Water resource management (WRM) practices, such as abstractions and discharges, may impact baseflow. Here the CAMELS-GB large-sample hydrology dataset is used to assess the impacts of such practices on baseflow index (BFI) using statistical models of 429 catchments from Great Britain. Two complementary modelling schemes, multiple linear regression (LR) and machine learning (random forests, RF), are used to investigate the relationship between BFI and two sets of covariates (natural covariates only and a combined set of natural and WRM covariates). The LR and RF models show good agreement between explanatory covariates. In all models, the extent of fractured aquifers, clay soils, non-aquifers, and crop cover in catchments, catchment topograp...
AbstractStudy regionThe study region encompasses the Upper Colorado River Basin (UCRB), which provid...
Quantification of temporal variations in baseflow is crucial for sustainable water resources managem...
Baseflow index (BFI) prediction in ungauged basins has largely been based on the use of catchment ph...
Linear regression methods can be used to quantify geological controls on baseflow index (BFI). This ...
Baseflow plays an important role in maintaining streamflow. Seventeen gauged watersheds and their ch...
Baseflow is critical for water balance budget, water resources management, and environmental evaluat...
A catchment's hydrological response is controlled by climatic forcing and by the landscape through w...
There is no general theory to explain differences in baseflow between catchments, despite evidence t...
Baseflow contributions from groundwater sources have been overlooked with regards to peak flows. Onl...
This study investigated how sporadic river datasets could be used to quantify temporal variations in...
The baseflow of the Wolf River (drainage area of 1,200 km2) in northeastern Wisconsin (USA) has dec...
This study investigates groundwater discharge to rivers in the Shire River Basin, Malawi, using the ...
A baseflow separation methodology combining the outcomes of the flow–duration curve and the digital ...
Linear regression methods can be used to quantify geological controls on baseflow index (BFI). This ...
Summary Baseflow is often considered to be the groundwater discharge component of streamflow. It is...
AbstractStudy regionThe study region encompasses the Upper Colorado River Basin (UCRB), which provid...
Quantification of temporal variations in baseflow is crucial for sustainable water resources managem...
Baseflow index (BFI) prediction in ungauged basins has largely been based on the use of catchment ph...
Linear regression methods can be used to quantify geological controls on baseflow index (BFI). This ...
Baseflow plays an important role in maintaining streamflow. Seventeen gauged watersheds and their ch...
Baseflow is critical for water balance budget, water resources management, and environmental evaluat...
A catchment's hydrological response is controlled by climatic forcing and by the landscape through w...
There is no general theory to explain differences in baseflow between catchments, despite evidence t...
Baseflow contributions from groundwater sources have been overlooked with regards to peak flows. Onl...
This study investigated how sporadic river datasets could be used to quantify temporal variations in...
The baseflow of the Wolf River (drainage area of 1,200 km2) in northeastern Wisconsin (USA) has dec...
This study investigates groundwater discharge to rivers in the Shire River Basin, Malawi, using the ...
A baseflow separation methodology combining the outcomes of the flow–duration curve and the digital ...
Linear regression methods can be used to quantify geological controls on baseflow index (BFI). This ...
Summary Baseflow is often considered to be the groundwater discharge component of streamflow. It is...
AbstractStudy regionThe study region encompasses the Upper Colorado River Basin (UCRB), which provid...
Quantification of temporal variations in baseflow is crucial for sustainable water resources managem...
Baseflow index (BFI) prediction in ungauged basins has largely been based on the use of catchment ph...