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Precipitation phase is fundamental to catchment hydrological response to precipitation events in cold regions and is especially variable over time and space in mountains. Phase is controlled by t...
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...
The diverse sources of uncertainty associated with the calculation of rainfall kinetic energy and rainfall erosivity, calculated from precipitation data, were investigated at a range of temporal and s...
Measurements of the surface fluxes of radiation, heat and water vapour were made at three tundra sites near N~-Alesund, Svalbard for the active seasons (June to September) of 1995 and 1996. In 1995 ...
The Canadian Regional Climate Model has recently been coupled with an advanced, second generation land surface model - the Canadian Land Surface Scheme. In addition, high resolution land cover and s...
The availability of the actual water use from agricultural crops is considered as the key factor for irrigation water management, water resources planning, and water allocation. Traditionally, evapotr...

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