The assessment of water withdrawals for irrigation is essential for managing water resources in cultivated tropical catchments. These water withdrawals vary seasonally, driven by wet and dry seasons. A land use map is one of the required inputs of hydrological models used to estimate water withdrawals in a catchment. However, land use maps provide typically static information and do not represent the hydrological seasons and related cropping seasons and practices throughout the year. Therefore, this study assesses the value of seasonal land use maps in the quantification of water withdrawals for a tropical cultivated catchment. We developed land use maps for the main seasons (long rains, dry, and short rains) for the semi-arid Kikuletwa cat...
Efficient water-resource management is essential with regard to food security, growing populations a...
This study provides a detailed assessment of land cover (LC) changes on the water balance components...
Land use change and climate variability are the main drivers of watershed hydrological processes. Th...
The assessment of water withdrawals for irrigation is essential for managing water resources in cult...
This research article was published by MDPI, 2019The assessment of water withdrawals for irrigation ...
In SWAT and SWAT+ models, the variations in hydrological processes are represented by Hydrological R...
In most (sub)-tropical African cultivated regions, more than one cropping season exists following th...
In arid and semi-arid areas, evaporation fluxes are the largest component of the hydrological cycle,...
Intensification of agricultural land use and population growth from 1990-2017 has caused changes in...
This research article published by MDPI, 2020In SWAT and SWAT+ models, the variations in hydrologica...
Study area Kikuletwa catchment, Upper Pangani River Basin, Tanzania. Study focus This study compare...
Mara is a transboundary river located in Kenya and Tanzania and considered to be an important life l...
Many parts of sub-Saharan Africa (SSA) are prone to land use and land cover change (LULCC). In many ...
Many parts of sub-Saharan Africa (SSA) are prone to land use and land cover change (LULCC). In many ...
Deterioration of upland soils, demographic growth, and climate change all lead to an increased utili...
Efficient water-resource management is essential with regard to food security, growing populations a...
This study provides a detailed assessment of land cover (LC) changes on the water balance components...
Land use change and climate variability are the main drivers of watershed hydrological processes. Th...
The assessment of water withdrawals for irrigation is essential for managing water resources in cult...
This research article was published by MDPI, 2019The assessment of water withdrawals for irrigation ...
In SWAT and SWAT+ models, the variations in hydrological processes are represented by Hydrological R...
In most (sub)-tropical African cultivated regions, more than one cropping season exists following th...
In arid and semi-arid areas, evaporation fluxes are the largest component of the hydrological cycle,...
Intensification of agricultural land use and population growth from 1990-2017 has caused changes in...
This research article published by MDPI, 2020In SWAT and SWAT+ models, the variations in hydrologica...
Study area Kikuletwa catchment, Upper Pangani River Basin, Tanzania. Study focus This study compare...
Mara is a transboundary river located in Kenya and Tanzania and considered to be an important life l...
Many parts of sub-Saharan Africa (SSA) are prone to land use and land cover change (LULCC). In many ...
Many parts of sub-Saharan Africa (SSA) are prone to land use and land cover change (LULCC). In many ...
Deterioration of upland soils, demographic growth, and climate change all lead to an increased utili...
Efficient water-resource management is essential with regard to food security, growing populations a...
This study provides a detailed assessment of land cover (LC) changes on the water balance components...
Land use change and climate variability are the main drivers of watershed hydrological processes. Th...