological model (PRMS) are used to investigate the response of a terminal tropical lake, Lake Abiyata, to climate variability and water use practices in its catchment. The hydrological model is used to investigate the response of the catchment to different climate and land-use change scenarios that are incorporated into the lake model. Lake depth-area-volume relationships were established from lake bathymetries. Missing data in the time series were filled using statistical regression techniques. Based on mean monthly data, the lake water balance model produced a good agreement between the simulated and observed levels of Lake Abiyata for the period 1968-83. From ...
Lake Hawassa is a topographically closed lake in the Central Main Ethiopian Rift Valley. The water l...
The aim of this study is to evaluate the hydrological impacts of climate change on the water balance...
A hydrological modelling at a catchment scale has been used to investigate the impact of climatic an...
Integrated dynamic water and chloride balance models with a catchment-scale hydrological model (PRMS...
In this paper, the water level fluctuations of eight Ethiopian Rift Valley lakes were analyzed for t...
A good understanding of the local and regional water cycle and how it is modified by landscape chang...
We develop and present a novel integrated water balance model that accounts for lake watergroundwate...
Lake Abiyata is a small, closed, saline–alkaline lake located in the central part of the Ethiopian R...
We develop and present a novel integrated water balance model that accounts for lake water—groundwat...
The Central Rift Valley (CRV) of Ethiopia is a closed basin where claims on land and water have stro...
The Main Ethiopian Rift Valley Lakes suffer from water level fluctuations due to several natural and...
Due to the rapid socio-economic development in the Ethiopian Rift Valley basin, the pressures on wat...
The Katar and Meki subbasins play a significant role in supporting the livelihoods of people in the ...
Lake Hawassa is a topographically closed lake in the Central Main Ethiopian Rift Valley. The water l...
The aim of this study is to evaluate the hydrological impacts of climate change on the water balance...
A hydrological modelling at a catchment scale has been used to investigate the impact of climatic an...
Integrated dynamic water and chloride balance models with a catchment-scale hydrological model (PRMS...
In this paper, the water level fluctuations of eight Ethiopian Rift Valley lakes were analyzed for t...
A good understanding of the local and regional water cycle and how it is modified by landscape chang...
We develop and present a novel integrated water balance model that accounts for lake watergroundwate...
Lake Abiyata is a small, closed, saline–alkaline lake located in the central part of the Ethiopian R...
We develop and present a novel integrated water balance model that accounts for lake water—groundwat...
The Central Rift Valley (CRV) of Ethiopia is a closed basin where claims on land and water have stro...
The Main Ethiopian Rift Valley Lakes suffer from water level fluctuations due to several natural and...
Due to the rapid socio-economic development in the Ethiopian Rift Valley basin, the pressures on wat...
The Katar and Meki subbasins play a significant role in supporting the livelihoods of people in the ...
Lake Hawassa is a topographically closed lake in the Central Main Ethiopian Rift Valley. The water l...
The aim of this study is to evaluate the hydrological impacts of climate change on the water balance...
A hydrological modelling at a catchment scale has been used to investigate the impact of climatic an...