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Derivation of Instantaneous Unit Hydrograph for a sub-basin using Linear Geomorphological Model and Geographic Information Systems
Geographic Information System GIS Linear Geomorphological Model LGM GIUH
2015/8/14
Rainfall is converted into runoff and reaches the river and it becomes river flow. Geomorphological Instantaneous Unit Hydrograph (GIUH) based approach, which uses the geomorphologic parameters, is us...
Estimating land-use change impacts on direct runoff and non-point source pollutant loads in the Richland Creek basin (Illinois,USA) by applying the L-THIA model
land-use change runoff non-point source pollution hydrological model
2015/8/13
An export coefficient approach to hydrological and non-point source (NPS) pollution modeling enables quick and simple assessment of long-term impacts for planning purposes. An export coefficient and g...
Surface water potential of the river Osun at Apoje sub-basin Nigeria
streamflow gauge heights Apoje sub-basin
2015/2/3
In order to archive the millennium goals of which water for all by the year 2015 is a major component; all efforts must be made to efficiently utilise the available water resources in various parts of...
Multi-model comparison of a major flood in the groundwater-fed basin of the Somme River (France)
Multi-model comparison major flood groundwater-fed basin Somme River
2010/2/1
The Somme River Basin is located above a chalk aquifer and the discharge of the somme River is highly influenced by groundwater inflow (90% of river discharge is baseflow). In 2001, the Somme River Ba...
RAINFALL INTERCEPTION IN A FOREST IN THE VELEN HYDROLOGICAL REPRESENTATIVE BASIN
RAINFALL INTERCEPTION VELEN HYDROLOGICAL REPRESENTATIVE BASIN
2009/10/29
In the summer and autumn ot 1973, 25 rain troughs were operating below
canopy and four in clearings of a predominantly coniferous forest in the
Velen hydrological research area. The collected rain w...
SYNTHESIS OF BASIN RESPONSE WITH INADEQUATE DATA
SYNTHESIS BASIN RESPONSE INADEQUATE DATA
2009/10/29
The present study is focussed on the problem of developing a basin response
function with inadequate data. The case of a catchment with some
measurements of output and with input data either totally...
Extrapolating Snow Measurements on the Marmot Creek Experimental Basin
Snow Measurements Marmot Creek Experimental Basin
2009/10/27
From 1969 to 1980, each March, snow depth and water equivalent were sampled
around 249 pins of a grid covering the forested portion of Marmot Creek
basin. Continuous record from four snow pillows an...
Forecasting Watercooling in the Kattegat,the Öresund,the Belt Sea and the Arkona Basin
Watercooling Kattegat Ö resund Belt Sea Arkona Basin
2009/10/27
Some problems associated with forecasting water cooling in the entrance to the
Baltic Sea are examined, using a diagnostic study from the severe ice winter of
1986187 as a starting point. In the stu...
Hydrological Analysis of Basin Behaviour from Soil Moisture Data
Hydrological Analysis Basin Behaviour Soil Moisture Data
2009/10/27
Soil moisture dynamics in the Velen drainage basin (Sweden) were analyzed in
order to assess the degree of and the reasons for spatial variation in basin
behaviour. The main tool was a modified vers...
A Test of Snowmelt-Runoff Model for a Major River Basin in Western Himalayas
Snowmelt-Runoff Model Major River Basin Western Himalayas
2009/10/27
In the Snowmelt-Runoff Model (SRM), the estimate of discharge volume is
based on temperature condition in the form of degree days which are used to
melt the snowpack in the area of the basin covered...
The Influence of Basin Aridity on the Efficiency of Runoff Predicting Models
Basin Aridity Efficiency Runoff Predicting Models
2009/10/26
The connection between runoff predicting models efficiency and basin aridity is
investigated by using data from five representative basins in the mountainous
central and northern Greece. Two substan...
Snowmelt Runoff and Total Solids Production in a Discontinuous Permafrost Basin
Snowmelt Runoff Solids Production Discontinuous Permafrost Basin
2009/10/26
Snowmelt runoff and total suspended solids were measured for two years on
Glenn Creek, a small, second-order, subarctic stream located near Fairbanks,
Alaska, within the Yukon-Tanana Uplands physiog...
Reconstructed Runoff from the High Arctic Basin Bayelva based on Mass-Balance Measurements
High Arctic Basin Bayelva Mass-Balance Measurements
2009/10/26
The river Bayelva drains a catchment area of 31.5 km2 in the Kongsfjord area close to the research station Ny-Ålesund (79° N 12°E) on the northwest coast of Spitsbergen. The basin is 54% glacier...
THE PREDICTION OF DAILY OUTFLOW FOR AN UNGAGED MOUNTAINOUS BASIN
DAILY OUTFLOW rainfall period Generalized Flood Pattern Method
2009/10/19
To evaluate the daily outflow from a 212-km2 basin in a mountainous part of the downstream Amur river, which has no rain gages, a modeling approach is needed. The average basin rainfall during a rainf...
RAINFALL-RUNOFF SIMULATION IN AN EXPERIMENTAL BASIN USING GIS METHODS
rainfall-runoff travel time map steep watershed
2009/10/12
A GIS-based rainfall-runoff model was developed to simulate the runoff discharge at the outlet of a 15.18 km2 gauged steep watershed that is located at the prefecture of Attica, Greece. The model抯 cor...