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This paper describes an exploration in using SVM (Support Vector Machine) models, which were initially developed in the Machine Learning community, in flood forecasting, with the focus on the identifi...
Considerable effort has been expended on the theoretical aspects of the applicability of the unsteady flow equations to natural overland flow. The major difficulty when these equations are used to s...
A conceptual model has been developed for the prediction of runoff on a daily basis from snowcovered and glacierized basins. The basin is divided into an icefree area and an icecovered area, which a...
Work presented here consists of two parts: the first part, presented before as a separate paper (Niemczynowicz 1984b), described studies performed on conceptual catchment, the secoGd part presented ...
Work reported here consists of two parts: the first part describes studies performed on a conceptual catchment, the second part, presented as a separate paper, describes studies on real catchments i...
Rainfall runoff phenomena in small watersheds are favorably modelled using the kinematic wave approach. The present investigation considers excess rainfall as time dependent but ignores spatial effe...
A physically based soil frost depth model usable with air temperature data and precipitation data, is presented. Snow depth is calculated from precipitation data using a physical snow cover model. T...
A physically-based rainfall-runoff model is used to investigate effects of moving storms on the runoff hydrograph of throughflow dominated idealised catchments. Simulations are undertaken varying th...
Modelling of runoff' in GCMs is a two-stage process: first, a residual water amount resulting from precipitation, evapotranspiration, snowmelt, infiltration and soil moisture movement at each time s...
In the first of this two-paper series, the main mechanisms for generation of runoff from rainfall in large basins with small to negligible slopes are analyzed using available data from the Rio Negro...
Superficial moraines grew in size during the entire 32-year-long period of direct monitoring of water and ice balance of the Djankuat Glacier in the Caucasus. The total area of debris cover on the g...
This paper demonstrates the spatial variability of surface runoff components, accumulated peak flow (Q a ) and excess runoff depth (R a ), in response to varying distribution of precipitation on a bas...
Plot Measurements of Snowmelt Runoff for Varying Soil Conditions.
Measurements of pH, alkalinity and electrical conductivity are used to examine the extent of the spatial and temporal variation in stream and ground water chemistry for the Upper Severn catchment, Pl...
A combined hydrological and chemical investigation was undertaken in a small moorland catchment at Plynlimon to determine the processes controlling storm runoff chemistry. Flow from natural soil pipe...

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