Low flow regime is tightly dependent on catchment hydrogeological features and a detailed surface and groundwater catchment analysis is necessary for an accurate characterization. However on a practical perspective regional statistical analysis is widely applied to derive indexes to characterize low flow regimes in poorly gauged watersheds. In this study we focus on some of the well known low flow statistics such as the Q7,T and the flow duration curve and we particularly investigate the importance of geological features. It has been found that it is possible to derive regional flow-duration and flow-frequency curves starting from the knowledge of a BFI regional value, which is essentially dependent on permeability
ABSTRACT: A regional hydrologic model is developed for estimating flow-dura-tion curves at ungauged ...
ABSTRACT Knowledge of natural water availability, which is characterized by low flows, is essential ...
Models incorporating the appropriate temporal scales of dominant indicators for low flows are assume...
Low flow regime is tightly dependent on catchment hydrogeological features and a detailed surface an...
Low flow characteristics are usually estimated from flow gauge stations. However hydrological data a...
Regional maps and equations for the magnitude and frequency of 1, 7 and 30-day low flows were derive...
Low flows can impact water use and instream ecology. Therefore, reliable predictions of low-flow met...
Well-integrated water management can notably require estimating low flows at any point of a river. D...
The paper intends to review the current status of low-flow hydrology — a discipline which deals with...
Regional maps and equations for the magnitude and frequency of 1, 7 and 30-day low flows were derive...
The paper uses a simple water balance model that partitions the precipitation between actual evapotr...
The walloon part of the Meuse’s watershed represents 12283 km² and 17694 km of river. The anthropoge...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceEstimating low-flow indices is of p...
A period-of-record flow duration curve (FDC) represents the relationship between the magnitude and f...
International audienceThe development of regionalised hydrological models or procedures for estimati...
ABSTRACT: A regional hydrologic model is developed for estimating flow-dura-tion curves at ungauged ...
ABSTRACT Knowledge of natural water availability, which is characterized by low flows, is essential ...
Models incorporating the appropriate temporal scales of dominant indicators for low flows are assume...
Low flow regime is tightly dependent on catchment hydrogeological features and a detailed surface an...
Low flow characteristics are usually estimated from flow gauge stations. However hydrological data a...
Regional maps and equations for the magnitude and frequency of 1, 7 and 30-day low flows were derive...
Low flows can impact water use and instream ecology. Therefore, reliable predictions of low-flow met...
Well-integrated water management can notably require estimating low flows at any point of a river. D...
The paper intends to review the current status of low-flow hydrology — a discipline which deals with...
Regional maps and equations for the magnitude and frequency of 1, 7 and 30-day low flows were derive...
The paper uses a simple water balance model that partitions the precipitation between actual evapotr...
The walloon part of the Meuse’s watershed represents 12283 km² and 17694 km of river. The anthropoge...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAUInternational audienceEstimating low-flow indices is of p...
A period-of-record flow duration curve (FDC) represents the relationship between the magnitude and f...
International audienceThe development of regionalised hydrological models or procedures for estimati...
ABSTRACT: A regional hydrologic model is developed for estimating flow-dura-tion curves at ungauged ...
ABSTRACT Knowledge of natural water availability, which is characterized by low flows, is essential ...
Models incorporating the appropriate temporal scales of dominant indicators for low flows are assume...