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B. Ambroise, J. Freer, K. Beven (1996)
APPLICATION OF A GENERALIZED TOPMODEL TO THE SMALL RINGELBACH CATCHMENT, VOSGES, FRANCEWater Resources Research, 32
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Spatially Distributed Modeling: Conceptual Approach to Runoff Prediction
K. Beven, M. Kirkby, N. Schofield, A. Tagg (1984)
Testing a physically-based flood forecasting model (TOPMODEL) for three U.K. catchmentsJournal of Hydrology, 69
P. Quinn, K. Beven, P. Chevallier, O. Planchon (1991)
THE PREDICTION OF HILLSLOPE FLOW PATHS FOR DISTRIBUTED HYDROLOGICAL MODELLING USING DIGITAL TERRAIN MODELSHydrological Processes, 5
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Etude générale des variations de débits en fonction des facteurs qui les conditionnent, 2, Les variations de débit en période non influencée par les précipitationsHouille Blanche, 3
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Bayesian Estimation of Uncertainty in Runoff Prediction and the Value of Data: An Application of the GLUE ApproachWater Resources Research, 32
M. Kirkby, K. Beven (1979)
A physically based, variable contributing area model of basin hydrology, 24
Alice Robson, K. Beven, C. Neal (1992)
Towards identifying sources of subsurface flow: A comparison of components identified by a physically based runoff model and those determined by chemical mixing techniquesHydrological Processes, 6
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Unsaturated and Saturated Flow Through a Thin Porous Layer on a HillslopeWater Resources Research, 21
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The unit response of groundwater outflow from a hillslopeWater Resources Research, 30
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Some limitations of the a/s index for predicting basin wide patterns of soil water drainageZ. Geomorph. Suppl. Band, 60
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On subsurface stormflow: Predictions with simple kinematic theory for saturated and unsaturated flowsWater Resources Research, 18
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P. Quinn, K. Beven, R. Lamb (1995)
The in(a/tan/β) index:how to calculate it and how to use it within the topmodel frameworkHydrological Processes, 9
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Spatial and temporal predictions of soil moisture dynamics, runoff, variable source areas and evapotranspiration for plynlimon, mid-wales.Hydrological Processes, 7
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An application of a physically based semi-distributed model to the Balquhidder catchmentsJournal of Hydrology, 145
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Catchment geomorphology and the dynamics of runoff contributing areasJournal of Hydrology, 65
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Preliminary studies of the application of TOPMODEL to the 36‐ha Ringelbach catchment suggested that the original form of exponential transmissivity function leading to the In (a/tan β) topographic index and first‐order hyperbolic base flow recession curve is not appropriate to this catchment. Two alternative forms of topographic index and soil‐topographic index are developed based on parabolic and linear transmissivity functions, leading to the more frequently observed second‐order hyperbolic and exponential recession curves, respectively. It is shown how these can be used in the same way as the original to relate catchment average water table depths to local water table depths so that patterns of saturation can be evaluated. Two companion (Ambroise et al., this issue; Freer et al., this issue) papers show how the new parabolic index is used in the prediction of Ringelbach discharges, and how the limitations of the model are reflected in the estimated predictive uncertainties using the Generalised Likelihood Uncertainty Estimation (GLUE) approach.
Water Resources Research – Wiley
Published: Jul 1, 1996
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