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In a model reliating snow water equivalent to 6 combinations of topo- graphic and forest variables on Marmot Creek experimental basin, 36 per cent of the variance was accounted...
A physically based model built upon extensive field observations of radiation dynamics and snow processes in cold regions forest environments was used to investigate the impacts of prescribed ...
The Smoky River tributary of the Peace River has an ungauged (in real-time) basin area of 23,769 km2, corresponding to 46% of its basin area of 51,839 km2. The purpose of this study was to develop a m...
In many parts of the world, snowmelt energetics is dominated by solar irradiance. This is particularly the case in the Canadian Rocky Mountains, where clear skies dominate the winter and spring. In m...
A model including slope effects on snow redistribution, interception and energetics was developed using the Cold Regions Hydrological Model platform, parameterized with minimal calibration and manipu...
Marmot Creek Research Basin was the subject of intense studies of snowmelt, water balance and streamflow generation in order to generate a five year database of precipitation inputs, snowpack dynamics...
Radiation is the main energy source for snowpack warming and melt in mountain needleleaf forests, and runoff from these forests is the main contributor to spring river flows in western North America....
Simulation of areal snowmelt and snowcover depletion over time can be carried out by applying point-scale melt rate computations to distributions of snow water equivalent (SWE). In alpine basins, thi...
The snow surface temperature is an important quantity in the snow energy balance, since it modulates the exchange of energy between the surface and the atmosphere as well as the conduction of energy i...
A technique of using satellite-derived data for constructing continuous snow characteristics fields for distributed snowmelt runoff simulation is presented. The satellite-derived data and the availabl...
Measurcmcnts on evaporation and the melting of snow cover are presented, followed by .an explanation of how the measured values depend on mctcorological factors and thc structure of the snow. The ob...
Following the development of rainfall-runoff models the attention of the international hydrologic program is now increasingly focused on the snowmelt- runoff. The present simple model is based on ta...
The snowmelt at a point is estimated through a simplified energy budget. From the energy equation a degree-day method is derived. The rate of snowmelt is found as a constant multiplied by the temper...
In connection with water acidification and the subsequent disappearance of fish populations and also massive fish kills during spring floods, particular interest has been focused upon the fate and e...
The snowmelt-runoff model developed by Martinec (1975) has been used to simulate daily streamflow on the 228 km2 Dinwoody Creek basin in Wyoming, U.S.A. using snowcover extent from Landsat and conve...

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